Relevant bibliographies by topics / Papuan Basin

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Academic literature on the topic 'Papuan Basin'

Author: Grafiati
Published: 4 June 2021
Last updated: 19 February 2022

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Journal articles on the topic "Papuan Basin"

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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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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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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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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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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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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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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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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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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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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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Dissertations / Theses on the topic "Papuan Basin"

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Morgan, Glenn Douglas School of Biological Earth &amp Environmental Science UNSW. "Sequence stratigraphy and structure of the tertiary limestones in the Gulf of Papua, Papua New Guinea." Awarded by:University of New South Wales. School of Biological, Earth and Environmental Science, 2005. http://handle.unsw.edu.au/1959.4/22913.

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A sequence stratigraphic study was conducted on the Mendi and Darai Limestone Megasequences in the foreland area of the Papuan Basin in Papuan New Guinea. It involved the integrated use of seismic, wireline log, well core and cuttings, strontium isotope age and biostratigraphic data. This study enhanced the understanding of the structure, stratigraphy and depositional architecture of the limestones, and the morphology of the basin at the time of deposition. The results of the study were integrated with published geological and tectonic models for the Papuan Basin to develop a consistent and coherent model for the depositional history of the limestones. Eleven third-order sequences were delineated within the Mendi and Darai Limestone Megasequences. Eight depositional facies were interpreted across these sequences, namely deep-shelf, shallow-shelf, backreef, reef, shoal, forereef, basin margin and submarine fan facies. Each facies was differentiated according to seismic character and geometry, well core and cuttings descriptions, and its position in the depositional framework of the sequence. Deposition of the Mendi Limestone Megasequence commenced in the Eocene in response to thermal subsidence and eustatic sea-level rise. Sedimentation comprised open-marine, shallow-water, shelfal carbonates. During the middle of the Oligocene, the carbonate shelf was exposed and eroded in response to the collision of the Australian and Pacific Plates, or a major global eustatic sea-level fall. Sedimentation recommenced in the Late Oligocene, however, in response to renewed extensional faulting and subsidence associated with back-arc extension. This marked the onset of deposition of the Darai Limestone Megasequence in the study area. The KFZ, OFZ and Darai Fault were reactivated during this time, resulting in the oblique opening of the Omati Trough. Sedimentation was initially restricted to the Omati Trough and comprised deep and shallow-marine shelfal carbonates. By the Early Miocene, however, movement on the faults had ceased and an extensive carbonate platform had developed across the Gulf of Papua. Carbonate reef growth commenced along topographic highs associated with the KFZ, and led to the establishment of a rimmed carbonate shelf margin. Shallow to locally deeper-marine, shelfal carbonates were deposited on this shelf, and forereef, submarine fan and basin margin carbonates were deposited basinward of the shelf margin. The Uramu High and parts of the Pasca High became submerged during this time and provided sites for pinnacle reef development. During the middle of the Early Miocene, a major global eustatic sea-level fall or flexure of the Papuan Basin associated with Early Miocene ophiolite obduction subaerially exposed the carbonate shelf. This resulted in submarine erosion of the forereef and basin margin sediments. Towards the end of the Early Miocene, however, sedimentation recommenced. Shallow-marine, undifferentiated wackestones and packstones were deposited on the shelf; forereef, submarine fan and basin margin sediments were deposited basinward of the shelf margin; and reef growth recommenced along the shelf margin and on the Pasca and Uramu Highs. By the end of the Early Miocene, however, the pinnacle reef on the Pasca High had drowned. During the middle of the Middle Miocene, subtle inversion associated with ophiolite obduction subaerially exposed the carbonate shelf, and resulted in submarine erosion of the forereef and basin margin sediments. Sedimentation recommenced towards the end of the Middle Miocene, however, in response to eustatic sea-level rise and flexure of the crust associated with foreland basin development. Shallow marine, undifferentiated wackestones, packstones and grainstones were deposited on the shelf; carbonate shoals were deposited along the shelf margin; and forereef, submarine fan and basin margin carbonates were deposited basinward of the shelf margin. Carbonate production rapidly outpaced accommodation space on the shelf during this time, resulting in highstand shedding and the development of a large prograding submarine fan complex basinward of the shelf margin. By the Late Miocene, carbonate deposition had ceased across the majority of the study area in response to a major global eustatic sea-level fall or inversion associated with terrain accreation events along the northern Papuan margin. Minor carbonate deposition continued on parts of the Uramu High, however, until the middle of the Late Miocene. During the latest Miocene, clastic sediments prograded across the carbonate shelf, infilling parts of the foreland basin. Plio-Pleistocene compression resulted in inversion and erosion of the sedimentary package in the northwestern part of the study area. In the southeastern part of the Papuan Basin, however, clastic sedimentation continued to the present day.
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Ma, KeYang. "Hydrocarbon source and depositional environments in the central Papual Basin, Papua New Guinea /." [St. Lucia, Qld.], 2005. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe18901.pdf.

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Cullen, Andrew Blinn. "The North New Guinea Basin, Papua New Guinea : a case study of basin evolution at a modern accretionary plate boundary /." Full-text version available from OU Domain via ProQuest Digital Dissertations, 1990.

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Moss, Roger. "Geochemistry and mineralogy of gold in the PACMANUS and Susu knolls hydrothermal systems, eastern Manus basin, Papua New Guinea." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0020/NQ53744.pdf.

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Fitz, Guy Gregory. "Offshore mapping and modeling of Miocene-Recent extensional basins adjacent to metamorphic gneiss domes of the D'Entrecasteaux Islands, eastern Papua New Guinea." 2011. http://hdl.handle.net/2152/14789.

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The D'Entrecasteaux Island (DEI) gneiss domes are fault-bounded domes with ~2.5 km of relief exposing ultrahigh-pressure (UHP) and high-pressure (HP) metamorphic gneisses and migmatites exhumed in an Oligocene-Miocene arc-continent collision and subduction zone subject to Late Miocene to Recent continental extension. To study the style of continental extension accompanying exhumation of the DEI gneiss domes, a grid of 1,518 km of 2-D multi-channel seismic (MCS) reflection data and well data is interpreted from the offshore areas surrounding the DEI, including the Trobriand basin and the Goodenough basin. The offshore study is combined with onshore geologic information to constrain the area's Oligocene to Recent basinal and tectonic evolution. MCS and well data show the Trobriand basin formed as a forearc basin caused by southward Miocene subduction at the Trobriand trench. Late Miocene basin inversion uplifted the southern and northern basin margins. Subduction slowed at ~8 Ma as the margin transitioned to an extensional tectonic environment. Since then, the Trobriand basin has subsided 1-2.5 km as a broad sag basin with few normal faults deforming the basin fill. South of the DEI, the Goodenough rift basin developed after extension began (~8 Ma) as the hanging-wall of the north-dipping Owen-Stanley normal fault bounding the southern margin of the basin. Rapid uplift of the adjacent footwall of the Owen-Stanley fault zone in the Papuan Peninsula accompanied the formation of the Goodenough submarine rift basin. The lack of upper crustal extension accompanying subsidence in the Trobriand and Goodenough basins suggests depth-dependent lithospheric extension from 8-0 Ma has accompanied uplift of the DEI gneiss domes. Structural reconstructions of seismic profiles show 2.3 to 13.4 km of basin extension in the upper crust, while syn-rift basin subsidence values indicate at least 20.7 to 23.6 km of extension occurred in the lower crust since ~8 Ma. Results indicating thinning is preferentially accommodated in the lower crust surrounding the DEI are used to constrain a schematic model of uplift of the DEI domes involving vertical exhumation of buoyant, post-orogenic lower crust, far-field extension from slab rollback, and an inverted two-layer crustal density structure.
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Salo, Jonathan Peter. "Evaluating sites for subsurface CO₂injection/sequestration : Tangguh, Bintuni Basin, Papua, Indonesia." 2005. http://hdl.handle.net/2440/49746.

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The venting of anthropogenic CO₂ emissions into the atmosphere at increasing rates is probably influencing global warming and climate change. The Tangguh LNG development project in Papua, Indonesia will produce significant volumes of CO₂, which might be vented into the atmosphere. The LNG process will necessitate the separation of CO₂, estimated at 2.4 trillion cubic feet (TCF sc), from the natural gas reserves prior to liquefaction and shipping. This study screens and assesses the possible alternatives to atmospheric venting, and recommends subsurface CO₂ injection and sequestration/storage in saline aquifers. The study identifies specific subsurface locations for several Environmentally-Sustainable Sites for CO₂ Injection (ESSCI) in Bintuni Basin, where the Tangguh production fields are located. Alternatives to atmospheric venting of the estimated CO₂ volume at Tangguh include both non-geologic and geologic disposal options. Non-geologic options such as biosphere sinks (enhanced forest or agricultural growth), deep-ocean sinks (subsea dispersal), and direct commercial usage (e.g. use in beverage or fertilizer production, fire-retardant manufacturing) are impractical and of questionable impact in remote Papua, Indonesia. Several subsurface geological disposal options were investigated, but the most viable geologic disposal option for Tangguh CO₂ is injection into the downdip aquifer leg of the Roabiba Sandstone Formation hydrocarbon reservoir. Injected CO₂, at supercritical phase, is expected to migrate updip into the sealed structural traps at Vorwata or Wiriagar Deep, as the natural gas reserves are produced. A probabilistic ranking of data quality and quantity for five potential ESSCI reservoirs determined that the Middle Jurassic Roabiba Sandstone Formation has the highest likelihood of viable ESSCI sequestration/storage. A probabilistic ranking of data quality and quantity for eight ESSCI structural traps within the western flank of Bintuni Basin, determined that Vorwata, followed by Wiriagar Deep, are the most viable ESSCI structural traps at the Middle Jurassic reservoir level. Five potential ESSCI seals were evaluated and it was determined the best seal potential occurs in the Pre-Ayot Shales, directly overlying the Middle Jurassic reservoir at Vorwata. This unit is capable of holding a 3300 to 4660 foot (1006 to 1420 meter) CO₂_column. Seal integrity of the Pre-Ayot is very good because it is a relatively homogeneous deep-water shale that is composed primarily of ductile illite and kaolinite clays with a minor quartz and feldspar content. Sequence stratigraphy analysis suggests that the zone extends over the entire Vorwata three-way dip closure, with thickness between 17 feet (5 m) and 233 (71 m) feet. The maximum effective storage capacity of the Middle Jurassic reservoirs for each structure was calculated, taking into account irreducible water, trapped water, and trapped residual gas pore volumes. The Vorwata structure is capable of storing 19.3 TCFsc supercritical CO₂ at reservoir temperature and pressure. The Wiriagar Deep structure has potential storage capacity of 3.5 TCFsc, and Ubadari 2.8 TCFsc, at their respective reservoir temperatures and pressures. A ‘Rating Product Ranking’ was developed to quantify the results of the quality and quantity of four factors: Reservoir Data, Structure Data, Seal Data, and Storage Ratio. Each structure, and the respective top and lateral seal overlying the Middle Jurassic reservoirs, was evaluated. The net result was that Vorwata rated a 0.88 on a scale of zero to one, where 1.0 represents 100% confidence in ESSCI potential. Ubadari and Wiriagar Deep scored, respectively, 0.52 and a 0.45. Finally, the structures were evaluated for relative proximity to the proposed CO₂_source (i.e. the LNG plant location). With a weighted distance factor calculated with the Rating product for each potential injection site, Vorwata rated 0.88 on a scale of zero to one, Wiriagar scored 0.24, and Ubadari scored only 0.09. The Middle Jurassic ‘Roabiba Sandstone Formation reservoir’ at the Vorwata structure has the greatest potential as an ESSCI storage site. The Middle Jurassic ‘Aalenian Sandstone Formation reservoir’ at the Wiriagar Deep is the second-best potential ESSCI storage site. The subsurface ESSCI injection location proposed for the ‘Roabiba Sandstone Formation’ aquifer, 10 km southeast and down-dip from the known gas-water contact (GWC), is on the southeast Vorwata plunging anticlinal nose. An alternate potential ESSCI injection location proposed for the ‘Roabiba Sandstone Formation’ aquifer is 6 km south of and down-dip from the known gaswater contact (GWC) on Vorwata structure southern flank. A key issue was to determine the possible risk of fault re-activation from CO₂_ injection. NE-SW striking vertical faults have the highest risk of re-activation requiring an increase of over ~1460 psi (103 kg/cc) over hydrostatic at 14,000 ft TVDss (4267 m), for slippage to occur. The closest fault with a high risk of re- activation is 5 km northwest of the recommended ESSCI site location. Supercritical CO₂_ pressure is not expected to exceed the estimated pressure determined to cause fault re-activation. A 3D geological model of the Mesozoic interval was constructed over a large area of western Bintuni Basin. The model was constructed so as to preserve as much geological heterogeneity as possible yet still have a manageable number of active cells. Faults were incorporated into the model as strike-slip vertical fault surfaces (or indexed fault polygons) as a separate attribute. The geo-cellular model was built suitable for importation into a reservoir simulator (VIP), and a 25-year simulation run for natural gas production from the Vorwata Middle Jurassic reservoir, with concurrent CO₂ injection downdip into the Vorwata Middle Jurassic aquifer at the primary recommended ESSCI site location. The simulation verified the recommended location with the CO₂ slowly migrating into the Vorwata structural trap within the Middle Jurassic reservoir, and not compromising the hydrocarbon reserves or production. It is recommended that additional data be acquired such as conventional core, formation water samples, and specific logs such as dipole-sonic, multi-chambered dynamic formation testers (MDT), and mechanical rotary sidewall coring tools (MSCT). Lastly, several CO₂ monitoring methods and techniques are recommended for Tangguh to monitor CO₂ migration, pressures, and potential leakages. One such method is a vertical monitoring well at the recommended injection site. Other monitoring techniques include smart well completions, detection monitors at production wells with tracers injected prior to CO₂ injection. In addition, crosswell seismic surveys, electromagnetic methods, and electrical-resistance tomography techniques are suggested during the injection phase.
http://proxy.library.adelaide.edu.au/login?url= http://library.adelaide.edu.au/cgi-bin/Pwebrecon.cgi?BBID=1174414
Thesis (Ph.D.) -- University of Adelaide, Australian School of Petroleum, 2005
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Chen, Hung-Yi, and 陳虹頤. "Structural Basis of Ubiquitin Recognition by SARS Coronavirus Papain-like Protease." Thesis, 2013. http://ndltd.ncl.edu.tw/handle/23269424442290528944.

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碩士
國立陽明大學
生命科學系暨基因體科學研究所
101
Severe acute respiratory syndrome (SARS) is a global infectious disease in 2003 caused by a novel species of human coronavirus (SARS-CoV). After the virus entry to host cell, the positive-sense RNA in the genome of SAR-SCoV is used to translate non-structural polyprotein. The polyprotein transforms into mature and functional form for viral replication by two proteases, papain-like protease (PLpro) and main protease. PLpro recognizes LXGG (sequence from P4-P1) in viral polyprotein. PLpro also functions as deubiquitinating and deISGlating in vitro, which may help the virus escape from the immune system of host. Until now, the detail mechanism for the substrate binding to PLpro is still unclear. Inmy thesis, I want to investigate the substrate binding mechanism of PLpro by structural and biochemical analysis. At the beginning, I tried to express and purify the C112S mutant of PLpro by Escherichia coli expression system. The kinetic assay suggested that C112S has no enzyme activity in that the lower proton transferring ofserine, compared to that of cysteine .The inactive mutant may be used to identify the substrate-enzyme complex. Here I report the structure of PLpro in complex with Ub by X-ray crystallography.Like other ubiquitin specific proteases, the C-terminal tail of Ub penetrates to the groove between thumb and palm domain. Moreover, the fingers domain holds the core of Ub. Superimposion with the structure of free PLpro, I suggested that the active site of the enzyme become closer and the fingers domain move forward to Ub.Surprisingly, CHES ,as a buffer material locates near the active site and interacts with the two residues of catalytic triad. Mutations on PLpro that disrupt these non-covalent inter actions to the C-terminal tail of Ub reduce the substrate binding affinity and protease activity. Our results provide direct structural insights into substrate binding mechanism of PLpro, it can contribute to design a more efficient drug to inhibit the PLpro.
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Carson, Brooke Elizabeth. "Late Quaternary sediment accumulations and foraminiferal populations on the slopes of Gladden Basin (offshore Belize) and southern Ashmore Trough (Gulf of Papua) mixed siliciclastic-carbonate systems." Thesis, 2007. http://hdl.handle.net/1911/20584.

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The Belize margin, in the western Caribbean Sea, and Ashmore Trough, in the western Gulf of Papua, represent modern tropical mixed siliciclastic-carbonate depositional systems where significant masses of both river born terrigenous siliciclastics and neritic/pelagic carbonates accumulate at variables rates over space and time. This study examines variations in sedimentolgic and micropaleontologic parameters relative to late Quaternary sea level, climate, and paleoenvironment. This is accomplished through the evaluation of carbonate and siliciclastic accumulations, as well as planktic foraminiferal populations, of a 37.7 m giant piston core (MD02-2532) acquired from the slope of Gladden Basin adjacent to the Belize Barrier Reef, as well as benthic foraminiferal populations of two shorter (11.3 m) piston cores (MV-74 and MV-07/06) acquired on the slopes of Ashmore Trough, adjacent to the northern most extent of the Great Barrier Reef. Neritic carbonate fluxes to the slopes of Gladden Basin are largely regulated by sea level and consistent with well-established highstand shedding depositional concepts. Over the last ∼850 ka, neritic carbonate production (and export to the adjacent slopes) switches on when sea level floods the neritic carbonate regions and switches off when sea level falls and neritic carbonate regions are exposed. Siliciclastic accumulations are also controlled primarily by eustatic sea level fluctuations, with additional influences from local and regional variations in physiography, climate, and/or ocean currents. Planktic foraminiferal taxa of Gladden Basin are typical of tropical to subtropical populations and display significant variations in their downcore relative abundances, suggesting notable changes in surface water masses and oceanographic parameters over the last ∼630 ka. Temperature and salinity, often associated with glacial or interglacial intervals, appear to predominately influence the planktic foraminiferal populations. In Ashmore Trough, benthic foraminiferal relative abundances and multivariate analyses indicate three distinct assemblages whose proportions change over the last ∼83 ka. These assemblages signify distinct paleoenvironmental settings driven by organic carbon flux and sediment supply, as well as changes in sea level. Analysis of these late Quaternary mixed systems provides better understanding of their preservation in the rock record, particularly relative to sea level and sequence stratigraphic concepts.
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Horz, Kersten [Verfasser]. "Late quarternary volcanic activity in the New Ireland Basin : distribution and geochemical evolution of tephra at the Tabar-Lihir-Tanga-Feni chain, Papua New Guinea / vorgelegt von Kersten Horz." 2002. http://d-nb.info/971996040/34.

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Books on the topic "Papuan Basin"

1

Shinkarev, Vladimir. Papuas iz Gondurasa: Domashniĭ ezh ; T͡S︡arʹ zvereĭ ; Stikhi, basni i pesni. Sankt-Peterburg: "Krasnyĭ matros", 1998.

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Papua New Guinea 2000 census: 2000 census basic tables : national level. Port Moresby: National Statistical Office, 2002.

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name, No. A biodiversity assessment of Yongsu - Cyclops Mountains and the Southern Mamberamo Basin, Papua, Indonesia. Washington, DC: Center for Applied Biodiversity Science, 2002.

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Papua New Guinea 2000 census: 2000 census basic tables : national level--rural sector. Port Moresby: National Statistical Office, 2002.

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Grubb, P. J. The forests of the Fatima basin and Mt. Kerigomna, Papua New Guinea, with a review of montane and subalpine rainforests in Papuasia. Canberra: Australian National University, 1985.

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Grubb, P. J. The forests of the Fatima basin and Mt. Kerigomna,Papua New Guinea, with a review of montane and subalpine rainforests in Papuasia. Canberra: Australian National University, 1985.

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Austin, Flannery, ed. The basic sixteen documents : constitutions, decrees, declarations : a completely revised translation in inclusive language. Northport, NY: Costello Publishing, 1996.

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Clark, Jeffrey. Perceptions of development by women of the Tari Basin, Southern Highlands Province: A sub-project of integrated rural development programme evaluation in Papua New Guinea by D.A.M. Lea and R. Crittenden. Boroko, Papua New Guinea: National Research Institute, 1990.

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de Vries, Lourens. The imperative paradigm of Korowai, a Greater Awyu language of West Papua. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198803225.003.0012.

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The imperative paradigm of Korowai, a Papuan language of West Papua, is the richest independent verb paradigm of Korowai: it makes the same distinctions as all other independent verb paradigms but makes more distinctions in grammatical person: three grammatical persons rather than conflation of second and third person as in all other Korowai and Greater Awyu verb paradigms. This formal richness is matched by functional richness: imperatives are used in a typologically striking range of contexts, for example in bridging constructions (tail–head linkage), in the domain of inner states (through quotative framing of emotion, thoughts, and intentions) and in both addressee-inclusive and addressee-exclusive contexts (in the case of first person plural imperatives). Diachronically, the Korowai imperative paradigm developed from a basic injunctive zero paradigm of proto Greater Awyu that has reflexes in all branches and languages of the Greater Awyu family.
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Penyusunan basis data potensi lahan: Pulau Papua. [Cibinong]: Pusat Survei Sumberdaya Alam Darat, Bakosurtanal, 2005.

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Book chapters on the topic "Papuan Basin"

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Binns, Raymond A. "Deep marine pumice from the Woodlark and Manus Basins, Papua New Guinea." In Explosive Subaqueous Volcanism, 329–43. Washington, D. C.: American Geophysical Union, 2003. http://dx.doi.org/10.1029/140gm22.

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Kroenke, L. W., Murli H. Manghnani, C. S. Rai, P. Fryer, and Ralph Ramananantoandro. "Elastic Properties of Selected Ophiolitic Rocks from Papua New Guinea: Nature and Composition of Oceanic Lower Crust and Upper Mantle." In The Geophysics of the Pacific Ocean Basin and Its Margin, 407–21. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm019p0407.

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Wang, K. P., and E. Chin. "Papua New Guinea." In Mineral Economics and Basic Industries in Asia, 243–47. Routledge, 2019. http://dx.doi.org/10.4324/9780429050824-21.

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Schultz, Jaime. "Sex Segregation." In Women's Sports. Oxford University Press, 2019. http://dx.doi.org/10.1093/wentk/9780190657710.003.0006.

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Why do we segregate sport on the basis of sex? In Playing With the Boys: Why Separate Is Not Equal, scholars Eileen McDonagh and Laura Pappano argue that there have been “three I’s” historically used to justify sex segregation in sport: Women’s physical differences from...
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Marlow, Michael S., Neville F. Exon, and Shawn V. Dadisman. "Hydrocarbon Potential and Gold Mineralization in the New Ireland Basin, Papua New Guinea." In Geology and Geophysics of Continental Margins. American Association of Petroleum Geologists, 1992. http://dx.doi.org/10.1306/m53552c8.

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Beaudoin, Yannick C., and Samantha Smith. "Habitats of the Su Su Knolls Hydrothermal Site, Eastern Manus Basin, Papua New Guinea." In Seafloor Geomorphology as Benthic Habitat, 843–52. Elsevier, 2012. http://dx.doi.org/10.1016/b978-0-12-385140-6.00062-1.

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Cook, A. C., and G. D. Karner. "Data report: Organic petrology of Leg 180 samples, western Woodlark Basin, Papua New Guinea." In Proceedings of the Ocean Drilling Program, 180 Scientific Results. Ocean Drilling Program, 2002. http://dx.doi.org/10.2973/odp.proc.sr.180.157.2002.

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"Leg 180 Summary: Active Continental Extension in the Western Woodlark Basin, Papua New Guinea." In Proceedings of the Ocean Drilling Program. Ocean Drilling Program, 2000. http://dx.doi.org/10.2973/odp.proc.ir.180.101.2000.

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DALRYMPLE, ROBERT W., ELAINE K. BAKER, PETER T. HARRIS, and MICHAEL G. HUGHES. "SEDIMENTOLOGY AND STRATIGRAPHY OF A TIDE-DOMINATED, FORELAND-BASIN DELTA (FLY RIVER, PAPUA NEW GUINEA)." In Tropical Deltas of Southeast Asia, 147–73. SEPM (Society for Sedimentary Geology), 2003. http://dx.doi.org/10.2110/pec.03.76.0147.

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Monteleone, B. D., S. L. Baldwin, T. R. Ireland, and P. G. Fitzgerald. "Thermochronologic constraints for the tectonic evolution of the Moresby Seamount, Woodlark Basin, Papua New Guinea." In Proceedings of the Ocean Drilling Program, 180 Scientific Results. Ocean Drilling Program, 2001. http://dx.doi.org/10.2973/odp.proc.sr.180.173.2001.

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Conference papers on the topic "Papuan Basin"

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Allan*, Tony, and David Holland. "Cenozoic Carbonate Deposition in the Eastern Papuan Basin." In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2211549.

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Krawczunski*, Lukasz, and Tom Herries. "Hydrocarbon Generation and Long Distance Migration in the Foreland Part of the Papuan Basin." In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2205988.

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Geslin*, Jeffrey K., and Brian J. Darby. "Papua New Guinea: Mesozoic Rift Basin Evolution and Its Control on Basin Fill." In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2209814.

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Brede, E. C. "Interactive overthrust interpretation: Cape Vogel basin, Papua, New Guinea." In SEG Technical Program Expanded Abstracts 1987. Society of Exploration Geophysicists, 1987. http://dx.doi.org/10.1190/1.1891896.

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A. Subroto, Eddy, and Benyamin Sapiie. "Source Rocks Assessment in Bintuni Basin, Papua, Indonesia: The Answer!" In Annual International Conference on Geological & Earth Sciences. Global Science & Technology Forum (GSTF), 2014. http://dx.doi.org/10.5176/2251-3353_geos14.42.

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Shakerley, A., C. Kergaravet, W. Gordon Canning, V. Bailly, and J. Ringenbach. "Rifting to drifting with core complexes - The tectonic architecture & evolution of the Offshore Papuan Plateau, PNG." In EAGE/AAPG Workshop on Reducing Exploration Risk in Rift Basins. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.202076023.

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Sucipto, Teguh Hari, Nur Laila Fitriati Ahwanah, Siti Churrotin, Norifumi Matake, Tomohiro Kotaki, and Soegeng Soegijanto. "Immunofluorescence assay method to detect dengue virus in Paniai-Papua." In 5TH INTERNATIONAL CONFERENCE AND WORKSHOP ON BASIC AND APPLIED SCIENCES (ICOWOBAS 2015). AIP Publishing LLC, 2016. http://dx.doi.org/10.1063/1.4943313.

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Ozza, T. "Prediction of Hydrocarbon Sources in The Walio Area, Salawati Basin, West Papua, Indonesia." In Digital Technical Conference. Indonesian Petroleum Association, 2020. http://dx.doi.org/10.29118/ipa20-g-207.

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Substantial seismic and well data have been gathered and used for the exploration and exploitation of the Salawati Basin since the 1970s. The interpretation of these data and implementation of findings resulted into several discoveries and producing fields associated with the Tertiary petroleum system of Klasafet-Kais, particularly in the Walio Area. The presence of pre-Tertiary petroleum systems remain speculative to date although numerous pre-Tertiary structural and stratigraphic traps can be defined, and hypothetical sourcing can be inferred to origin from shales of the Permo-Triassic Aifam Group and the Late Jurassic – Late Cretaceous Kembelangan Formation. Yet the actual hydrocarbon charging of those traps has not been proven. Surface geochemical surveys were conducted in the Walio Area with the objective to characterize the origin of hydrocarbons of the area and possibly uncover the presence of a pre-Tertiary source. Pre-Tertiary sediments are encountered in three exploration wells of the Walio Area and pre-Tertiary traps were defined by the interpretation of 3D seismic. Surface geochemical surveys were conducted in the Walio Area to map the distribution of oil and gas microseeps and try to determine their source. Whole oil chromatography and isotope & biomarker analysis were also performed on Kais reservoired oil samples to determine source rock lithology, depositional environment, and age. Hydrocarbon analysis of one-meter-deep soil samples revealed the distribution of volatile and liquid hydrocarbon microseeps in the survey area. Total Organic Carbon (TOC) and Rock-Eval Pyrolysis measurement was carried out to outcrop samples of the Klasafet Fm., Kembelangan Fm., Tipuma Fm., and Aifat Fm. The outcrop samples resulted in lean TOC, and produced very low S2 values to which the Tmax cannot be estimated. Hydrocarbon microseeps were found occurring over and off existing fields and pre-Tertiary traps. Both light oil microseeps (35° API) and heavy oil microseeps (14° API) were identified over fresh and biodegraded crude oil Kais reservoirs, respectively in the Walio Area. Microseeps with lighter hydrocarbon compositions (e.g. C5/C17 ratio) may reflect leakage from deeper pre-Tertiary sources.
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Bailey, Brad, Galal Salem, and Patrick Haltmeier. "Testing the Tertiary Basin Floor Fan Play in the Gulf of Papua, PNG." In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2208867.

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Ozza, Tsania. "Exploring Mesozoic Play Type of Salawati Basin, West Papua, Indonesia: A Modern Study Approach." In Indonesian Petroleum Association 42nd Annual Convention and Exhibition. Indonesian Petroleum Association, 2018. http://dx.doi.org/10.29118/ipa19.g.81.

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Reports on the topic "Papuan Basin"

1

Processed shaded relief and bathymetry of the Lihir Island Group, New Ireland Basin, Papua New Guinea. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210463.

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Colour-shaded bathymetry, Lihir Island Group, New Ireland Basin, Papua New Guinea (compilation of data from SO-94, SO-133 and SO-166 bathymetric mapping). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215674.

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Bathymetry of the New Ireland Basin region, Papua New Guinea including four detailed island groups based on Cruise SO-94 of the RV Sonne: Tabar, Lihir, Tanga, and Feni. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207611.

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