Bibliography of Geology and Geophysics of the Southwestern Pacific
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New Zealand: E&P Review
New Zealand: E&P Review Mac Beggs, Exploration Manager 2 March 2011 Excellence in Oil & Gas, Sydney From the conference flyer - • Major opportunities and • Favourable terms and clean motivations to operate government • Prospectivity – but skewed to high risk offshore frontiers • Access to services and • Adjunct to Australian service sector skills • Major markets • Unencumbered oil export arrangements • Gas market 150-250 BCF/year • Sovereign risk New Zealand Oil & Gas Limited 2 ⎮ Outline • Regulatory framework for E&P in New Zealand • History of discovery and development • Geography of remaining prospectivity • Recent and forecast E&P activities – Onshore Taranaki fairway – Offshore Taranaki fairway – Frontier basins – Unconventional resources • Gas market overview • Concluding comments New Zealand Oil & Gas Limited 3 ⎮ Regulatory Framework for Oil & Gas E&P in New Zealand • Mineral rights to petroleum vested in the Crown, 1937 • Crown Minerals Act 1991 • Royalty and tax take provides for excellent returns to developer/producer (except for marginal and mature assets) – Royalty of 5% net revenue, or 20% accounting profit – Company tax reducing to 28% from 1 April 2011 • Administered by an agency within Ministry of Economic Development (Crown Minerals) www.crownminerals.govt.nz • High profile since change of government in late 2008 – Resources identified as a driver for economic growth – Senior Minister: Hon Gerry Brownlee (until last week) • Continuing reforms should streamline and strengthen administration New Zealand Oil & Gas Limited -
Seismic Interpretation of Structural Features in the Kokako 3D Seismic Area, Taranaki Basin (New Zealand) Edimar Perico*, Petróleo Brasileiro S.A
Seismic interpretation of structural features in the Kokako 3D seismic area, Taranaki Basin (New Zealand) Edimar Perico*, Petróleo Brasileiro S.A. and Dr. Heather Bedle, University of Oklahoma. Summary The Western Platform represents an important tectonic unit The basin experienced different tectonic regimes over time in the Taranaki Basin and can considered a stable region. and the hydrocarbons traps are strongly related to Although, seismic characterization of Late Cretaceous to compressive structures (Coleman, 2018). King and Thrasher Early Miocene intervals reveals changes in the deformation (1996) highlight three main stages for the Taranaki Basin styles of normal faults. In some cases, the features vary development: (1) mid-Late Cretaceous to Paleocene intra- vertically from concentrated brittle zones (main planar continental rift transform; (2) Eocene to Early Oligocene discontinuity) to wide damage areas with deformation passive margin and (3) Oligocene to Recent active margin structures composed by smaller fault segments. In addition, basin. Muir et al. (2000) relates the origin of the basin with possible correlations were presented between structural NE and NNE basement faults formed during mid-Cretaceous features and siliciclastic deposits. Key takeaways from this due to the break-up of Gondwana. Considering the main research can be applied to areas with high hydrocarbon rifting processes, Strogen et al. (2017) recognize two phases: potential to guide the exploration of siliciclastic reservoirs NW to WNW half-grabens (c. 105 – 83 Ma) and an associated with faults. Lastly, the structural features extensional regime responsible for the formation of NE described were correlated with regional settings and help to depocenters (c. 80 – 55 Ma). -
Agricultural Systems of Papua New Guinea Working Paper No
AGRICULTURAL SYSTEMS OF PAPUA NEW GUINEA Working Paper No. 6 MILNE BAY PROVINCE TEXT SUMMARIES, MAPS, CODE LISTS AND VILLAGE IDENTIFICATION R.L. Hide, R.M. Bourke, B.J. Allen, T. Betitis, D. Fritsch, R. Grau, L. Kurika, E. Lowes, D.K. Mitchell, S.S. Rangai, M. Sakiasi, G. Sem and B. Suma Department of Human Geography, The Australian National University, ACT 0200, Australia REVISED and REPRINTED 2002 Correct Citation: Hide, R.L., Bourke, R.M., Allen, B.J., Betitis, T., Fritsch, D., Grau, R., Kurika, L., Lowes, E., Mitchell, D.K., Rangai, S.S., Sakiasi, M., Sem, G. and Suma,B. (2002). Milne Bay Province: Text Summaries, Maps, Code Lists and Village Identification. Agricultural Systems of Papua New Guinea Working Paper No. 6. Land Management Group, Department of Human Geography, Research School of Pacific and Asian Studies, The Australian National University, Canberra. Revised edition. National Library of Australia Cataloguing-in-Publication Entry: Milne Bay Province: text summaries, maps, code lists and village identification. Rev. ed. ISBN 0 9579381 6 0 1. Agricultural systems – Papua New Guinea – Milne Bay Province. 2. Agricultural geography – Papua New Guinea – Milne Bay Province. 3. Agricultural mapping – Papua New Guinea – Milne Bay Province. I. Hide, Robin Lamond. II. Australian National University. Land Management Group. (Series: Agricultural systems of Papua New Guinea working paper; no. 6). 630.99541 Cover Photograph: The late Gore Gabriel clearing undergrowth from a pandanus nut grove in the Sinasina area, Simbu Province (R.L. -
Explanatory Notes for the Tectonic Map of the Circum-Pacific Region Southwest Quadrant
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP CP-37 U.S. GEOLOGICAL SURVEY Explanatory Notes for the Tectonic Map of the Circum-Pacific Region Southwest Quadrant 1:10,000,000 ICIRCUM-PACIFIC i • \ COUNCIL AND MINERAL RESOURCES 1991 CIRCUM-PACIFIC COUNCIL FOR ENERGY AND MINERAL RESOURCES Michel T. Halbouty, Chairman CIRCUM-PACIFIC MAP PROJECT John A. Reinemund, Director George Gryc, General Chairman Erwin Scheibner, Advisor, Tectonic Map Series EXPLANATORY NOTES FOR THE TECTONIC MAP OF THE CIRCUM-PACIFIC REGION SOUTHWEST QUADRANT 1:10,000,000 By Erwin Scheibner, Geological Survey of New South Wales, Sydney, 2001 N.S.W., Australia Tadashi Sato, Institute of Geoscience, University of Tsukuba, Ibaraki 305, Japan H. Frederick Doutch, Bureau of Mineral Resources, Canberra, A.C.T. 2601, Australia Warren O. Addicott, U.S. Geological Survey, Menlo Park, California 94025, U.S.A. M. J. Terman, U.S. Geological Survey, Reston, Virginia 22092, U.S.A. George W. Moore, Department of Geosciences, Oregon State University, Corvallis, Oregon 97331, U.S.A. 1991 Explanatory Notes to Supplement the TECTONIC MAP OF THE CIRCUM-PACIFTC REGION SOUTHWEST QUADRANT W. D. Palfreyman, Chairman Southwest Quadrant Panel CHIEF COMPILERS AND TECTONIC INTERPRETATIONS E. Scheibner, Geological Survey of New South Wales, Sydney, N.S.W. 2001 Australia T. Sato, Institute of Geosciences, University of Tsukuba, Ibaraki 305, Japan C. Craddock, Department of Geology and Geophysics, University of Wisconsin-Madison, Madison, Wisconsin 53706, U.S.A. TECTONIC ELEMENTS AND STRUCTURAL DATA AND INTERPRETATIONS J.-M. Auzende et al, Institut Francais de Recherche pour 1'Exploitacion de la Mer (IFREMER), Centre de Brest, B. -
Effects of Pelagic Longline Fishing on Seamount Ecosystems Based on Interviews with Pacific Island Fishers
Effects of Pelagic Longline Fishing on Seamount Ecosystems Based on Interviews with Pacific Island Fishers This publication was prepared by IUCN as a part of the Oceanic Fisheries Management Project, funded by the Global Environment Facility, through the United Nations Development Program. The Project aims to achieve global environmental benefits by enhanced conservation and management of transboundary oceanic fishery resources in the Pacific Islands region and the protection of the biodiversity of the Western Tropical Pacific Warm Pool Large Marine Ecosystem. It is executed by the Pacific Islands Forum Fisheries Agency in conjunction with the Secretariat of the Pacific Community and IUCN. Website: http://www.ffa.int/gef/. The designation of geographical entities in this document, and the presentation of the material, do not imply the expression of any opinion whatsoever on the part of IUCN or contributory organizations concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The views expressed in this publication do not necessarily reflect those of IUCN or contributory organizations, nor does citing of trade names or commercial processes constitute endorsement. Published by: IUCN Oceania Regional Office, Suva, FIJI Copyright: © 2010 International Union for the Conservation of Nature and Natural Resources, Oceania Regional Office. Reproduction of this publication for educational or other non-commercial purposes is authorized without prior written permission from the copyright holders provided the source is fully acknowledged. Reproduction of this publication for resale or other commercial purposes is prohibited without prior written permission of the copyright holders. Cover photos: Interviewing fishermen in Tonga, courtesy of Telmo Morato. -
The Late Castlecliffian and Early Haweran Stratigraphy of the Manawatu and Rangitikei Districts
GSNZ Conference 2006 Manawatu-Rangitikei FieldTrip Guide THE LATE CASTLECLIFFIAN AND EARLY HAWERAN STRATIGRAPHY OF THE MANAWATU AND RANGITIKEI DISTRICTS Griffins Road Quarry. The Upper Griffins Road Tephra is above Brad Pillan’s head. The Middle Griffins Road Tephra is at his waist level, and Brent Alloway is sampling the Lower Griffins Road Tephra just above the Aldworth river gravels (OI 10). 1 2 2 ALAN PALMER , JOHN BEGG , DOUGAL TOWNSEND & KATE 2 WILSON 1 Soil and Earth Sciences, INR, Massey University, PB 11-222, Palmerston North. ([email protected]) 2 Institute of Geological and Nuclear Sciences, PO Box 30-368, Lower Hutt. GSNZ Miscellaneous Publication 122B Supplement 1 ISBN 0-908678-06-1 Page 1 GSNZ Conference 2006 Manawatu-Rangitikei FieldTrip Guide THE LATE CASTLECLIFFIAN AND EARLY HAWERAN STRATIGRAPHY OF THE MANAWATU AND RANGITIKEI DISTRICTS 1 2 2 2 ALAN PALMER , JOHN BEGG , DOUGAL TOWNSEND & KATE WILSON 1 Soil and Earth Sciences, INR, Massey University, PB 11-222, Palmerston North. ([email protected]) 2 Institute of Geological and Nuclear Sciences, PO Box 30-368, Lower Hutt. INTRODUCTION The age of many mid-late Quaternary surfaces in the area between Wanganui and Palmerston North has been poorly known because: 1. The marine terraces are not as well defined as they are west of Wanganui (Pillans, 1990). 2. The wave cut surfaces are difficult to locate, and the underlying sediments are sand dominated and softer. 3. The loess cover on marine and river terraces is of the Pallic Soil facies, i.e. pale grey and mottled, making paleosols difficult to see in the poorly drained loess. -
The Naturalist and His 'Beautiful Islands'
The Naturalist and his ‘Beautiful Islands’ Charles Morris Woodford in the Western Pacific David Russell Lawrence The Naturalist and his ‘Beautiful Islands’ Charles Morris Woodford in the Western Pacific David Russell Lawrence Published by ANU Press The Australian National University Canberra ACT 0200, Australia Email: [email protected] This title is also available online at http://press.anu.edu.au National Library of Australia Cataloguing-in-Publication entry Author: Lawrence, David (David Russell), author. Title: The naturalist and his ‘beautiful islands’ : Charles Morris Woodford in the Western Pacific / David Russell Lawrence. ISBN: 9781925022032 (paperback) 9781925022025 (ebook) Subjects: Woodford, C. M., 1852-1927. Great Britain. Colonial Office--Officials and employees--Biography. Ethnology--Solomon Islands. Natural history--Solomon Islands. Colonial administrators--Solomon Islands--Biography. Solomon Islands--Description and travel. Dewey Number: 577.099593 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying or otherwise, without the prior permission of the publisher. Cover image: Woodford and men at Aola on return from Natalava (PMBPhoto56-021; Woodford 1890: 144). Cover design and layout by ANU Press Printed by Griffin Press This edition © 2014 ANU Press Contents Acknowledgments . xi Note on the text . xiii Introduction . 1 1 . Charles Morris Woodford: Early life and education . 9 2. Pacific journeys . 25 3 . Commerce, trade and labour . 35 4 . A naturalist in the Solomon Islands . 63 5 . Liberalism, Imperialism and colonial expansion . 139 6 . The British Solomon Islands Protectorate: Colonialism without capital . 169 7 . Expansion of the Protectorate 1898–1900 . -
Profiles and Results from Survey Work at Ha’Atafu, Manuka, Koulo and Lofanga
PACIFIC REGIONAL OCEANIC AND COASTAL FISHERIES DEVELOPMENT PROGRAMME (PROCFish/C/CoFish) TONGA COUNTRY REPORT: PROFILES AND RESULTS FROM SURVEY WORK AT HA’ATAFU, MANUKA, KOULO AND LOFANGA (November and December 2001; March to June 2002; April to June, September and October 2008 ) by Kim Friedman, Silvia Pinca, Mecki Kronen, Pierre Boblin, Lindsay Chapman, Franck Magron, Aliti Vun isea and Pierre Labrosse This document has been produced with the financial assistance of the European Community The views expressed herein are those of the Secretariat of the Pacific Community and do not reflect the official opinion of the European Community i ©Copyright Secretariat of the Pacific Community (SPC), 2009 All rights for commercial / for profit reproduction or translation, in any form, reserved. SPC authorises the partial reproduction or translation of this material for scientific, educational or research purposes, provided SPC and the source document are properly acknowledged. Permission to reproduce the document and/or translate in whole, in any form, whether for commercial / for profit or non-profit purposes, must be requested in writing. Original SPC artwork may not be altered or separately published without permission. Original text: English Secretariat of the Pacific Community Cataloguing-in-publication data Tonga country report: profiles and results from survey work at Ha’atafu, Manuka, Koulo and Lofanga (November and December 2001; March to June 2002; April to June, September and October 2008) / by Kim Friedman, Silvia Pinca, Mecki Kronen, Pierre Boblin, Lindsay Chapman, Franck Magron, Aliti Vunisea and Pierre Labrosse (Pacific Regional Oceanic and Coastal Fisheries Development Programme (PROCFish/C/CoFish) / Secretariat of the Pacific Community) I. -
Ritter Island Volcano—Lateral Collapse and the Tsunami of 1888
August 6, 2003 18:4GeophysicalJournalInternational gji2016 Geophys. J. Int. (2003) 154, 891–902 Ritter Island Volcano—lateral collapse and the tsunami of 1888 Steven N. Ward1 and Simon Day2 1Institute of Geophysics and Planetary Physics, University of California, Santa Cruz, CA 95064, USA. E-mail: [email protected] 2Benfield Hazard Research Centre, Department of Earth Sciences, University College, London, Gower Street, London WC1E 6BT. E-mail: [email protected] Accepted 2003 April 9. Received 2003 April 7; in original form 2002 September 8 SUMMARY In the early morning of 1888 March 13, roughly 5 km3 of Ritter Island Volcano fell violently into the sea northeast of New Guinea. This event, the largest lateral collapse of an island volcano to be recorded in historical time, flung devastating tsunami tens of metres high on to adjacent shores. Several hundred kilometres away, observers on New Guinea chronicled 3 min period waves up to 8 m high, that lasted for as long as 3 h. These accounts represent the best available first-hand information on tsunami generated by a major volcano lateral collapse. In this article, we simulate the Ritter Island landslide as constrained by a 1985 sonar survey of its debris field and compare predicted tsunami with historical observations. The best agreement occurs for landslides travelling at 40 m s−1, but velocities up to 80 m s−1 cannot be excluded. The Ritter Island debris dropped little more than 800 m vertically and moved slowly compared with landslides that descend into deeper water. Basal friction block models predict that slides with shorter falls should attain lower peak velocities and that 40+ ms−1 is perfectly compatible with the geometry and runout extent of the Ritter Island landslide. -
Exploration of New Zealand's Deepwater Frontier * GNS Science
exploration of New Zealand’s deepwater frontier The New Zealand Exclusive Economic Zone (EEZ) is the 4th largest in the world at about GNS Science Petroleum Research Newsletter 4 million square kilometres or about half the land area of Australia. The Legal Continental February 2008 Shelf claim presently before the United Nations, may add another 1.7 million square kilometres to New Zealand’s jurisdiction. About 30 percent of the EEZ is underlain by sedimentary basins that may be thick enough to generate and trap petroleum. Although introduction small to medium sized discoveries continue to be made in New Zealand, big oil has so far This informal newsletter is produced to tell the eluded the exploration companies. industry about highlights in petroleum-related research at GNS Science. We want to inform Exploration of the New Zealand EEZ has you about research that is going on, and barely started. Deepwater wells will be provide useful information for your operations. drilled in the next few years and encouraging We welcome your opinions and feedback. results would kick start the New Zealand deepwater exploration effort. Research Petroleum research at GNS Science efforts have identified a number of other potential petroleum basins around New Our research programme on New Zealand's Zealand, including the Pegasus Sub-basin, Petroleum Resources receives $2.4M p.a. of basins in the Outer Campbell Plateau, the government funding, through the Foundation of deepwater Solander Basin, the Bellona Basin Research Science and Technology (FRST), between the Challenger Plateau and Lord and is one of the largest research programmes in GNS Science. -
1 Bibliography 1. Kaa, DJ Van De. the Demography of Papua and New
1 Bibliography 1. Kaa, D. J. van de. The Demography of Papua and New Guinea's Indigenous Population [Ph.D. Dissertation]. Canberra: Australian National University; 1971. xiii, 235 pp. Note: [general PNG]. 2. Kaa, D. J. van de. Estimates of Vital Rates and Future Growth. In: Kaa, D. J. van de; Stanhope, J. M.; Epstein, T. S.; Fry, N. H.; Beltz, C. L. People and Planning in Papua and New Guinea. Canberra and Boroko: Australian National University, New Guinea Research Unit; 1970: 1-23. (New Guinea Research Bulletins; v. 34). Note: [general PNG]. 3. Kaa, D. J. van de. The Future Growth of Papua New Guinea's Indigenous Population. In: Ward, Marion W., Editor. Population Growth and Socio-economic Change: Papers from the Second Demography Seminar, Port Moresby, 1970. Canberra and Boroko: Australian National University, New Guinea Research Unit; 1971: 16-30. (New Guinea Research Bulletins; v. 42). Note: [general PNG]. 4. Kaa, D. J. Van de. Medical Work and Changes in Infant Mortality in Western New Guinea. Papua and New Guinea Medical Journal. 1967; 10: 89-94. Note: [1959-1962: Schouten Is, Fak-Fak, Lower Waropen, Nimboran, Moejoe, Noemfoor]. 5. Kaa, D. J. van de. Opportunities for Research in Papua-New Guinea and Irian Barat: Demography. In: Reeves, Susan C.; Dudley, May. New Guinea Social Science Field Research and Publications 1962-67. Canberra and Port Moresby: Australian National University, New Guinea Research Unit; 1969: 202-203. (New Guinea Research Bulletins; v. 32). Note: [general PNG]. 6. Kaa, D. J. van de. Population Censuses in Papua New Guinea. South Pacific Bulletin. -
Financial Inclusion and Financial Capability
Financial Inclusion and Financial Capability in Morobe and Madang Provinces, Papua New Guinea Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized An initial report of the Papua New Guinea Public Disclosure Authorized National Financial Capability Survey Bank of Papua New Guinea Institute of National Affairs 9363_PNG FinancialCapacitySurvey_1601939_CVR.indd 1 11/19/15 8:17 AM Bank of Papua New Guinea Papua New Guinea Institute for National Affairs The World Bank Financial Inclusion and Financial Capability in Morobe and Madang Provinces Papua New Guinea An initial report of the Papua New Guinea National Financial Capability Survey This Project is financially supported by the Korean Poverty Reduction and Socio-Economic Development Trust Fund II 9363_PNG FinancialCapacitySurvey_1601939_CH00_FM.indd 1 11/18/15 10:15 AM Cataloguing-in-Publication Data ISBN 9980-77-182-8 National Library Service—Papua New Guinea First published: June 2015 Published by: Institute of National Affairs P.O. Box 1530 Port Moresby NCD Papua New Guinea Copyright: This report is a joint product of the project team composed of staff and consultants from Bank of Papua New Guinea, the Institute of National Affairs and The World Bank. The findings, interpretations, and conclusions expressed in this report are entirely those of the authors and should do not necessarily reflect the views of Board of the Bank of Papua New Guinea, the Executive Directors of The World Bank or the governments they represent, or the Board of Institute of National Affairs. The Bank of Papua New Guinea, Institute of National Affairs, and The World Bank do not guarantee the accuracy of the data included in this work.