Journal articles: 'Papuan Basin'

1

Swift, Michael. "Recent geological advances in the understanding of the Torres Basin." APPEA Journal 53, no. 2 (2013): 459. http://dx.doi.org/10.1071/aj12070.

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The Torres Basin is a recently discovered Mesozoic basin in the Papuan Plateau, southeast Papua New Guinea. Newly acquired deepwater offshore seismic data and older regional data have been (re)interpreted with the view of defining structural regimes in line with the onshore geological maps and conceptual cross sections. A regional time-space plot has been developed to elucidate the breakup of the northeastern Australian Plate with a focus on the geological history of the Papuan Plateau, which holds the Torres Basin geological section. This in turn has led to a re-evaluation of the structural style and history of the southern coastal region incorporating the East Australian Early Cretaceous Island Arc; it highlights that a significant horizontal structural grain needs to be considered when evaluating the petroleum potential of the region. The southern margin is characterised as a frontal thrust system, similar to the nearby Papuan Basin. A series of regional strike lines in conjunction with the dip lines is used to divide the region into prospective and non-prospective exploration play fairways. The role of transfer faults, basement-detachments faults, regional-scale thrust faults, and recent normal faulting is discussed in the compartmentalisation of the geological section. There is basement-involved anticlinal development on a large scale and a complementary smaller-scale thin-skinned anticlinal trend. These trends are characterised as having significant strike length and breadth. Anticlinal trap fairways have been defined and have similar size and distribution as that of the Papuan Basin.

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2

Ahmed, Manzur, Herbert Volk, Tony Allan, and David Holland. "Origin of oils in the Eastern Papuan Basin, Papua New Guinea." Organic Geochemistry 53 (December 2012): 137–52. http://dx.doi.org/10.1016/j.orggeochem.2012.06.002.

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3

Amiribesheli, Said, and Andrew Weller. "The prospectivity of the Cape Vogel Basin, Papua New Guinea." APPEA Journal 59, no. 2 (2019): 840. http://dx.doi.org/10.1071/aj18094.

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The frontier and underexplored Cape Vogel Basin (CVB), north of the Papuan Peninsula, is thought to be underlain by Late Palaeocene–Eocene oceanic crust and overlain by Cenozoic sediments. Several impartial data provide evidence of working petroleum system(s) including a flow of oil from a 1920s well, and two 1970s wells that encountered minor hydrocarbon traces and good source material. The 1970s wells chased Miocene reef plays (like the discoveries in the Gulf of Papua). No Miocene reefs were encountered, with both wells terminating in volcanics. Integration of open-file 2D seismic, modern 2D PSDM seismic and shipborne gravity and magnetic data improves the subsurface imaging and thus understanding of prospectivity. The data reveal a significant sedimentary section (including Mesozoic sediments) and that the volcanics are not laterally continuous (i.e. products of short periods of volcanism). The data also suggests several Mesozoic–Cenozoic plays (e.g. carbonate reefs, incised canyons). Repeatable sea surface slicks, and observable bottom-simulating reflectors and direct hydrocarbon indicators, also provide evidence of working petroleum system(s). It is hypothesised that the CVB has affinities with the Gulf of Papua with the extension of the Australian craton north of the Papuan Peninsula, with widespread deposition in the Mesozoic–Cenozoic, and with source rocks estimated to be within the hydrocarbon generative window. With incorporation of onshore data and presence of significant gravity low, it is postulated that the central and north-west were less susceptible to Late Cretaceous and Palaeocene differential uplift and erosion (related to Coral Sea breakup and extension), and thus have a higher chance of Late Mesozoic preservation.

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4

GASSMANN, DIRK, and STEPHEN J. RICHARDS. "Two new damselflies of the genus Idiocnemis Selys from Gulf Province, Papua New Guinea (Odonata: Platycnemididae)." Zootaxa 4560, no. 1 (February 22, 2019): 121. http://dx.doi.org/10.11646/zootaxa.4560.1.6.

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Two new species of the genus Idiocnemis Selys, 1886 from southern Papua New Guinea are described: Idiocnemis lakekamuensis sp. nov. from the Lakekamu Basin and I. milou sp. nov. from Lakekamu and the Kikori River lowlands. Males and females are illustrated and compared with other species of the Idiocnemis bidentata group. Both new species are known only from the Papuan Gulf Foreland area of endemism and may be considered endemic to it.

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5

Haig, D. W., and D. Medd. "Latest Miocene to Early Pliocene bathymetric cycles related to tectonism, Puri Anticline, Papuan Basin, Papua New Guinea." Australian Journal of Earth Sciences 43, no. 4 (August 1996): 451–65. http://dx.doi.org/10.1080/08120099608728267.

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6

Winn, R. D., and P. Pousai. "Synorogenic alluvial-fan – fan-delta deposition in the Papuan foreland basin: Plio-Pleistocene Era Formation, Papua New Guinea." Australian Journal of Earth Sciences 57, no. 5 (July 2010): 507–23. http://dx.doi.org/10.1080/08120099.2010.492909.

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7

Spooner, M. I., and R. I. McCarthy. "Structural and Reservoir Development of the Western Papuan Basin Gas and Condensate Fields." ASEG Extended Abstracts 2018, no. 1 (December 2018): 1–8. http://dx.doi.org/10.1071/aseg2018abt4_3a.

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8

Barclay, S. A., K. Liu, and D. Holland. "RESERVOIR QUALITY, DIAGENESIS AND SEDIMENTOLOGY OF THE PALE AND SUBU SANDSTONES: RE-VISITING THE EASTERN PAPUAN BASIN, PAPUA NEW GUINEA." APPEA Journal 43, no. 1 (2003): 515. http://dx.doi.org/10.1071/aj02027.

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Two shallow diamond drill holes (Subu–1 and Subu–2) continuously cored in August and September 2001 by InterOil Australia represent the first sub-surface penetrations of reservoir quality sandstones in the Eastern Papuan Basin of Papua New Guinea. These wells intersected two sedimentologically distinct thick quartz sandstones (>100 m). The upper sandstone unit is Campanian in age and is correlated with the Pale Sandstone, whereas the lower sandstone is of Turonian age and has not been reported previously, and is tentatively named as the Subu Sandstone in this paper.The core has been the subject of detailed reservoir quality and diagenetic study as part of a multi-disciplinary study conducted by CSIRO Petroleum. The results of the reservoir quality portion of this study form the basis of this report and demonstrate the following:There are two distinct depositional systems present with a lower sandy slope apron and basin floor fan system (Subu Sandstone) and a younger upper shoreface-shallow marine depositional system (Pale Sandstone).While the porosity and permeability data for subsurface samples (5 to 16% and 0.1 to 1000mD) are lower than previously reported by Boult and Carman (1990) for surface samples both the sandstone units demonstrate thick, good reservoir quality reservoir capable of holding significant volumes of hydrocarbons.Bitumen is present in the pore space through out the sandstones in both wells. The presence of biodegraded hydrocarbons demonstrates that liquid hydrocarbons have been generated in the basin and have either migrated through the Subu and Pale sandstone or have been reservoired in them.Associated with the bitumen is pyrite precipitated as an in-situ by-product of shallow biodegradation of the parent liquid hydrocarbon as indicated by sulphur isotope analysis.Diagenetic effects include compaction (the dominant control on reservoir quality), minor quartz cementation, minor secondary porosity generation, and in thin zones localised carbonate cementation.Despite their very different depositional settings and age difference the thin section petrology of the Pale and Subu sandstones are very similar. The subtle difference between them is textural (grain size, sorting) and detrital clay content. The Subu Sandstone is typically finer grained, displays a higher degree of sorting and has a higher detrital clay content than the Pale Sandstone.The character of these sandstones may have as much to do with provenance as with depositional environment and may indicate a separate quartz-rich depositional system sourcing sediment from the Australian craton independent of the Fly Platform Toro/Imburu systems.

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9

Bunch, Mark, Ric Daniel, Mark Lawrence, Greg Browne, Saju Menacherry, Tess Dance, and Malcolm Arnot. "Multi-scale characterisation of the Paaratte Formation, Otway Basin, for CO2 injection and storage." APPEA Journal 52, no. 2 (2012): 664. http://dx.doi.org/10.1071/aj11078.

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A resurgent interest in the gas potential of the Gulf of Papua has been enhanced by the recent announcement of developing new LNG facilities in Port Moresby. Petroleum Geo-Services (PGS) has recently acquired a 6,000-km2Multi-Client 3D (MC3D) survey in the gulf. Although most of the discoveries in PNG are from the highland areas, the gulf is a proven hydrocarbon province with gas/condensate accumulations previously discovered in several reef build-ups. It is thought that sediments from the Papuan Fold Belt produced clastic dominated deltas in the Gulf area. Although this play is untested offshore, there is evidence these sandy facies exist and could contain hydrocarbons. On the first phase of acquisition/interpretation, an efficient screening workflow called Prospect Scanner, developed to highlight areas of AVO effects in large 3D seismic datasets, was tested. It uses pre-stack seismic time migrated (PSTM) gathers to extract AVO attributes that are then inverted to derive relative acoustic and shear impedance volumes. Using idealised cross-plots, the relationship between Vp/Vs ratio and the Ip values gives a good indication of the fluid and lithology of the tested interval. The results are loaded into a conventional interpretation package for interpretation/visualisation. Prospect Scanner has highlighted previously undrilled turbidite and basin floor fan prospects in the region. The Vp/Vs versus Ip cross-plot shows clustering ofthe sand anomaly and good separation from the majority of the plot. These points correspond to the idealised location for a gas sand. Past concerns about lateral prediction of reservoir presence and quality associated with the basin floor fans can be addressed through this workflow.

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10

Hobson, D. M. "A THIN SKINNED MODEL FOR THE PAPUAN THRUST BELT AND SOME IMPLICATIONS FOR HYDROCARBON EXPLORATION." APPEA Journal 26, no. 1 (1986): 214. http://dx.doi.org/10.1071/aj85021.

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In the Papuan thrust belt the main risk in hydrocarbon exploration lies in identifying structural traps which are detached below the level of the primary reservoir. Because of the difficulty in obtaining usable seismic in the remote, inaccessible terrain, identification of prospects has been based on the interpretation of structural cross-sections drawn from geological maps. The structural models commonly used have been geometrically inadmissible, and as a result, some wells have penetrated thrusts at depth, before reaching the reservoir horizon.More rigorously constrained regional cross sections through the thrust belt may be constructed using the principles of thin skinned tectonics. These may be used to identify structural provinces, characterised by different types of thrust pattern. In turn, the probability of reservoir involvement in a particular structure is directly related to its location in a particular province.The cross-sections show that there has been as much as 100 km of shortening in the hinterland of the thrust belt. Restored versions of the cross sections may be used to reconstruct the shape of the basin and ideally to identify regions favourable for source and reservoir sediment distribution. In Papua New Guinea, palinspastic maps are currently feasible only for Miocene strata, but with the present level of exploration activity increased stratigraphic information should soon permit reconstructions for older formations.

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11

McConachie, B. A., P. W. Stainton, M. G. Barlow, and J. N. Dunster. "THE OFFSHORE CARPENTARIA BASIN-GULF OF CARPENTARIA, NORTH QUEENSLAND." APPEA Journal 34, no. 1 (1994): 614. http://dx.doi.org/10.1071/aj93047.

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The Carpentaria Basin is late Jurassic to early Cretaceous in age and underlies most of the Gulf of Carpentaria and surrounding onshore areas. The Carpentaria Basin is stratigraphically equivalent to the Eromanga and Papuan Basins where similar reservoir rocks produce large volumes of hydrocarbons.Drillholes Duyken–1, Jackie Ck–1 and 307RD12 provide regional lithostratigraphic and tectonic control for the Q22P permit in the offshore Carpentaria Basin. Duyken–1 penetrated the upper seal section in the Carpentaria Basin and a full sequence through the overlying Karumba Basin. Jackin Ck–1 intersected the lower reservoir units and a condensed upper seal section of the Carpentaria Basin. Coal drillhole 307RD12 tested the late Jurassic to early Cretaceous reservoir section in the Carpentaria Basin and also intersected an underlying Permian infrabasin sequence.Little is known of the pre Jurassic sedimentary section below the offshore Carpentaria Basin but at least two different rock packages appear to be present. The most encouraging are relatively small, layered, low velocity, channel and half-graben fill, possibly related to Permian or Permo-Triassic sedimentary rocks to the east in the Olive River area. The other packages consist of poorly defined, discontinuous, high velocity rocks believed to be related to those of the Bamaga Basin which have been mapped further north.During the period 1990-1993 Comalco Aluminium Limited reprocessed 2188 km of existing seismic data and acquired 2657 km of new seismic data over the offshore Carpentaria Basin. When combined with onshore seismic and the results of drilling previously undertaken by Comalco near Weipa on northwestern Cape York Peninsula, it was possible to define a significant and untested play in the Carpentaria Depression, the deepest part of the offshore Carpentaria Basin.The main play in the basin is the late Jurassic to early Cretaceous reservoir sandstones and source rocks, sealed by thick early Cretaceous mudstones. Possible pre-Jurassic source rocks are also present in discontinuous fault controlled half-grabens underlying the Carpentaria Basin. New detailed basin modelling suggests both the lower part of the Carpentaria Basin and any pre Jurassic section are mature within the depression and any source rocks present should have expelled oil.

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12

MANIK, HOTLAN, HUSMY YURMIATY, INDRAWATI YUDHA ASMARA, HANDARTO HANDARTO, JOHAN ISKANDAR, and RUHYAT PARTASASMITA. "Wattled Brushturkey hunting system in the Sigim and Sinaitousi communities in the buffer zone of the Arfak Mountain Nature Reserve, West Papua, Indonesia." Biodiversitas Journal of Biological Diversity 19, no. 3 (May 1, 2018): 849–56. http://dx.doi.org/10.13057/biodiv/d190313.

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Manik H, Yurmiaty H, Asmara IY, Handarto, Iskandar J, Partasasmita R. 2018. Wattled Brushturkey hunting system in the Sigim and Sinaitousi communities in the buffer zone of the Arfak Mountain Nature Reserve, West Papua, Indonesia. Biodiversitas 19: 849-856. Illegal hunting is still the cause of the decline of wildlife populations in nature. This is particularly the case with protected wildlife and endemic species, such as the Wattled Brushturkey in Palau West Papuan. Thus, research needs to be done on the hunting system at the site. The aim of this research was to know Wattled Brushturkey (Aepypodius arfakianus) hunting system by Sigim and Sinaitousi villagers, Arfak Mountains of West Papua. The research used descriptive method with field observation technique and semistructured interviews. The results showed that the main purpose of hunting Wattled Brushturkey conducted by the Sigim and Sinaitousi communities is to consume the meat, while a part of egg hunting is for sale. The hunting by the two villagers was generally done in groups. The frequency of hunting depends on needs and demand. Hunting is done using snares, dogs, and combinations of snares and dogs. The tools used are snares, machetes, air rifles, arrows nad bows. The modern tools such as gun have been used in both villages. The hunting of Wattled Brushturkey begins in the morning and continues until late afternoon. The location of hunting is usually primary forest, secondary forest of former garden and river basin.

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13

Harrington, Amanda, Cyrille Reiser, Bob Burmaz, and Rod Reed. "Amplitude-versus-offset (AVO) screening in frontier basins: an example from the Gulf of Papua, Papua New Guinea." APPEA Journal 52, no. 2 (2012): 701. http://dx.doi.org/10.1071/aj11115.

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A resurgent interest in the gas potential of the Gulf of Papua has been enhanced by the recent announcement of developing new LNG facilities in Port Moresby. Petroleum Geo-Services (PGS) has recently acquired a 6,000-km2 Multi-Client 3D (MC3D) survey in the gulf. Although most of the discoveries in PNG are from the highland areas, the gulf is a proven hydrocarbon province with gas/condensate accumulations previously discovered in several reef build-ups. It is thought that sediments from the Papuan Fold Belt produced clastic dominated deltas in the Gulf area. Although this play is untested offshore, there is evidence these sandy facies exist and could contain hydrocarbons. On the first phase of acquisition/interpretation, an efficient screening workflow called Prospect Scanner, developed to highlight areas of AVO effects in large 3D seismic datasets, was tested. It uses pre-stack seismic time migrated (PSTM) gathers to extract AVO attributes that are then inverted to derive relative acoustic and shear impedance volumes. Using idealised cross-plots, the relationship between Vp/Vs ratio and the Ip values gives a good indication of the fluid and lithology of the tested interval. The results are loaded into a conventional interpretation package for interpretation/visualisation. Prospect Scanner has highlighted previously undrilled turbidite and basin floor fan prospects in the region. The Vp/Vs versus Ip cross-plot shows clustering of the sand anomaly and good separation from the majority of the plot. These points correspond to the idealised location for a gas sand. Past concerns about lateral prediction of reservoir presence and quality associated with the basin floor fans can be addressed through this workflow.

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14

Boult, P. J. "A review of the petroleum potential of Papua New Guinea with a focus on the eastern Papuan Basin and the Pale Sandstone as a potential reservoir fairway." Geological Society, London, Special Publications 126, no. 1 (1997): 281–91. http://dx.doi.org/10.1144/gsl.sp.1997.126.01.17.

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15

Gardien, Véronique, Christophe Lécuyer, and Jean-François Moyen. "Dolerites of the Woodlark Basin (Papuan Peninsula, New Guinea): A geochemical record of the influence of a neighbouring subduction zone." Journal of Asian Earth Sciences 33, no. 3-4 (July 2008): 139–54. http://dx.doi.org/10.1016/j.jseaes.2007.12.003.

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16

Petkovski, Maki, and Keith Bradey. "The success of pre-stack depth migration over the Anama structure in the Papuan Foreland Basin, PNG: a case history." ASEG Extended Abstracts 2001, no. 1 (December 2001): 1–4. http://dx.doi.org/10.1071/aseg2001ab108.

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17

O’SHEA, MARK, and STEPHEN J. RICHARDS. "A striking new species of Papuan groundsnake (Stegonotus: Colubridae) from southern Papua New Guinea, with a dichotomous key to the genus in New Guinea." Zootaxa 4926, no. 1 (February 4, 2021): 26–42. http://dx.doi.org/10.11646/zootaxa.4926.1.2.

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We describe a new species of groundsnake of the genus Stegonotus (Colubridae) from the Purari River basin in Gulf Province, Papua New Guinea. The new species can be most readily distinguished from all other New Guinean Stegonotus by its unique dorsal colour pattern which consists of a dark head and creamy-white anterior one third to two thirds of the body, grading into increasingly dense dark pigmentation on the posterior of the body and tail. It is most similar to S. iridis from the Raja Ampat Archipelago off western New Guinea, but that species has a different pattern of pigmentation dorsally, has a lower ventral scale count (198–211 vs. 229–239), and exhibits a different temporal scale arrangement. The description of S. aplini sp. nov. brings to fourteen the number of Stegonotus species described from New Guinea. A dichotomous key to described species in the New Guinea region is provided.

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18

Nelson, Andrew, David Holland, O’karo Yogi, Rodrigo Heidorn, and Desmond Leech. "Integrated use of Seismic, Ground and Airborne Gravity/Gravity Gradiometer, and Ground Geological Mapping Methods in the Eastern Papuan Basin, PNG." ASEG Extended Abstracts 2004, no. 1 (December 2004): 1–4. http://dx.doi.org/10.1071/aseg2004ab107.

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19

Dika, Alam Maha. "Nasionalisme Papua Dalam Organisasi Aliansi Mahasiswa Papua (Studi Kasus : Aliansi Mahasiswa Papua Komite Kota Yogyakarta)." Jurnal DinamikA 1, no. 2 (December 1, 2020): 33–54. http://dx.doi.org/10.18326/dinamika.v1i2.33-54.

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The Papuan Student Alliance (AMP) is a Papuan student organization that voices problems in Papua, especially politics. AMP has goals for Papuan independence which are contained in the organization's vision and platform. AMP itself is divided into seven committees in various cities, one of which is the Yogyakarta City Committee. The results of this study conclude that the Papuan nationalism that has developed within the Yogyakarta KK AMP is due to several reasons, among others; 1) Indonesia is considered a failure in carrying out nation-building in Papua; 2) Experience of violence experienced by the Papuan people; 3) The basic needs of the Papuan people are not fulfilled. Apart from the historical factor of Papua which has a strong connection with Papuan nationalism, the failure of nation-building by Indonesia in Papua is also a factor that makes Papuan nationalism continue to develop in the Yogyakarta KK AMP. In the construction of Papuan nationalism, the Yogyakarta KK AMP builds a shared identity through shared psychology regarding the oppression experienced by the Papuan people so far. The joint history that was formed by the AMP KK Yogyakarta is about Papua which has made efforts to become independent and then this independence was annexed by Indonesia. For the AMP KK Yogyakarta, the Papuan people have experienced violence (memoria passionis), land grabbing, exploitation of natural resources, discrimination, marginalization, and the crisis of freedom. Therefore, the common goal of AMP KK Yogyakata is Papuan independence as an initial stage towards a better Papua.

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20

George, Simon C., Herbert Volk, Manzur Ahmed, Walter Pickel, and Tony Allan. "Biomarker evidence for two sources for solid bitumens in the Subu wells: Implications for the petroleum prospectivity of the East Papuan Basin." Organic Geochemistry 38, no. 4 (April 2007): 609–42. http://dx.doi.org/10.1016/j.orggeochem.2006.12.002.

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21

Furnas, MJ, and AW Mitchell. "Pelagic primary production in the Coral and southern Solomon Seas." Marine and Freshwater Research 47, no. 5 (1996): 695. http://dx.doi.org/10.1071/mf9960695.

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Phytoplankton primary production was measured around the periphery of the Coral Sea during October 1985 and in the boundary current systems bordering the northern Australian Great Barrier Reef (GBR) and Papuan Barrier Reef (PBR) during October 1985 and June-July 1988. Under strong wind conditions (mean winds 8-12 m s-1), the north-western Papuan Barrier Reef region was characterized by a shallow surface mixed layer, shallow nutriclines (25-75 m) and shallow subsurface chlorophyll maxima. Under low wind stress conditions (mean winds <5 m s-1), the southern and western Coral Sea were also characterized by a shallow surface mixed layer and stable underlying density profiles but deep (>I00 m) nutriclines and deep (60-125 m) subsurface chlorophyll and primary production maxima. Regardless of location, most primary production occurred above the 20% mid-day isolume surface. Phytoplankton standing crop and primary production in all regions were dominated by picoplankton (<2 μm size fraction). Very high primary production rates (1-3 g C m-2 day-1) were measured at a number of stations adjacent to the western margin of the PBR and within the central basin of the Louisiade Archipelago. Evidence for upwelling along the western margin of the PBR was observed under both north-easterly (normal to the reef axis) and south-easterly (parallel to the reef axis) wind regimes; however, surface outcropping of upwelled water did not occur. Oceanic primary production in the Coral Sea is estimated to be between 100 and 200 g C m-2 year-1. Primary production in and around the Louisiade Archipelago appears to be on the order of 200-300 g C m-2 year-1. Near-surface chlorophyll standing crop was generally better correlated with near-surface primary production than was total chlorophyll with total areal primary production.

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22

Flassy, Don Augustinus Lamaech. "Prestige and Powers of "The World Big Power'', Tanah Papua as Specific Case." Journal of Education and Vocational Research 9, no. 1 (November 30, 2018): 23–43. http://dx.doi.org/10.22610/jevr.v9i1.2559.

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The article, Prestige and Powers of "The World of Big Power'', Tanah Papua as Specific Case, the author intends for Subtopic to two and at the same time can also to accommodate the third problem of formulation being raised in dissertation entitled: " Re-Roadmap of the Papuan in State of Papua Courant West : â€œA Peaceful Solution Recovering of Identityâ€. That is by treading Returning Roadmap, referring to Unilateral Declaration of Independence/UDI of the Papua Nation and the Federal Republic of West Papua/NRFPB on October 19, 2011. The study describes in five main topics, namely, (1) Defining "Hidden Structure" in Melanesian-Papua Social Cultural highlighting Papuanistiecs and Melanesianology; (2) Prestige and Powers of â€œThe World Big Power'', Tanah Papua as Specific Case, reveals how the influence of â€The Giant Powersâ€ to the problem of Papua; (3) Federalism in Indonesia revealing Melanesian-Papua in Tanah Papua as Special Case versus the Unitary Republic of Indonesia; (4) Constitution vis-Ã -vis Constitution illustrates the philosophical correlation among Indonesian constitution 1945 versus Papua constitution 1999; (5) Unilateral Declaration/UDI of the Papua Nation and NRFPB on October 19, 2011. The background of the study is based on two keys of Morgenthou thoughts: First, Morgenthou (2012) confirmed that, during the 17 years from 1945 to 1962, the process to Indonesia-nizing the Papuans are generally still in the stage of seeding while growing only in some urban areas and the government center. Awareness to be Indonesian-ness was yet to reach all areas of Papua. Morgenthou (2012) that the presence of all Indonesia's past greatly influenced the policies and the approach taken by both the Dutch and Indonesian government through the nationalistâ€™s initiators role at that time. Second, study of LIPI in 2007 (Soewarsono, ed.) is still questions to the Indonesian-ness of Papuans reinforces the view of Morgenthou (2012), which states that the process to Indonesian-ness among Papuans still weak. Morgenthou concluded that, in fact, to understand the history of Papua will become a basic reference for the government seek and find out the right way and dignified in overcoming the issues of Papua, though on the other hand George Junus Aditjondro, 1999 clamming, the Government and Important People of Indonesia has curled the history of Papua which by the Papuans wanting to be straightened out: "This is the dark history of Papua in Indonesian Historiography". Thoughts of Morgenthou strengthens the authors thought that the various problems occurred in Papua, especially the facts involve "Merdeka Papua". Referring to the failure of Indonesia-nizing of the Papuans, it appears that it is not necessary regrettable because in fact, they are different by nature or in the growth process since in the hands of Dutch colonial control of the Dutch East Indies (for Papua 1826-1949-1962). Precisely when indecision of the President of Indonesia to the case of Papua was safe step into alternative measures of the Melanesian-Papua themselves must be hacked through, UDI of Papuan Nation and NRFPB on October 19, 2011. The research focuses on studies of literature and interviews by the method of Descriptive Analysis and to assemble the Hidden Structure and Correlation Studies to reflect the relationships between aspects on the basis of Motivation Theory, Theory of Conflict, Theory of Social Change and Theory of Balance and Theory of Realist implied through sub-theories positioned as tools to characterize, recognize, and understanding as well as tools to analyze (dissect) the problems issues to be raised in this written work. In connection with this, the author is improving the nature of Hidden Structure as Grand Theory. Formulations of the problems might be: (1). How to understand the present of the Melanesian-Papua in Tanah Papua? (2). May the existence of Papua to be returning to the attention of Prestige and Powers of "The World Big Power" for its political status to be reviewed at the UN? (4). Whether, the Melanesian-Papua and the Indonesian in Tanah Papua can together according to the federalist order of Melanesian-Papua? (4). How is the condition of Indonesian society and customs of Melanesian-Papua can be brought together to create a bilateral solidarity for the multilateralbeneficial and usefulness?

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23

Putro, Kristian Hariyono. "PERENCANAAN PEMBANGUNAN DI PAPUA DAN BONUS DEMOGRAFI 2020 (DEVELOPMENT PLANNING IN PAPUA AND DEMOGRAPHIC BONUS 2020)." Jurnal Tata Kelola & Akuntabilitas Keuangan Negara 2, no. 1 (June 29, 2016): 49. http://dx.doi.org/10.28986/jtaken.v2i1.37.

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ABSTRAKPerubahan demografi dan cepatnya modernisasi yang mengakibatkan tergusurnya penduduk asli Papua telah memicu antipati serta tuntutan untuk merdeka. Para pendatang dengan pendidikan yang lebih baik mendominasi pasar ekonomi dan dalam prosesnya menyisihkan penduduk lokal dari keuntungan ekonomi dan kesejahteraan. Perpindahan penduduk dalam skala besar yang disebut ‘program transmigrasi’ ke Papua juga mendorong timbulnya perasaan identitas yang terenggut diantara penduduk asli. Seluruh proses tersebut membangun persepsi bersama bahwa mereka menghadapi pemusnahan ras, atau paling tidak ancaman serius atas kelangsungan demografi dan budaya mereka. Di sisi lain, diprediksikan bahwa kebijakan penurunan tingkat kelahiran akan membawa kesempatanbagi Indonesia mengalami ‘bonus demografi’ pada tahun 2020-an. Esai ini akan fokus ke Papua karena kompleksitas masalahnya di berbagai bidang seperti ekonomi, pendidikan serta kesehatan yang timbul seiring perubahan demografi. Memanfaatkan data sekunder dari Sensus Penduduk terakhir pada tahun 2010 yang diolah dengan program Stata, esai ini menggunakan metode komparasi untuk mengetahui perbandingan komposisi demografi di Papua dan menganalisa secara deskriptif sumber-sumber data terkait. Sebagai simpulan,memang terdapat ketimpangan dalam komposisi demografi masyarakat Papua yang dapat menghambat kesempatan menikmati bonus demografi 2020. Esai ini menyarankan agar pemerintah merevitalisasi program keluarga berencana yang fokus kepada partisipasi perempuan untuk mencapai rasio 2,1 kelahiran per perempuan. Pemerintah juga hendaknya membuat kebijakan yang ditujukan untuk meningkatkan akses masyarakat asli Papua ke pelayanan dasar seperti pendidikan dan fasilitas kesehatan.Kata Kunci: ABSTRACTDemographic change and rapid modernization that resulted in the displacement and dislocation of indigenous Papuan, has been stimulating their antipathy and demand for independence. Better educated settlers have dominated the growing market-economy and sidelined local people from the benefits of economics and welfare. Large scale flows of migration have also drive a sense of identity being wrenched among Papuans. Together these processes have given rise to a collective perception that Papuans are facing a serious threat over their demographic and cultural survival. On the other hand, it was projected that in 2020s, lower fertility rate policy will bring opportunity to Indonesia experiencing ‘demographic bonus’. This essay will focus on Papua Island due to its problems complexity in many sectors that arise along with demographic change. Using secondary data of population census 2010, this essay adopts comparation method to find demographic composition in Papua and analyze the data descriptively. In conclusion, there is inequality in Papua’s demographic composition which could challenge the opportunity of demographic bonus 2020. This essay recommends The government to revitalize family planning program which focus on women and girls participation to reach 2.1 fertility rates. The government should also execute policies which aimed to increase access of indigenous Papuans to basic services such as education and health facilities.Keywords: Demographic bonus, fertility rate, inequality,HDI, migration, family planning.

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Flassy, Don Augusthinus Lamaech. "Seeking for Recovering Their Identity: The Melanesian-Papua Treading Returning Roadmap." Journal of Social and Development Sciences 8, no. 1 (April 24, 2017): 37–47. http://dx.doi.org/10.22610/jsds.v8i1.1617.

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The study describes 5 main areas, namely, (1)"Hidden Structure" that in the Social Meaning of Melanesian-Papua Cultural highlights Papuanistiecs and Melanesianology; (2) The Prestige and Power exposes the influence of the Big World Power to the problem of Papua; (3) Federalism in Indonesia reveal to the Melanesian-Papua in Land Papua as Special Specific Case versus unitary of The Republic of Indonesia; (4) Constitution vis-Ã -vis Constitution on constitutional philosophical correlation Indonesia constitution 1945 versus Papua constitution 1999; (5) Unilateral Declaration of Independence/UDI October 19, 2011, concerning Freedom-Melanesian Papuans in Land Papua as Nation and State. The background of this study is based on two main thoughts keys, namely: First, Meteray (2012: 268, 2013: 4) confirmed that, during the 17 years from 1945 to 1962, the process to Indonesian-sizing the Papuans are generally still in the stage of seeding while growth only in some areas of government and urban centresâ€™. Awareness to be Indonesian-ness is yet to reach all areas of Papua. Meteray adding that the presence of Indonesian-sizing in past greatly influenced by the policies and the approach taken by both the Dutch and Indonesian government through the role of nationalists initiators of the period (2012: 264-267); Second; LIPI study in 2007 (Soewarsono, ed) are still questions to the Indonesian-sizing of the Papuans reinforce the view of Meteray stated that it is to Indonesian-sizing among the Papuans still weak (Meteray 2013: 1). Meteray concluded that, in fact, to understand the history of Papua will become a basic reference for the government seek and find out the right way and dignified in overcoming the issues of Papua, though on the other hand Aditjondro, 1999 clamming, the Government and Important People of Indonesia has curled the history of Papua which by the Papuans wanting to be straightened out, He calls this act as: "The dark history of Papua in Indonesian Historiography". Thoughts of Meteray and Aditjondro strengthens the authors thought that the various problems occurred in Papua, especially the facts involves "M"/Merdeka (Freedom) Papua". Referring to the failure of Indonesian-sizing of the Papuans, it appears that it is not necessary regrettable because in fact, they are different. Precisely when indecision of the President of Indonesia to the case of Papua is safe step into alternative measures of the Melanesian-Papua people themselves must be hacked through, UDI October 19, 2011. This research focuses on the study of literature and interviews with the method of Descriptive Analysis and Method of Structure Linkage to assemble the Hidden Structure and Correlation Studies to reflect the relationships between aspects on the basis of Motivation Theory, Theory of Social Change and Theory of Balance and Theory of Realist and related by make use of Hidden Structure as Grand Theory. The formulation of the problem is (1). How to understand the present of Melanesian-Papuans in Land Papua? (2). Whether existing of Papua as "trust territory" of the UN is still attracting the winning of Prestige and Power of "the Big Power of the World" to be back to discusses at the UN of a future in accordance with Article 74 and Article 78 of the UN Charter? (3). Whether, Melanesia-Papua and Indonesian in Papua can together according to the federalist order of Melanesian-Papua? (4). How is the condition of social customs and traditions of Indonesia and Papua can be met?

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Mesak, Marinus, Yanyan Mochamad Yani, and Windy Dermawan. "CHINESE INVOLVEMENT IN VANUATU AND SOLOMON ISLAND FOREIGN POLICY AGAINST THE PAPUA ISSUE." Sociae Polites 21, no. 1 (June 30, 2020): 95–110. http://dx.doi.org/10.33541/sp.v20i2.1931.

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The influence of China in the Pacific region increases due to the Belt and Road Initiative (BRI) program that focuses its assistance and soft loans on the development of basic infrastructure and other supporting infrastructure. Increased economic influence has an impact on changes in regional geopolitical maps. China appears to be increasingly dominant in influencing the foreign policy of the region’s countries, including China’s involvement in controlling Vanuatu and Solomon Island’s foreign policy. At present, the issue of Papua is on the main agenda of Vanuatu and Solomon Island’s foreign policy. Significant funds are needed to finance the process of advocating for the issue of Papua in the Pacific region and the international community. One source of funding comes from Chinese aid. This article will review China’s position as a source of the financing for the Papuan separatist movement based in Vanuatu and Solomon Islands, by using a power approach and economic diplomacy. Keywords: China, Belt, and Road Initiative, economic, diplomacy, Power, Vanuatu, Solomon Island, and Internationalization of Papuan Issues.

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De Quelyoe, Flora Yvonne, Sarlota Ratang, and Christine Marina Wakarmamu. "The Impact of Poverty Reduction Program into Papuan Women Economy Behavior in District of Kemtuk Gresi, Jayapura Regency (Case Study)." Journal of Education and Vocational Research 7, no. 2 (August 1, 2016): 41–46. http://dx.doi.org/10.22610/jevr.v7i2.1338.

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Based on The Intenasional Summit which had launced the 8th important issues on Millenium Development Goals (MDGs), is very usefull to improve the communitylife. The quality of womenâ€™s life has been one of basic aspects to build sustainable development of a nation (Khofifah, 1998). Sustainable development can take place if the entire communities (men and women) being optimally involved in whole development program with using efficient and effective principles. The quality of life is largerly determined by formal and non formal education, both poor degree of health and nutrition, buruknya derajat kesehatan dan gizi, and also the presence of accessbility to development resources. Those factors mentioned above are mutual supporting and can not be separated from one another. Although, development activity in Papua Province is growing up, the society is still livingin the cycles of poverty, especially for women in District of Kemtuk Gresy, Jayapura Regency, Province of Papua. The aims of the study are : 1) to know the impact of Poverty Reduction Program (into the changing of economy behavior of Papuan Women in Kemtuk Gresi, Jayapura Regency, Papua Province; 2) to explore how Poverty Reduction Program influenced the generating income of Papuan Women. The methods of data collection are in-depth interview to 150 respondents, and 5 key informants (Community, Traditional, Religion, Women, and Youth Leaders), and observation as well. In order to find the answer, is using descriptive qualitative. The result of the first research question indicated that in terms of Changing of economic behavior: 34 percent of Papuan Women in Kemtuk Gresi are changing their economic behavior, mainly their production and marketing strategy; whereas 66 percent of respondents are still in traditional way for production and marketing. The second result is 38 percent of respondentâ€™s income is increasing, and 44 percent respondents are remains static or even volatile, finally, 18 percent respondents are going out from economic activities, because of missing capital of business. Starting from the result, we can give some recommendations: 1) changing economic behavior should be started from young people, so all parties should participate intensively to push young women entrepreneur to engage in business activity; 2) the government should involve traditional leaders to support women entrepreneurs by providing a piece of land or other forms of capital.

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Warami, Hugo. "INTEGRASI ILMU LINGUISTIK DALAM WACANA POLITIK UNDANG-UNDANG OTONOMI KHUSUS PAPUA: PERSPEKTIF STUDI MORFOLOGI." CaLLs (Journal of Culture, Arts, Literature, and Linguistics) 4, no. 1 (June 25, 2018): 65. http://dx.doi.org/10.30872/calls.v4i1.1296.

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This study is part of an effort to understand the true value of basic philosophy that is revealed behind the law is really very meaningful in finding the words and concepts to describe the meaning of a text of the law. The provision of a special autonomy space for Papua is seen as a new sign that becomes a beacon within nationalists from the threat of Papuan nationalist groups (separatists and federalists) who are constantly creating new signs in the social semiotics space in Papua. Language as the home of life, capable of echoing and symbolized as a form of resurrection that is ready to threaten the unitary state system. The purpose of this study is to uncover political discourse in the text of law number 21 on Special Autonomy of Papua laden with linguistic nuances (morphology) which is not only what is understood, but the understanding itself is essentially linguistic as well. The method used in this research refers to qualitative method with descriptive research type which serves to present a detailed picture about a particular situation, social background, relationship, class or certain characteristic in Papua Special Autonomy Law. The main data in this study is the writing data (main) which is derived from the text of the Special Autonomy Law of Papua. The qualitative data derived from the text of the law in the form of words, phrases, clauses and sentences that provide an overview of the integration of morphological studies can then be described and explored in their meaning according to their use in the text.

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Ontosari, David, Benyamin Sapiie, Hermes Panggabean, and Eddy Slameto. "Basin Geometry Analysis of "NOKEN" Area, Mesozoic Interval, Akimeugah Basin, Papua." Bulletin of Geology 2, no. 2 (September 2018): 229–42. http://dx.doi.org/10.5614/bull.geol.2018.2.2.3.

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Barlow, Russell. "Agent demotion through inverted word order." Studies in Language 43, no. 4 (December 31, 2019): 1015–37. http://dx.doi.org/10.1075/sl.19010.bar.

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Abstract Passivization has been characterized as a strictly morphological phenomenon. Some definitions of passivization even require the passive construction to exhibit special verbal morphology. Increasingly, however, there have been descriptions of languages that have “morphology-free” passive constructions. This paper presents data from Ulwa, a Papuan language of the Sepik region of Papua New Guinea, which forms its passive constructions through a syntactic operation. Specifically, passives are formed through the inversion of subject and predicate. Whereas the canonical transitive active sentence in Ulwa has the basic constituent order SOV, the corresponding passive sentence has the order VS, where the S of the passive corresponds to the O of the active. Agent arguments are optional; when they do appear in passive constructions, they are marked as obliques. The Ulwa data support claims that it is possible for passivization to be a syntactic phenomenon that operates on the level of the clause.

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Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, Hermes Panggabean, Iyan Haryanto, Eko Budi Lelono, Juwita Trivianty Musu, and Panuju Panuju. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (February 25, 2019): 37. http://dx.doi.org/10.33332/jgsm.2019.v20.1.37-47.

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North Papua Basin is a fore arc basin located in northern coastal of Papua Island. This basin filled by Middle-Upper Miocene turbidite sediment and overlied by Upper Miocene – Quarternary clastic sediment. Upper Miocene – Quaternary clastic sediments (Mamberamo Formation) composed by interbedding conglomerate, sandstone and shale as molasses deposit. A detailed stratigraphic study was performed to identify facies and its association of the Mamberamo Formation to that give a new perspective on the characteristics and development of facies succession of Lower Mamberamo Formation. Result shows that the Lower Mamberamo Formation consists of three facies: A) cross bedding sandstone (subtidal), B) heterolothic silty shale (intra-tidal), C) carbonaceous shale (supra-tidal) deposited on Late Miocen to Plio-Pleistocene during centra range orogeny (syn-orogeny) as molasses deposits.Keywords: Fore arc basin, North Papua Basin, Mamberamo Formation, molasse deposits.

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Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, Hermes Panggabean, Iyan Haryanto, Eko Budi Lelono, Juwita Trivianty Musu, and Panuju Panuju. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (February 25, 2019): 37. http://dx.doi.org/10.33332/jgsm.geologi.20.1.37-47.

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North Papua Basin is a fore arc basin located in northern coastal of Papua Island. This basin filled by Middle-Upper Miocene turbidite sediment and overlied by Upper Miocene – Quarternary clastic sediment. Upper Miocene – Quaternary clastic sediments (Mamberamo Formation) composed by interbedding conglomerate, sandstone and shale as molasses deposit. A detailed stratigraphic study was performed to identify facies and its association of the Mamberamo Formation to that give a new perspective on the characteristics and development of facies succession of Lower Mamberamo Formation. Result shows that the Lower Mamberamo Formation consists of three facies: A) cross bedding sandstone (subtidal), B) heterolothic silty shale (intra-tidal), C) carbonaceous shale (supra-tidal) deposited on Late Miocen to Plio-Pleistocene during centra range orogeny (syn-orogeny) as molasses deposits.Keywords: Fore arc basin, North Papua Basin, Mamberamo Formation, molasse deposits.

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Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, Hermes Panggabean, Iyan Haryanto, Eko Budi Lelono, Juwita Trivianty Musu, and Panuju Panuju. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (February 25, 2019): 37. http://dx.doi.org/10.33332/jgsm.geologi.v20i1.399.

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North Papua Basin is a fore arc basin located in northern coastal of Papua Island. This basin filled by Middle-Upper Miocene turbidite sediment and overlied by Upper Miocene – Quarternary clastic sediment. Upper Miocene – Quaternary clastic sediments (Mamberamo Formation) composed by interbedding conglomerate, sandstone and shale as molasses deposit. A detailed stratigraphic study was performed to identify facies and its association of the Mamberamo Formation to that give a new perspective on the characteristics and development of facies succession of Lower Mamberamo Formation. Result shows that the Lower Mamberamo Formation consists of three facies: A) cross bedding sandstone (subtidal), B) heterolothic silty shale (intra-tidal), C) carbonaceous shale (supra-tidal) deposited on Late Miocen to Plio-Pleistocene during centra range orogeny (syn-orogeny) as molasses deposits.Keywords: Fore arc basin, North Papua Basin, Mamberamo Formation, molasse deposits.

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Mamengko, David Victor, Yoga B.Sendjadja, Budi Mulyana, Hermes Panggabean, Iyan Haryanto, Eko Budi Lelono, Juwita Trivianty Musu, and Panuju Panuju. "Perkembangan Fasies Sedimen Formasi Mamberamo Berumur Miosen Akhir-Pliosen di Cekungan Papua Utara." Jurnal Geologi dan Sumberdaya Mineral 20, no. 1 (February 25, 2019): 37. http://dx.doi.org/10.33332/jgsm.v20i1.399.

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North Papua Basin is a fore arc basin located in northern coastal of Papua Island. This basin filled by Middle-Upper Miocene turbidite sediment and overlied by Upper Miocene – Quarternary clastic sediment. Upper Miocene – Quaternary clastic sediments (Mamberamo Formation) composed by interbedding conglomerate, sandstone and shale as molasses deposit. A detailed stratigraphic study was performed to identify facies and its association of the Mamberamo Formation to that give a new perspective on the characteristics and development of facies succession of Lower Mamberamo Formation. Result shows that the Lower Mamberamo Formation consists of three facies: A) cross bedding sandstone (subtidal), B) heterolothic silty shale (intra-tidal), C) carbonaceous shale (supra-tidal) deposited on Late Miocen to Plio-Pleistocene during centra range orogeny (syn-orogeny) as molasses deposits.Keywords: Fore arc basin, North Papua Basin, Mamberamo Formation, molasse deposits.

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Kusnida, Dida, and Tommy Naibaho. "LATE NEOGENE SEISMIC STRUCTURES OF THE SOUTH BATANTA BASIN, WEST PAPUA." BULLETIN OF THE MARINE GEOLOGY 29, no. 1 (February 15, 2016): 11. http://dx.doi.org/10.32693/bomg.29.1.2014.61.

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Study on multi-channel seismic records from South Batanta Basin, West Papua acquired during RV Geomarin III cruise in 2013 were aimed to invent and map geological aspects and for geo-tectonic and geological history studies. Seismic data indicate that sediment sequences which can be observed from our seismic system in the study area are characterized by pre-extension sediments (Lower Early Miocene-Upper Early Pliocene), syn-extension sediments (Lower Middle Pliocene-Upper Late Pliocene), post-extension sediments (Early Pleistocene), and syn-inversion sediments (Late Pleistocene-Recent) typical of the West Papua tectonic system. In the study area, sediment sequences are possibly characterized by clastical sedimentary cover such as slumps, debrites and turbidites. Key words: South Batanta Basin, seismic sequence, tectonic, faults, clastical sediments. Studi rekaman seismik multi kanal dari Cekungan Batanta Selatan, Papua Barat yang diperoleh selama pelayaran KR Geomarin III pada tahun 2013 bertujuan untuk menginventarisir dan memetakan aspek-aspek geologi serta untuk studi geo-tektonik dan sejarah geologi. Data seismik menunjukkan bahwa urutan sedimen yang dapat diamati dari sistem seismik di daerah studi ditandai oleh sedimen pra-ekstensi (Miosen Awal Bagian Bawah-Pliosen Awal Bagian Atas), sedimen syn-ekstensi (Pliosen Tengah Bagian Bawah-Pliosen Akhir Bagian Atas), sedimen post-ekstensi (Plestosen Awal), dan sedimen syn-inversi (Pleistosen Akhir-Resen) tipikal sistem tektonik Papua Barat. Di daerah studi, urutan sedimen dicirikan oleh sedimen penutup klastika kemungkinan berupa slump, debrit dan turbidit. Kata kunci: Cekungan Batanta Selatan, sekuen seismik, tektonik, sesar, sedimen klastika.

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Alexander, Michael, Robert Marksteiner, and Corine Prieto. "A Prospective Deep Basin in Southern Papua New Guinea?" ASEG Extended Abstracts 2015, no. 1 (December 2015): 1–3. http://dx.doi.org/10.1071/aseg2015ab026.

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Uswanas, Mohammad, Yeremias T. Keban, Agus Heruanto Hadna, and Pande Made Kutanegara. "Kinerja Pendidikan Dasar Setelah Sembilan Tahun Otonomi Asimetris di Provinsi Papua Barat." Populasi 26, no. 2 (September 15, 2019): 61. http://dx.doi.org/10.22146/jp.44150.

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Special Autonomy (Otsus) for Papua and West Papua is expected to improve people’s welfare comprehensively. The implementation of Otsus for Papua and West Papua has emphasized on the development or improvement of education, particularly basic education, particularly the basic education. The granting of Otsus status is accompanied by a sufficient financial supports to conduct development programs in both provinces. However, a question has araised which needed to be answered. Did the large financial support could significantly increase the coverage as well as improve the quality of basic education services in West Papua Province? The purpose of this study is to determine the driving and hindering factors of education performance in West Papua Province by utilizing descriptive-evaluative methods and ex-post facto. Secondary data is obtained from relevant institutions and pimary data is obtained from in-depth interviews, participatory observations, document reviews and Focus Group Discussions (FGD). The study reveals that the policy of asymmetric decentralization education in West Papua Province is far from expectations. Factors that hindered the improvement basic education in West Papua Province are policy implementations, standardization of achievements, regional sovereignity in preparing program plans and action plans. Asides from that were specific factors, such as accessibilty, school proximity, geographical constraints and low dedication of teachers.

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37

Eska-Mikołajewska, Justyna. "Znaczenie modelu westminsterskiego w kształtowaniu się pozycji ustrojowej parlamentu w Papui-Nowej Gwinei." Przegląd europejski 1 (October 5, 2019): 37–56. http://dx.doi.org/10.5604/01.3001.0013.5173.

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The article presents the issues of the political position of the parliament in one of the largest states of the South Pacific subregion – Papua New Guinea. Shaping its legal and political system, the state profoundly derived from the British practice. This process was initiated in the first decade of the 20th century as a result of Australian rule, which had lasted by that time the state gained its independence in 1975. As a consequence, all the basic features of Westminster democracy were adopted, with the unitary form of government and the unicameral parliament. The analysis allowed to indicate that the character of Papuan democracy has evolved over the years, and therefore some elements of the Westminster model have become inadequate and not very effective. These changes concerned mainly superior state structures, including the parliament. It is a body increasingly controlled by the executive nowadays, that lost its original representative character. In this article, the author has adopted the following research methods: an analysis of legal sources and a critical analysis as well as a descriptive method. The text was divided into three main parts, the introduction and the conclusion.

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Triyogo Varianto, Yohanes Ardhito, Sugeng Sapto Surjono, and Salahuddin Salahuddin. "Erosion and its Implication on Hydrocarbon Generation in ‘ARD’ Block, Akimeugah Basin,West Papua." Journal of Applied Geology 4, no. 2 (December 31, 2019): 58. http://dx.doi.org/10.22146/jag.53204.

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Akimeugah Basin in the western part of Aru Trough is included as a Paleozoic Basin which is one of the potential hydrocarbon-producing basins in Eastern Indonesia. Tectonic evolution in Akimeugah Basin during Cambrian to present has produced a very significant erosion that affected the hydrocarbon generation process. ‘ARD’ Block study uses three exploratory well data including well report and 26 lines of 2D seismic data with a total length of 5,812.55 kilometers and the distance between seismic lines ranging from 10 to 15 kilometers. Seismic data is processed with IHS Kingdom software for tectonostratigraphy analysis, while calculation and erosion analysis are performed by combining well data consisting of sonic, vitrinite reflectance and seismic. To get a burial history model and generation & expulsion period, this study utilizes Petromod software. Five phases of the tectonic evolution led to four times of erosional period with a sediment thickness of 290 – 3,370 feet were loss. The erosion of the sedimentary rocks causes the maturation process delayed more than 200 million years. Burial history in the study area with the erosion absence assumption results a hydrocarbon generation starting from around 210 million years ago. Meanwhile, by considering the loss of eroded sedimentary rocks during four tectonic phases, hydrocarbon generation time just occurred 3.1 million years ago.

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Horz, Kersten H., Tim J. Worthington, Kyaw Winn, and Peter Stoffers. "Late Quaternary tephra in the New Ireland Basin, Papua New Guinea." Journal of Volcanology and Geothermal Research 132, no. 1 (April 2004): 73–95. http://dx.doi.org/10.1016/s0377-0273(03)00421-9.

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Haberle, Simon G. "Late Quaternary vegetation change in the Tari Basin, Papua New Guinea." Palaeogeography, Palaeoclimatology, Palaeoecology 137, no. 1-2 (February 1998): 1–24. http://dx.doi.org/10.1016/s0031-0182(97)00097-7.

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Muhartanto, A., A. H. Hamdani, S. Safrizal, L. Fauzielly, and A. Triwerdhana. "Source rocks study and thermal modelling in Salawati basin, West Papua." Journal of Physics: Conference Series 1402 (December 2019): 066023. http://dx.doi.org/10.1088/1742-6596/1402/6/066023.

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Sudarmi, Nurtania, and Widyaningrum Widyaningrum. "Analisis Kandungan Asam Lemak Mudah Terbang dengan Penambahan Buah Sirih dalam Ransum Ruminansia (In-Vitro)." wahana peternakan 4, no. 2 (September 25, 2020): 14–18. http://dx.doi.org/10.37090/jwputb.v4i2.210.

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Further socialization is needed regarding the importance of paying attention to the basic nutritional needs of cattle. The use of local plants that are often used by the community, such as betel fruit, is a worthy study to be explored. However, people still do not know the other benefits contained in betel fruit. In order to obtain optimal results, the study was carried out with in vitro experiments. Data processing was performed using factorial completely randomized design with three replications. The treatment factors were differentiated based on the length of the betel fruit immersion process in ice water and the length of storage time. The analysis showed that cold storage of grass with betel fruit was successful in increasing the Volattile Fatty Acid component (P> 0.01). The habits of the people of West Papua in utilizing local plants, especially those with tannin, have been scientifically proven to be useful. Cold storage of betel fruit with the addition of grass as ration for cattle has a very significant effect on the levels of iC4 (as iso butyrate), nC4 (as n butyrate), iC5 (as iso valerate), and nC5 (as n valerate). In addition, the Papuan people's habit of adding local plants, especially betel fruit as additional feed has been scientifically proven to be useful. Keywords: Betel Fruit, Ruminants, Grass, In Vitro, VFA

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Usman, Ediar, and Panuju Panuju. "STUDY OF GAS POTENCY BASED ON GRAVITY ANOMALY MODELING AND SEISMIC PROFILE ANALYSIS AT BANGGAI-SULA BASIN." BULLETIN OF THE MARINE GEOLOGY 28, no. 2 (February 15, 2016): 1. http://dx.doi.org/10.32693/bomg.28.2.2013.55.

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Banggai-Sula Basin is one of the basins with character of the micro-continent derived from northern part of Australia. Some traces the migration in the central part of Papua are slate, schist, and gneiss, current movement is facilitated by the Sorong Fault, which runs from the northern part of Papua to eastern part of Sulawesi. Results of gravity anomaly model (2D and 3D), seepage distribution, seismic and fields existing of oil and gas production in the western part of the Banggai-Sula Basin obtained a new prospect area in the northern part of Peleng Island, western part of Banggai Island, southern part of Banggai-Taliabu Islands, western and eastern part of Sulabesi Island. The new prospect area is reflected in the centre with form of the low morphology on gravity model and prospect trap on seismic data in the western part of Tolo Bay. Results of chemical analysis on the source rock of Buya Formation on Tmax vs Hydrogen Index (Tmax vs HI) Diagram shows the type III kerogen quality and the Oxygen Index vs Hydrogen Index (OI vs HI) Diagram shows the gas prone Type II, so that giving the impression that this area has the potential to containing the gas. The quality of the gas is included in the category of immature to mature type. Key word : marine geology, gravity anomaly model, trap, source rock, hydrocarbon quality, Banggai-Sula Basin Cekungan Banggai-Sula merupakan salah satu cekungan dengan karakter mikro-kontinen yang berasal dari pecahan Australia bagian utara. Beberapa jejak migrasi terdapat di bagian tengah Papua berupa batuan slate, schist, dan gneiss, pergerakannya saat ini difasilitasi oleh Sesar Sorong yang membujur dari Papua bagian utara hingga bagian timur Sulawesi. Hasil pemodelan gaya berat (2D dan 3D), daerah rembesan, seismik dan keberadaan lapangan produksi migas di bagian barat Cekungan Banggai-Sula diperoleh hasil daerah prospek baru di bagian utara P. Peleng, bagian barat P. Banggai, selatan P. Banggai-Taliabu, barat dan timur P. Sulabesi. Daerah prospek tersebut tercermin dari daerah pusat cekungan dengan bentuk morfologi rendahan pada data gaya berat dan prospek perangkap (leads) pada data seismik di bagian barat sekitar Teluk Tolo. Hasil analisis kimia batuan sumber pada Diagram Tmax vs Indeks Hidrogen menunjukkan kualitas kerogen tipe III dan pada Diagram Indeks Oksigen vs Indeks Hidrogen menunjukkan tipe II gas prone, sehingga memberikan gambaran bahwa daerah ini berpotensi mengandung gas. Kualitas gas tersebut termasuk dalam kategori belum matang sampai matang. Kata kunci : geology kelautan, model anomali graviti, perangkap, batuan induk, kualitas hidrokarbon, Cekungan Banggai-Sula

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44

Bogdanov, Yu A., A. P. Lisitzin, R. A. Binns, A. I. Gorshkov, E. G. Gurvich, V. A. Dritz, G. A. Dubinina, O. Yu Bogdanova, A. V. Sivkov, and V. M. Kuptsov. "Low-temperature hydrothermal deposits of Franklin Seamount, Woodlark Basin, Papua New Guinea." Marine Geology 142, no. 1-4 (October 1997): 99–117. http://dx.doi.org/10.1016/s0025-3227(97)00043-1.

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45

Goodenough, Peter W., Peter J. Kilshaw, Fiona McEwan, and A. Jane Owen. "Monoclonal antibodies to the two most basic papaya proteinases." Bioscience Reports 6, no. 8 (August 1, 1986): 759–66. http://dx.doi.org/10.1007/bf01116544.

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The proteinases from Carica papaya include papain, isoenzymes of chymopapain and two proteinases A and B distinguished by their unusually high pI. The identity of one of the most basic proteinases has been questioned. The present report describes the preparation and characterisation of two monoclonal antibodies that react specifically with papaya proteinases A and B respectively and a third that identifies a common structural feature found in papain and proteinase A.

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46

Takeuchi, Wayne. "Notes on Phyllanthera (Apocynaceae) from the upper Sepik of Papua New Guinea: P. lancifolia and P. piforsteriana sp. nov." Phytotaxa 163, no. 3 (March 26, 2014): 173. http://dx.doi.org/10.11646/phytotaxa.163.3.4.

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Phyllanthera piforsteriana (Apocynaceae) is described from the Sepik River basin in Papua New Guinea. Distributional notes are also provided for P. lancifolia, a frequent associate of the new species but otherwise rarely represented in herbarium collections.

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Ransta, L. Lekatompessy. "‘Mama-mama’ in Papua and the Access to Market." E3S Web of Conferences 73 (2018): 08015. http://dx.doi.org/10.1051/e3sconf/20187308015.

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The spearhead of people's economy in Papua is local traders which usually called as 'mama-mama', they try to increase family economy in Papua. The struggle among woman to seek basic necessities for their family needs serious attention from the government, particularly how to access traditional market as the place for them to sell the products of agriculture products or handcrafts such as noken and others. This article describes the existence of 'mama-mama' as women who have dual role in family, and also discusses social movement of mama-mama in Papua to access traditional market through 'Solidaritas Pedagang Asli Papua (SOLPAP)'. Besides, this article also discusses government role and the existence of social movement in implementing empowerment among mama-mama Papua regarding the training how to manage agriculture products and family coaching.

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MICHALSKI, JOHN, STEPHEN RICHARDS, and GUNTHER THEISCHINGER. "An interesting new species of Nososticta Hagen from southern New Guinea (Odonata, Disparoneuridae)." Zootaxa 3590, no. 1 (December 18, 2012): 73. http://dx.doi.org/10.11646/zootaxa.3590.1.7.

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Nososticta acuminata, a new disparoneurid damselfly from the Lakekamu Basin in Gulf Province of Papua New Guinea, is described. It is most similar to N. smilodon Theischinger & Richards, but the male has uniquely pointed superior anal appendages.

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Craddock, Paul R., Wolfgang Bach, Jeffrey S. Seewald, Olivier J. Rouxel, Eoghan Reeves, and Margaret K. Tivey. "Rare earth element abundances in hydrothermal fluids from the Manus Basin, Papua New Guinea: Indicators of sub-seafloor hydrothermal processes in back-arc basins." Geochimica et Cosmochimica Acta 74, no. 19 (October 2010): 5494–513. http://dx.doi.org/10.1016/j.gca.2010.07.003.

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Takeuchi, Wayne. "A distinctive addition to the tree flora of Papua New Guinea: Helicia woxvoldiana sp. nov. (Proteaceae), a large-flowered myrmecophyte from the upper Sepik." Phytotaxa 172, no. 2 (June 13, 2014): 94. http://dx.doi.org/10.11646/phytotaxa.172.2.4.

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Helicia woxvoldiana (Proteaceae) is described from the Sepik River basin in Papua New Guinea, from classical localities on the Kaiserin-Augusta-Fluss itinerary of 1912–13. The new species is a canopy myrmecophyte with the largest flowers in Papuasian Helicia.

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Journal articles on the topic 'Papuan Basin'

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