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Monday, May 11, 2020 | History

3 edition of Geology of New Ireland, Papua New Guinea found in the catalog.

Geology of New Ireland, Papua New Guinea

P. D. Hohnen

Geology of New Ireland, Papua New Guinea

by P. D. Hohnen

  • 87 Want to read
  • 27 Currently reading

Published by Australian Govt. Pub. Service in Canberra .
Written in English

    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

      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.


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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.

Geology of New Ireland 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.