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Добірка наукової літератури з теми "Tectonics of Papua New Guinea"

Автор: Grafiati
Опубліковано: 10 грудня 2022
Оновлено: 28 січня 2023

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Статті в журналах з теми "Tectonics of Papua New Guinea"

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Klootwijk, Chris, John Giddings, Chris Pigram, Charles Loxton, Hugh Davies, Rick Rogerson, and David Falvey. "Papua New Guinea Highlands: palaeomagnetic constraints on terrane tectonics." Tectonophysics 362, no. 1-4 (February 2003): 239–72. http://dx.doi.org/10.1016/s0040-1951(02)00640-6.

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2

Davies, H. L., J. Lock, D. L. Tiffin, E. Honza, Y. Okuda, F. Murakami, and K. Kisimoto. "Convergent tectonics in the Huon Peninsula region, Papua New Guinea." Geo-Marine Letters 7, no. 3 (September 1987): 143–52. http://dx.doi.org/10.1007/bf02238044.

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Klootwijk, Chris, John Giddings, and Chris Pigram. "Palaeomagnetic constraints on terrane tectonics: Highlands and Sepik regions, Papua New Guinea." Exploration Geophysics 24, no. 2 (June 1993): 291–94. http://dx.doi.org/10.1071/eg993291.

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4

Galewsky, Joseph, Eli A. Silver, Christina D. Gallup, R. L. Edwards, and Donald C. Potts. "Foredeep tectonics and carbonate platform dynamics in the Huon Gulf, Papua New Guinea." Geology 24, no. 9 (1996): 819. http://dx.doi.org/10.1130/0091-7613(1996)024<0819:ftacpd>2.3.co;2.

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Cullen, Andrew B., and John D. Pigott. "Post-Jurassic tectonic evolution of Papua New Guinea." Tectonophysics 162, no. 3-4 (May 1989): 291–302. http://dx.doi.org/10.1016/0040-1951(89)90250-3.

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6

Benes, Vladimir, Steven D. Scott, and Ray A. Binns. "Tectonics of rift propagation into a continental margin: Western Woodlark Basin, Papua New Guinea." Journal of Geophysical Research: Solid Earth 99, B3 (March 10, 1994): 4439–55. http://dx.doi.org/10.1029/93jb02878.

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7

Jablonski, Dariusz, and Mark Ballesteros. "New Regional Data and Advances in Understanding of the Stratigraphy, Tectonics, Structure and Prospectivity of the Gulf of Papua (Papua New Guinea)." ASEG Extended Abstracts 2018, no. 1 (December 2018): 1. http://dx.doi.org/10.1071/aseg2018abt7_4a.

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8

Blenkinsop, Tom, Gerard Tripp, and Dave Gillen. "The relationship between mineralization and tectonics at the Kainantu gold–copper deposit, Papua New Guinea." Geological Society, London, Special Publications 453, no. 1 (October 26, 2017): 269–88. http://dx.doi.org/10.1144/sp453.11.

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9

Sweet, S., and E. A. Silver. "Tectonics and Slumping in the Source Region of the 1998 Papua New Guinea Tsunami from Seismic Reflection Images." Pure and Applied Geophysics 160, no. 10-11 (October 1, 2003): 1945–68. http://dx.doi.org/10.1007/s00024-003-2415-z.

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10

Baldwin, Suzanne L., Brian D. Monteleone, Laura E. Webb, Paul G. Fitzgerald, Marty Grove, and E. June Hill. "Pliocene eclogite exhumation at plate tectonic rates in eastern Papua New Guinea." Nature 431, no. 7006 (September 2004): 263–67. http://dx.doi.org/10.1038/nature02846.

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Дисертації з теми "Tectonics of Papua New Guinea"

1

Cameron, Milo Louis. "Rifting and subduction in the papuan peninsula, papua new guinea| The significance of the trobriand tough, the nubara strike-slip fault, and the woodlark rift to the present configuration of papua new guinea." Thesis, The University of Alabama, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=3620068.

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The calculated extension (~111 km) across the Woodlark rift is incompatible with the > 130 km needed to exhume the Metamorphic Core Complexes on shallow angle faults (< 30°) using N-S extension in the Woodlark Basin. High resolution bathymetry, seismicity, and seismic reflection data indicate that the Nubara Fault continues west of the Trobriand Trough, intersects the Woodlark spreading center, and forms the northern boundary of the Woodlark plate and the southern boundary of the Trobriand plate. The newly defined Trobriand plate, to the north of this boundary, has moved SW-NE along the right lateral Nubara Fault, creating SW-NE extension in the region bounded by the MCC's of the D'Entrecasteaux Islands and Moresby Seamount. Gravity and bathymetry data extracted along four transect lines were used to model the gravity and flexure across the Nubara Fault boundary. Differences exist in the elastic thickness between the northern and southern parts of the lines at the Metamorphic Core Complexes of Goodenough Island (Te_south = 5.7 x 103 m; Te_north = 6.1 x 103 m) and Fergusson Island (Te_south = 1.2 x 103 m; Te_north = 5.5 x 103 m). Differences in the elastic strength of the lithosphere also exist at Moresby Seamount (Te_south = 4.2 x 103 m; Te_north = 4.7 x 103 m) and Egum Atoll (Te_south =7.5 x 103 m; Te_north = 1.3 x 104 m). The differences between the northern and southern parts of each transect line imply an east-west boundary that is interpreted to be the Nubara Fault. The opening of the Woodlark Basin resulted in the rotation of the Papuan Peninsula and the Woodlark Rise, strike slip motion between the Solomon Sea and the Woodlark Basin at the Nubara Fault, and the formation of the PAC-SOL-WLK; SOL-WLK-TRB triple junctions. The intersection of the Woodlark Spreading Center with the Nubara Fault added the AUS-WLK-TRB triple junction and established the Nubara Fault as the northern boundary of the Woodlark plate.

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2

Koudashev, Oleg. "Large-Scale Structure and Geochronology of Porphyry and Epithermal Deposits Along the Northern Collisional Margin of the Australian Continental Lithosphere." Phd thesis, Canberra, ACT : The Australian National University, 2016. http://hdl.handle.net/1885/144451.

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In this thesis I combine 40Ar/39Ar geochronology and tectonics to investigate porphyry and epithermal deposits along the northern collisional margin of the Australian continental lithosphere using case studies on the islands of New Guinea and Sulawesi. The tectonic evolution of these islands reflects the effects of progressive northward movement after rifting off from Gondwana, with this movement involving interaction with multiple subduction zones and several accretion events. The island of New Guinea contains a number of world-class porphyry deposits forming the New Guinea copper-gold belt, including the world’s largest gold producer Grasberg. In comparision, the island of Sulawesi hosts multiple small and medium sized deposits but no major porphyries like New Guinea. The work reported here established the age of the hydrothermal system at the Yandera porphyry, located in the northern highlands of Papua New Guinea. The 3 Ma age obtained is younger than lithologies observed in drill core, or at the surface, suggesting that mineralisation in Yandera is genetically unrelated to the Yandera Porphyry suite of intrusives, making Yandera a detached/wallrock porphyry. Argon geochronology using step heating diffusion experiments was shown capable of identifying the age of hydrothermal overprinting, and providing an age for mineralisation U-Pb geochronology from an earlier study showed the porphyry suite to be 6.3-7.1 Ma. The age of ductile fabrics, interpreted to be related to an extensional shear zone, and metamorphism in the Bundi Fault Zone, north of the Yandera deposit, was established to be 8-13 Ma, which is coeval with the emplacement of the Bismarck Intrusive Complex and smaller satellite intrusives. These ages were much older than the mineralisation at Yandera. Thus the surface geology, except for younger fauts, was largely irrelevant to the formation of the deposit, except in respect to ground preparation. Geochronology of the Tombulilato, Tapadaa and Gunnung Pani deposits on the North Arm of Sulawesi also produced very young ages ranging from 5.5-1.8 Ma. Similar to Yandera,the Tapadaa porphyry deposit was also found to be hosted in an igneous intrusion that was older than the age of mineralisation, placing Tapadaa in a similar time period to the nearby epithermal deposits in Tombulilato. This thesis also reports the analysis of earthquake hypocenters and seismic tomography datasets, used to interpret the geometry and structure of subducted lithosphere beneath the areas of interest. The Yandera deposit and deposits in the North Arm of Sulawesi were found to be located above portions of subducted lithosphere adjacent to slab tears. Deposits were also found to be associated with structures and processes that should allow the fast ascent of magmas through the crust such as major strike-slip faults and uplift. Formation of the deposits of Tombulilato and Tapadaa was interpreted to occur as a result of north-directed subduction and rollback of the Molucca Sea Slab. Formation of the Yandera deposit was interpreted to occur due to tearing of subducted lithosphere as the result of oblique collision with the Finisterre terrane. The formation of these deposits was proposed to coincide with initiation of movement on nearby major strike-slip faults. (U-Th)/He geochronology showed that the Yandera deposit formed during a period of rapid denudation/exhumation of the New Guinea Highlands. Analysis of published ages conducted in this thesis for deposits in the Southwest Pacific indicates that the temporal distribution of these deposits is not random, suggesting region-scale controls on the formation of such deposits. This implies large scale tectonic and/or mantle processes play a part in the formation of such deposits. Possible geodynamic scenarios are discussed in the final chapter.
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Koloa, Mura, and n/a. "National development planning in Papua New Guinea." University of Canberra. Management, 1993. http://erl.canberra.edu.au./public/adt-AUC20060815.124347.

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4

Lomas, G. C. J. (Gabriel Charles Jacques). "The Huli language of Papua New Guinea." Australia : Macquarie University, 1989. http://hdl.handle.net/1959.14/22313.

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Анотація:
Thesis (PhD) -- Macquarie University, School of English and Linguistics, 1989.
Bibliography: leaves 385-393.
Introduction -- Traditional Huli society -- Segmental phonology -- Prosodies -- Verbs -- Adverbials -- NominaIs -- Word complexes -- Group complexes -- Semantic patterns -- Linguistic and social change -- Texts.
This thesis describes the language of the Huli speech community of the Southern Highlands of Papua New Guinea. The first chapter situates the speech community in its historical setting, and refers to previous, mainly non-linguistic, studies. The second chapter situates the commuity in its geographical and 'traditional' setting, recording putative migrations and dialectal variations. The third chapter describes segmental phonology at a level of detail not previously given in accounts of the language, while the fourth chapter presents a tentative exploration of prosodic features. The fifth chapter describes verbs, the sixth adverbials, and the seventh nominals: in each instance there is an emphasis on morphology and morphophonemic processes hitherto unrecorded for Huli. The eighth chapter describes word complexes, and the ninth group complexes, using a systemic-functional approach that establishes a descriptive framework that indicates useful insights into the pragmatics of the language. Chapter ten selects and explores, in varying degrees, semantic features that are typologically interesting, while chapter eleven re-focusses the thesis on sociolinguistic issues. The twelveth chapter presents a dozen texts, which it interprets and comments on in the light of linguistic and sociological descriptions presented previously. The appendices that follow give the data bases for some of the descriptions given in the thesis body. The body of the thesis is concerned with describing the language as it is being created and used by living, real, people. Hence, the language forms at each level are described and interpreted in relation to their functions in creating meaning. This has necessitated presenting in some detail phonological and morphological data that need to be described if the language is to be seen as the growing, changing expression of the living society that uses and creates it.
Mode of access: World Wide Web.
xviii, 452 leaves, ill
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5

Barnish, G. "Studies on Strongloides in Papua New Guinea." Thesis, University of Liverpool, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.383456.

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Lomas, G. C. J. "The Huli language of Papua New Guinea." Phd thesis, Australia : Macquarie University, 1989. http://hdl.handle.net/1959.14/22313.

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Abers, Geoffrey Alexander. "Active tectonics and seismicity of New Guinea." Thesis, Massachusetts Institute of Technology, 1989. http://hdl.handle.net/1721.1/51475.

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Wittwer, Glyn. "Price stabilisation of coffee in Papua New Guinea /." Title page, contents and summary only, 1990. http://web4.library.adelaide.edu.au/theses/09EC/09ecw832.pdf.

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Bun, Krufinta. "MONITORING WUCHERERIA BANCROFTI ELIMINATION IN PAPUA NEW GUINEA." Case Western Reserve University School of Graduate Studies / OhioLINK, 2019. http://rave.ohiolink.edu/etdc/view?acc_num=case1560346194908835.

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Stewart, Lynn Leslie. "Our people are like gardens" : music, performance and aesthetics among the Lolo, West New Britain Province, Papua, New Guinea." Thesis, University of British Columbia, 1989. http://hdl.handle.net/2429/30917.

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Relationships among the Aesthetic, culture, and music are problematic- Frequently considered as epiphenomenal to culture, music and the arts are typically seen as adjuncts to ceremonial activity- This dissertation examines the nature of the Aesthetic, music and performance in the context of the Lolo, Araigilpua Village, West New Britain Province, Papua New Guinea, in an attempt to develop a definition of the Aesthetic applicable for cross-cultural research and to discover the ways in which the Aesthetic and culture articulate. For the purposes of this dissertation, the Aesthetic is defined as that facet of religion focused on responses to extraordinary powers thought to maintain what are considered to be proper relationships between human members of a community and extraordinary powers. Three forms of aesthetics, social, performance, and musical, are taken as the means and methods of directing interactions between man and extraordinary powers. At present, the Lolo are engaged in a process of secularisation resulting primarily from the introduction of Christianity, Western medicine and money. This dissertation examines the relationship between the Aesthetic and social life, and addresses the impact of changes to the Aesthetic.
Arts, Faculty of
Anthropology, Department of
Graduate
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Книги з теми "Tectonics of Papua New Guinea"

1

Mobbs, Kim. Tectonic interpretation of the Papua New Guinea region from repeat satellite measurements. Sydney, NSW, Australia: School of Geomatic Engineering, University of New South Wales, 1997.

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2

Gascoigne, Ingrid. Papua New Guinea. New York: M. Cavendish, 1998.

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3

Gascoigne, Ingrid. Papua New Guinea. New York: M. Cavendish, 1998.

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4

Fox, Mary Virginia. Papua New Guinea. Chicago: Childrens Press, 1994.

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5

McConnell, Fraiser. Papua New Guinea. Oxford, England: Clio Press, 1988.

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6

Rowan, McKinnon, Murray Jon, and Wheeler Tony 1946-, eds. Papua New Guinea. 6th ed. Hawthorn, Vic: Lonely Planet, 1998.

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Papua New Guinea. 2nd ed. New York: Marshall Cavendish Benchmark, 2009.

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8

Hunter, John. Papua New Guinea phrasebook. South Yarra, Vic., Australia: Lonely Planet, 1986.

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9

K, Tanham George. Papua New Guinea today. Santa Monica, Calif: Rand, 1990.

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10

Dodwell, Christina. In Papua New Guinea. London: Pan, 1985.

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Частини книг з теми "Tectonics of Papua New Guinea"

1

Matsuyama, Masafumi, and Harry Yeh. "Effects of Tsunami at Sissano Lagoon, Papua New Guinea: Submarine-Landslide, and Tectonics Origins." In Submarine Landslides and Tsunamis, 151–62. Dordrecht: Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-010-0205-9_15.

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2

Lee, Sang-Mook, and Etienne Ruellan. "Tectonic and magmatic evolution of the Bismarck Sea, Papua New Guinea: Review and new synthesis." In Back-Arc Spreading Systems: Geological, Biological, Chemical, and Physical Interactions, 263–86. Washington, D. C.: American Geophysical Union, 2006. http://dx.doi.org/10.1029/166gm14.

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3

Sweet, S., and E. A. Silver. "Tectonics and Slumping in the Source Region of the 1998 Papua New Guinea Tsunami from Seismic Reflection Images." In Landslide Tsunamis: Recent Findings and Research Directions, 1945–68. Basel: Birkhäuser Basel, 2003. http://dx.doi.org/10.1007/978-3-0348-7995-8_9.

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4

van der Borg, H. H., M. Koning van der Veen, and L. M. Wallace-Vanderlugt. "Papua New Guinea." In Horticultural Research International, 566–68. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-0003-8_46.

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5

Kidd, R. W. "Papua New Guinea." In The GeoJournal Library, 409–14. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2999-9_44.

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Taylor, Ann C. M. "Papua New Guinea." In International Handbook of Universities, 721. London: Palgrave Macmillan UK, 1993. http://dx.doi.org/10.1007/978-1-349-12912-6_117.

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7

Turner, Barry. "Papua New Guinea." In The Stateman’s Yearbook, 978–82. London: Palgrave Macmillan UK, 2007. http://dx.doi.org/10.1007/978-1-349-74024-6_244.

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Turner, Barry. "Papua New Guinea." In The Statesman’s Yearbook, 983–87. London: Palgrave Macmillan UK, 2008. http://dx.doi.org/10.1007/978-1-349-74027-7_244.

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9

Peaslee, Amos J. "Papua New Guinea." In Constitutions of Nations, 1101–211. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-017-1147-0_4.

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Tapo, Michael, and Pedro G. Cortez. "Papua New Guinea." In Emerging Challenges and Trends in TVET in the Asia-Pacific Region, 185–97. Rotterdam: SensePublishers, 2011. http://dx.doi.org/10.1007/978-94-6091-391-4_17.

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Тези доповідей конференцій з теми "Tectonics of Papua New Guinea"

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Gold, D. ,. P. "New Tectonic Reconstructions of New Guinea Derived from Biostratigraphy and Geochronology." In Digital Technical Conference. Indonesian Petroleum Association, 2020. http://dx.doi.org/10.29118/ipa20-g-61.

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Biostratigraphic data from exploration wells in Papua, West Papua of Indonesia, Papua New Guinea and Australia were reviewed, revised and updated using modern stratigraphic interpretations. Revised stratigraphic interpretations were combined with zircon U-Pb geochronologic data to produce new tectonic reconstructions of the Indonesian provinces of West Papua and Papua. Zircon U-Pb geochronologic data used in this study include new results from the Papuan Peninsula, combined with existing datasets from West Papua, Papua New Guinea, eastern Australia and New Caledonia. Supplementary geochronologic data were used to provide independent validation of the biostratigraphic data. Findings from a compilation of biostratigraphic and zircon age data provide a framework to produce new tectonic models for the origin of New Guinea’s terranes. Two hypotheses are presented to explain observations from the biostratigraphic and geochronologic data. The ‘Allochthonous Terrane’ Model suggests that many of the terranes are allochthonous in nature and may have been derived from eastern Australia. The ‘Extended Rift’ Model suggests that the New Guinea Terranes may have been separated from north-eastern Australia by an elongate rift system far more extensive than previously described. These new tectonic models are essential for our geological understanding of the regional and can be used to drive successful petroleum exploration in this frontier area.
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Swift*, Michael, and Hugh Davies. "A History of Extensional, Compressional, Foreland and Now Extensional Tectonics in South Eastern Papua New Guinea." 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/ice2015-2208854.

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3

Albrecht, Robert, John Calame, Mike Cook, Ignacio Falcon, and Patrick Lee. "High-Pressure Natural Gas Pipeline in Geohazard Region of Papua New Guinea Sustains Mw7.5 Earthquake: Key Factors of Successful Outcome." In 2020 13th International Pipeline Conference. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/ipc2020-9473.

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Abstract ExxonMobil PNG Limited (EMPNG) operates the Papua New Guinea Liquefied Natural Gas Project (PNG LNG), an integrated LNG project comprising wellpads, gathering lines, gas conditioning plant, onshore and offshore export pipelines, liquefaction plant and marine terminal in Papua New Guinea (PNG). The PNG LNG project is a joint venture with participation by ExxonMobil, Oil Search Limited (OSL), Kumul Petroleum, Santos, JX Nippon Oil and Gas Exploration and Mineral Resources Development Company, and began production in 2014. The highlands of PNG presents a challenging physical environment, with high rainfall, steep terrain, active tectonics and seismicity, and ongoing landsliding and erosion. The PNG LNG onshore gas and condensate pipelines confront these physical challenges by having to traverse approximately 150 km of steep volcanic, mudstone and Karstic highlands along the Papuan Fold and Thrust Belt, the modern leading edge of active mountain-building, plus an additional 150 km in Karstic lowlands. During design, construction and operations of the pipelines, ExxonMobil has addressed these challenges in partnership with the engineering, construction and specialist consulting communities. On February 25th, 2018 (UTC) a Magnitude 7.5 earthquake struck the PNG highlands. The event, along with its approximately 300 aftershocks, caused widespread community impact, landsliding and damage to over 1000s of km2, and was centered directly under the highlands portion of the PNG LNG pipelines. The pipelines however, did not lose containment or pressure, and, following inspections and repairs to the PNG LNG gas conditioning plant, PNG LNG production was restored within seven weeks of the main shock. This technical paper and companion oral presentation discuss the key factors of this successful outcome, in particular the sustained condition of the gas and condensate pipelines. Contributing factors to the pipeline’s success include route selection, pipe material specification, early commitment to field studies, careful assessment of geohazards, high awareness of off-ROW community impacts, micro-routing during construction, and active geohazard management during startup and operations. The paper demonstrates that, with respect for the host community, thoughtful engineering, careful construction and ongoing surveillance, pipelines can be safely and successfully designed, constructed and operated in remote and extreme geohazardous environments.
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Dow, Michael J., Christopher Marcel Schmickl, Angus Ian Ross, and Dion Baggio. "Introduction of an Innovative Rotary Steerable System in Papua New Guinea Improves Drilling Performance in Poor Quality Wellbores with Tectonic Breakout." In SPE Asia Pacific Oil and Gas Conference and Exhibition. Society of Petroleum Engineers, 2011. http://dx.doi.org/10.2118/147809-ms.

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Christopherson, Karen R. "Magnetotellurics in Papua New Guinea." In SEG Technical Program Expanded Abstracts 1989. Society of Exploration Geophysicists, 1989. http://dx.doi.org/10.1190/1.1889606.

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Bampton, Alvin. "Teaching computer science in Papua New Guinea." In the 6th annual conference on the teaching of computing and the 3rd annual conference. New York, New York, USA: ACM Press, 1998. http://dx.doi.org/10.1145/282991.283004.

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7

Nose, Masahiko. "The Habitual Pastin Amele, Papua New Guinea." In GLOCAL Conference on Asian Linguistic Anthropology 2019. The GLOCAL Unit, SOAS University of London, 2019. http://dx.doi.org/10.47298/cala2019.2-4.

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Анотація:
This study attempts to clarify the tense systems in Madang Province, Papua New Guinea; particularly, the past tense and habitual past forms in the sample three languages in the area: Amele, Waskia, and Kobon. This study thus investigates past tense and habitual features, and discusses how the people in the area interpret past events. The study then discusses how these people map their temporal frames in their grammars (“anthropology of time”, Gell 1996). To aid analysis, I collected data through observing descriptive grammars and fieldwork, finding that Amele exhibits three types of past tense and habitual tense forms, as in (1). Kobon has two distinct simple and remote past tenses, as in (2). Kobon has habitual aspect with the help of the verb “to be.” Waskia, in contrast, has a distinction between realis and irrealis meanings, and the realis forms can indicate past and habitual meanings (two habitual forms: one is include in realis, another is with the help of the verb “stay”), as shown in (3). (1) Amele: Today’s past: Ija hu-ga. “I came (today).” Yesterday’s past: Ija hu-gan. “I came (yesterday).” Remote past: Ija ho-om. “I came (before yesterday).” Habitual past (by adding the habitual form “l”): Ija ho-lig. “I used to come.” (2) Kobon (Davies 1989): Simple past: Yad au-ɨn. “I have come.” Remote past: Nöŋ-be. “You saw” Habitual aspect (by using the verb “mid” to be): Yad nel nipe pu-mid-in. “I used to break his firewood.” (3) Waskia (Ross and Paol 1978): Realis: Ane ikelako yu naem. “I drank some water yesterday.” (simple past) Realis: Ane girako yu no-kisam “In the past I used to drink water” (habitual past) Habitual (by using the verb “bager“ (stay)): Ane girako yu nala bager-em. “In the past I used to drink water.“ Finally, this study claims that Amele and Kobon have remoteness distinctions; near and remote past distinctions, but there is no such a distinction in Waskia. The observed habitual usages are different to each other. Nevertheless, the three languages have a grammatical viewpoint of habitual past mapping.
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Wagner, E. R., and M. S. Juneau. "Helicopter-Supported Drilling Operation in Papua New Guinea." In SPE/IADC Drilling Conference. Society of Petroleum Engineers, 1991. http://dx.doi.org/10.2118/21926-ms.

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Gibson, W. R., C. L. Lawson, and R. L. Crowson. "Alliance Drilling in Papua New Guinea: A Case History." In SPE/IADC Drilling Conference. Society of Petroleum Engineers, 1995. http://dx.doi.org/10.2118/29335-ms.

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M. Hoversten, G. "Papua New Guinea MT: looking where seismic is blind." In 54th EAEG Meeting. European Association of Geoscientists & Engineers, 1992. http://dx.doi.org/10.3997/2214-4609.201410392.

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Звіти організацій з теми "Tectonics of Papua New Guinea"

1

A., Babon. Snapshot of REDD+ in Papua New Guinea. Center for International Forestry Research (CIFOR), 2011. http://dx.doi.org/10.17528/cifor/003443.

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Papua New Guinea - Contacts with University of Papua and New Guinea. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/04241.

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3

Papua New Guinea - Central Bank - Bank of Papua New Guinea - Accounting Procedures. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/04120.

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Papua New Guinea - Central Bank - Bank of Papua New Guinea - Banking Legislation. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/04133.

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Papua New Guinea - Central Bank - Bank of Papua New Guinea - Banking Legislation. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/04137.

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Papua New Guinea - T.P.N.G. Committee. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/04234.

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Papua New Guinea - Films - Production. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/04019.

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Papua New Guinea - Customs Duty. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/04243.

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Papua New Guinea - Films - Contract. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/04017.

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Papua New Guinea - Meetings - Working Party on Future Currency Arrangement for Papua New Guinea. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/04195.

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