Geology of New Ireland, Papua New Guinea

by P. D. Hohnen

Publisher: Australian Govt. Pub. Service in Canberra

Written in English
Published: Pages: 39 Downloads: 758
Share This

Places:

  • Papua New Guinea,
  • New Ireland Province.
  • Subjects:

    • Geology -- Papua New Guinea -- New Ireland Province.,
    • Mines and mineral resources -- Papua New Guinea -- New Ireland Province.
    • Edition Notes

      StatementP.D. Hohnen.
      SeriesBulletin / Department of National Development, Bureau of Mineral Resources, Geology and Geophysics ;, 194, PNG / Department of National Development, Bureau of Mineral Resources, Geology and Geophysics ;, 12, Bulletin (Australia. Bureau of Mineral Resources, Geology and Geophysics) ;, 194., Report PNG ;, 12.
      Classifications
      LC ClassificationsQE340 .A39 no. 194, QE349.N45 .A39 no. 194
      The Physical Object
      Paginationv, 39 p. :
      Number of Pages39
      ID Numbers
      Open LibraryOL1923803M
      ISBN 100642029040
      LC Control Number90135874

Woodlark Island, known to its inhabitants simply as Woodlark or Muyua, is the main island of the Woodlark Islands archipelago, located in Milne Bay Province and the Solomon Sea, Papua New Guinea.. Although no formal census has been conducted since , the current population is estimated at approximately people (see section below on Population Issues).Coordinates: 9°7′35″S °48′20″E / °S . Get this from a library! Geophysical data collected in by the R/V S.P. Lee in the Manus and New Ireland regions of Papua New Guinea. [Michael S Marlow; Geological Survey (U.S.);]. Fergusson Island, largest of the D’Entrecasteaux Islands, Papua New Guinea, in the southwestern Pacific island lies 30 miles (50 km) across Ward Hunt Strait from the southeastern tip of New Guinea, in the Solomon is separated from Goodenough Island (northwest) by Moresby Strait and from Normanby Island (southeast) by Dawson Strait. Keywords: Country update, geothermal projects, Lihir, Papua New Guinea ABSTRACT Geothermal power development, presently focused on tiny Lihir Island, located about kilometers northeast of the national capital, Port Moresby, forms part of the New Ireland Province of Papua New Guinea. Unusual challenges.

Coastal and Marine Geology Program: Description: 7 p. Larger Work Type: Book: Larger Work Title: Geology and offshore resources of Pacific Island Arcs: New Ireland and Manus region, Papua New Guinea: First page: Last page: Country: Papua New Guinea: Online Only (Y/N) N: Additional Online Files (Y/N) N: Google Analytic Metrics: Metrics. Any fiction set in Papua New Guinea Score A book’s total score is based on multiple factors, including the number of people who have voted for it and how highly those voters ranked the g: New Ireland. Lissenung Island Resort is a minute boat ride from Kavieng town in New Ireland Province. There are 7 ocean-front rooms (6 with private facilities) in 4 spread-out duplex bungalows, furnished with hardwood floors and spacious verandahs. Tropical and international alfresco dining enhance your experience of island life. Other than a handful of local staff, you won't see . Tectonic plates activity in the PNG area. (Modified after Hamilton ()) Papua New Guinea comprises the eastern half of the island of Guinea in the western Pacific Ocean (the western half being part of Indonesia), together with New Ireland, New Britain and Bougainville and a number of smaller islands. It has a mountainous spine, rising to.

Lihir volcano forms the small Lihir Island, the largest of a group of island north of New Ireland (Papua New Guinea). It is the largest of the volcanic chain east of New Ireland. Lihir is composed of 5 overlapping basaltic stratovolcanoes, including Luise, Kinami, and Huniho. 4 y. Feldspathoid-bearing potassic rocks and associated types from volcanic islands off the coast of New Ireland, Papua New Guinea: a preliminary account of geology and petrology. In Volcanism in Australasia (pp. ). Elsevier Amsterdam. Lindley, I. D. (). Late Quaternary geology of Ambitle Volcano, Feni Island Group, Papua New Guinea. Books with the subject: Papua New Guinea. Up to 20 books are listed, in descending order of popularity. Ladolam Gold deposit (Lihir Mine), Luise Stratovolcano, Lihir Island, New Ireland Province, Papua New Guinea: A gold mine and the world's largest known low-sulfidation epithermal gold deposit. It is located in an active hydrothermal system. Ore formation involved an earlier un-economic porphyry stage, and a.

Geology of New Ireland, Papua New Guinea by P. D. Hohnen Download PDF EPUB FB2

Buy Geology of New Ireland, Papua New Guinea (Bulletin / Department of National Development, Bureau of Mineral Resources, Geology and Geophysics) on FREE SHIPPING on qualified orders.

Get this from a library. Geology of New Ireland, Papua New Guinea. [P D Hohnen]. Hydrocarbon potential of the Bougainville and southeastern New Ireland Basins, Papua New Guinea (Report / Geological Survey of Papua New Guinea) [W.

D Stewart] on *FREE* shipping on qualifying : W. D Stewart. New Guinea Island is politically divided along °E long. into Papua New Guinea (PNG) to the east and the Indonesian province of Irian Jaya to the west.

The western part of the island is one of the few remaining land areas in the world where Cited by: 7. ISBN: OCLC Number: Description: pages: illustrations ; 28 cm: Contents: Tripartite study of the New Ireland-Manus Region, Papua New Guinea: an introduction / N.F. Exon, M.S. Marlow --Geology of New Ireland and Djaul Islands, Northeastern Papua New Guinea / W.D.

Stewart, M.J. Sandy --Stratigraphy of Manus Island, Western New Ireland Basin, Papua New. This W-NW belt known as New Guinea Mobile Belt, a km wide zone of continuos belt from Papua Nugini to Irian Jaya (Dow et al., ).

The New Guinea Mobile Belt is terminated by EW trending continental strike-slip fault, the Tarera-Aiduna Fault Zone (TAFZ), at Bird’s g: New Ireland.

The part of the New Ireland basin studied here is a fore-arc basin which contains Neogene sediments, and lies between two ridges formed as part of an old north-facing arc-trench system in the Oligocene and Miocene. The southern ridge is the old volcanic axis and consists of volcanic rocks forming New Ireland, New Hannover, and the Admiralty : N.

Exon, D. Tiffin. Volume: 66 () Issue: 7. (July) First Page: Last Page: Title: Geology of Offshore New Ireland Basin in Northern Papua, New Guinea: ABSTRACT Author(s): N. Exon, D. Tiffin Article Type: Meeting abstract Abstract: The mi ( km) wide New Ireland basin extends north-westward from southwest of Bougainville to north of the Admiralty Islands.

We have. Geological Survey of Papua New Guinea, and CCOP/SOPAC (Suva). The aim of all these studies is to better assess the petroleum geology of this arcuate northwest-trending basin, which ex• tends km from northwest of Manus Island to east of New Ireland, and averages km in width (Fig.

Papua New Guinea is one of nearly countries illustrated on our Blue Ocean Laminated Map of the World. This map shows a combination of political and physical features.

It includes country boundaries, major cities, major mountains in shaded relief, ocean depth in blue color gradient, along with many other features. [Geological map of Papua New Guinea, New Ireland and New Britain] [cartographic material] Wikipedia Citation Please see Wikipedia's template documentation for further citation fields that may be required.

New Ireland, island of the Bismarck Archipelago, Papua New Guinea, southwestern Pacific island, lying just north of New Britain, from which it is separated by St. George’s Channel, has an area of 3, square miles (8, square km).

It stretches for about miles ( km) from northwest to southeast but is very narrow, with the. New Guinea (Tok Pisin: Niugini; Hiri Motu: Niu Gini; Indonesian: Papua, historically, Irian) is a large island separated by the shallow Torres Strait from the rest of the Australian is the world's second-largest island, after Greenland, covering a land area ofkm 2 (, sq mi), and the largest island wholly or partly within the Southern Hemisphere and on: Melanesia.

New Ireland (Tok Pisin: Niu Ailan) or Latangai, is a large island in Papua New Guinea, approximately 7, km 2 (2, sq mi) in area with c.

people. It is named after the island of is the largest island of New Ireland Province, lying northeast of the island of New islands are part of the Bismarck Archipelago, named after Otto von Archipelago: Bismarck Archipelago.

DOI: /j Corpus ID: A new species of Cethosia and a new subspecies of Delias (Lepidoptera: Nymphalidae and Pieridae) from New Ireland, Papua New Guinea. Australia took control inin the early stages of World War I, and renamed the island as New Ireland, after the island of Ireland.

It became part of the Mandated Territory of New Guinea declared in by the League of Nations and administered by l: Kavieng. Papua New Guinea is a young and dynamic country, with a very complex geological-tectonic history.

But in short summary, its history has involved volcanic arc initiation, closure and accretion over the last 30 million years. This resulted in several belts of porphyry deposits in continental and oceanic settings. New Ireland’s never-ending beaches, popular cultural festivals, smattering of islands and uncrowded reefs and waves make it a dream destination in Papua New Guinea.

If you’re looking to do some diving, surfing or blue water game fishing, New Ireland will keep you very busy. Hire a canoe from the beachfront in Kavieng and spend a leisurely day exploring the islands.

For. The island of New Guinea, comprising the Independent State of Papua New Guinea in the east A vast amount of literature dating from addresses the geology of New Guinea (for a • Tectonics of the New Guinea Region Missing: New Ireland.

Sediment cores were recovered from the New Ireland Basin, east of Papua New Guinea, in order to investigate the late Quaternary eruptive history Cited by: 8. This is a List of islands in Papua New Guinea, as to most of its main islands, by Province listed NW to SE.

[1] Numbered provinces in Papua New Guinea, referred to in the text. Age: Cenozoic ( - 66 Ma) Lithology: Volcanic rocks Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database.

doi: / Geological Survey of Canada, Open File []. Biologically, New Ireland is one of the least biologically studied regions of Papua New Guinea—its mountainous southern zone has long been considered both a high priority for biodiversity conservation and a major "scientific unknown." Conservation International agreed to organize a rapid assessment of the forests and wildlife of southern New Author: Bruce M.

Beehler. GEOLOGY AND OFFSHORE RESOURCES OF PACIFIC ISLAND ARCS- NEW IRELAND AND MANUS REGION, PAPUA NEW GUINEA. Circum-Pacific Council for Energy and Mineral Resources Earth Science Series, Volume 9.

GEOLOGY AND OFFSHORE RESOURCES OF PACIFIC ISLAND ARCS- NEW IRELAND AND MANUS REGION, PAPUA NEW GUINEA. The Weitin Fault runs across the southern tip of New Ireland, Papua New Guinea and marks the boundary between the Bismark and the Pacific plate with an interseismic slip rate of ~13 cm/year.

Onit produced a M w earthquake, which according to our optical image correlation results, ruptured the surface for over 30 km and Author: Kejie Chen, Kejie Chen, Chris Milliner, Jean‐Philippe Avouac.

Ambitle is a volcanic island which, together with Babase, another volcanic island, is one of the two Feni Islands in the Bismarck Archipelago. The island is located within the Papua New Guinea 's New Ireland Province, to the east of the island of New Ireland.

Ambitle is a stratovolcano, reaching metres (1, feet) above sea on: Bismarck Archipelago, Papua New Guinea. Papua New Guinea. The mines Ok Tediis located in the remote western part of the Papua New Guinea mainland some 18 kilometres east of the border with Indonesia.

It is a large, porphyry copper-gold system including skarns and is hosted by dioritic stocks of Miocene age. Ok Tedi is a large-scale open-cut. Reference: Noku, S.K., Akasaka, M. & Matsueda, H. (): The Crater Mountain Deposit, Papua New Guinea: Porphyry-related Au-Te System.

Resource Geology, 61, ; Noku, S., & Akasaka, M. Geology and Mineralogy of Crater Mountain deposit, Papua New Guinea.

In Abstracts for Annual Meeting of the Mineralogical Society of Japan Abstracts for the 50th. Submarine Gold Mineralization Near Lihir Island, New Ireland Fore-Arc, Papua New Guinea Sven Petersen Department of Economic Geology and Leibniz Laboratory for Applied Marine Research, Freiberg University of Mining and Technology, Brennhausga Cited by: Lihir volcano forms the small Lihir Island, the largest of a group of island north of New Ireland (Papua New Guinea).

It is the largest of the volcanic chain east of New Ireland. Lihir is composed of 5 overlapping basaltic stratovolcanoes, including Luise, Kinami, and Huniho.

4 young submarine volcanoes offshore Lihir Island belong to the. Books Advanced Search New Releases Best Sellers & More Children's Books Textbooks Textbook Rentals Best Books of the Month of results for Books: History: Australia & Oceania: Papua New Guinea.Towards development--the long history of petroleum exploration in Papua New Guinea / F.

K. Rickwood --Fifty years of oil search / S. Warren Carey --Geofinder traversing and data computation / G. J. Carman --Seismic images of Papua New Guinea / S. Pono --The use and limitations of non-seismic geophysics in the Papuan Thrust Belt / A. J. Billings.The Lihir group of islands, located in New Ireland Province of Papua New Guinea, is home to the Lihir language.

The main island, Aniolam, has been the site of a major gold-mining operation since The mine and its attendant economic development have ushered in a period of dramatic social and political : Karl Neuhaus.