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Australia's Natural
Parliament of Australia Department of Parliamentary Services Parliamentary Library Information, analysis and advice for the Parliament RESEARCH PAPER www.aph.gov.au/library 1 April 2008, no. 25, 2007–08, ISSN 1834-9854 Australia’s natural gas: issues and trends Mike Roarty Science, Technology, Environment and Resources Section Executive summary • Australia has limited crude oil but is relatively well endowed with natural gas resources. The natural gas industry has shown remarkable growth—both the domestic and export sectors—over the last few decades and this is projected to continue. • The bulk of Australia’s gas resources are located long distances from the eastern Australian markets. These are offshore northwest Western Australia (Carnarvon and Browse basins) and in the Timor Sea to the north of Australia (Bonaparte Basin). Because of the uneven distribution of our gas resources it had been thought that gas would need to be piped from these fields when the closer smaller eastern fields run down prior to 2020. • The above scenario is now less likely with the development of newer gas fields in the Gippsland, Bass and Otway Basins located offshore in southern Victoria. Furthermore, there has been rapid development of coal seam gas reserves in Queensland and New South Wales with the potential to become a major source of gas for eastern Australia. • The natural gas export sector is presently supplied from the North West Shelf and Bayu- Undan, Darwin. Additional export volumes are expected from the North West Shelf in late 2008 and thereafter from a number of new ventures including Greater Gorgon, Pluto, Pilbara LNG, and Browse Gas all in Western Australia, and coal seam gas field developments in Queensland and New South Wales. -
Seabed Habitats and Hazards of the Joseph Bonaparte Gulf and Timor Sea, Northern Australia
GEOSCIENCE AUSTRALIA Seabed Habitats and Hazards of the Joseph Bonaparte Gulf and Timor Sea, Northern Australia Rachel Przeslawski, James Daniell, Tara Anderson, J. Vaughn Barrie, Andrew Heap, Michael Hughes, Jin Li, Anna Potter, Lynda Radke, Record Justy Siwabessy, Maggie Tran, Tanya Whiteway and Scott Nichol 2011/40 GeoCat # 72805 APPLYING GEOSCIENCE TO AUSTRALIA’S MOST IMPORTANT CHALLENGES Seabed Habitats and Hazards of the Joseph Bonaparte Gulf and Timor Sea, Northern Australia GEOSCIENCE AUSTRALIA RECORD 2011/40 by Rachel Przeslawski1, James Daniell1, Tara Anderson1, J. Vaughn Barrie2, Andrew Heap1, Michael Hughes3, Jin Li1, Anna Potter1, Lynda Radke1, Justy Siwabessy1, Maggie Tran1, Tanya Whiteway1, Scott Nichol1 1. Geoscience Australia, GPO Box 378, Canberra, ACT 2601 2. Geological Survey of Canada – Pacific, Natural Resources Canada, PO Box 6000, Sidney British Columbia, Canada 3. Current Address: Office of the Chief Scientist, GPO Box 9839, Canberra, ACT 2601 Department of Resources, Energy and Tourism Minister for Resources and Energy: The Hon. Martin Ferguson, AM MP Secretary: Mr Drew Clarke Geoscience Australia Chief Executive Officer: Dr Chris Pigram © Commonwealth of Australia (Geoscience Australia) 2011 With the exception of the Commonwealth Coat of Arms and where otherwise noted, all material in this publication is provided under a Creative Commons Attribution 3.0 Australia Licence (http://creativecommons.org/licenses/by/3.0/au/) Geoscience Australia has tried to make the information in this product as accurate as possible. However, it does not guarantee that the information is totally accurate or complete. Therefore, you should not solely rely on this information when making a commercial decision. ISSN 1448-2177 ISBN 978-1-921954-51-1 GeoCat # 72805 Bibliographic reference: Przeslawski, R., Daniell, J., Anderson, T., Barrie, J.V., Heap, A., Hughes, M., Li, J., Potter, A., Radke, R., Siwabessy, J., Tran, M., Whiteway, T., Nichol, S. -
The Future of Australian LNG Exports
September 2014 The Future of Australian LNG Exports: Will domestic challenges limit the development of future LNG export capacity? David Ledesma, James Henderson* & Nyrie Palmer** OIES PAPER: NG 90 *Senior Research Fellows, OIES, **Senior Regulatory Officer, NSW Resources and Energy The contents of this paper are the authors’ sole responsibility. They do not necessarily represent the views of the Oxford Institute for Energy Studies or any of its members. Copyright © 2014 Oxford Institute for Energy Studies (Registered Charity, No. 286084) This publication may be reproduced in part for educational or non-profit purposes without special permission from the copyright holder, provided acknowledgment of the source is made. No use of this publication may be made for resale or for any other commercial purpose whatsoever without prior permission in writing from the Oxford Institute for Energy Studies. ISBN 978-1-78467-008-5 September 2014: The Future of Australian LNG Exports ii Acknowledgments The authors would like to thank everyone who helped us in drafting the paper, in Australia as well as the UK. Your contributions have helped to enrich the document and ensure accuracy of the content and conclusions September 2014: The Future of Australian LNG Exports iii Preface With seven the new LNG projects under construction and due for completion in the 2014 – 2018 timeframe amounting in addition to existing facilities, Australia is expected to overtake Qatar as the world’s largest supplier of LNG by the end of the 2010s. With its plentiful gas reserves, prior track record of LNG project execution and operation and relative proximity to the fast growing Asian LNG markets the degree of comparative advantage would seem to guarantee a benign investment environment. -
Pdf [12] Whittam, D.B., Norvick, M.S
International Journal of Geosciences, 2016, 7, 792-827 Published Online June 2016 in SciRes. http://www.scirp.org/journal/ijg http://dx.doi.org/10.4236/ijg.2016.76061 Geological Conditions and Hydrocarbon Accumulation Processes in the Sahul Platform, Northern Bonaparte Basin, Australia Rakotondravoavy Jules1,2*, Jiaren Ye1, Qiang Cao1 1Key Laboratory of Tectonics and Petroleum Resources, China University of Geosciences, MOE, Wuhan, China 2Département des Sciences de la Terre et de l'Environnement à la Faculté des Sciences de Technologies et de l’Environnement de l'Université de Mahajanga, Mahajanga, Madagascar Received 14 May 2016; accepted 26 June 2016; published 29 June 2016 Copyright © 2016 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/ Abstract The Sahul Platform where the Sunset-Loxton Shoals and Chuditch gas fields were discovered is lo- cated between the Timor Trough to the north and the Malita Graben to the south. These areas are located respectively 440 km and 380 km northwest of Darwin in the northern Bonaparte Basin, Australia. Based on the structural evolution of the northern Bonaparte Basin, data from the wells Loxton Shoals 1, Sunset 1 and Chuditch 1 in the Sahul Platform and Heron 1 in the Malita Graben depocentre, and the Seismic Line N11606 were used to clarify the geological conditions and re- construct the hydrocarbon accumulation processes in the study area. BasinMod 1-D, 2-D, and 3-D software was used for modeling. The Plover Formation source rock was a poor-to-good hydrocar- bon generative potential and reached the middle to late mature oil window in the Sunset-Loxton Shoals field whereas in the Chuditch field, it was an overall fair-to-good hydrocarbon generative potential, and attained the Late mature oil window. -
Basin Evolution Palispatic Model of Bonaparte Basin, Australia Northwest Shelf
Journal of Applied Geology, vol. 2(2), 2017, pp. 94–108 DOI: http://dx.doi.org/10.22146/jag.39988 Basin Evolution Palispatic Model of Bonaparte Basin, Australia Northwest Shelf Nomensen Ricardo,∗ Hendra Amijaya, and Salahuddin Husein Department of Geological Engineering, Faculty of Engineering, Gadjah Mada University, Yogyakarta, Indonesia ABSTRACT. This research area is located on the Australian NW Shelf close to the western edge of the Sahul Platform. This research is aimed to generate the palispatic basin model of Bonaparte Basin, Australian Northwest Shelf. It is to predict the impact of Neogene col- lision on the petroleum system distribution on Australian Northwest Shelf. The main data used in this research are seismic data using qualitative method analysis. The well data is used to well-seismic tied. After data acquisition, the seismic data are interpreted based on the horizon and structure interpretation. These interpretation are to reconstruct the basin evolution thorough geologic time. According to data analysis, the basin evolution pal- ispatic model are divided into Paleo-proterozoic, Paleozoic, Triassic, Early Jurassic, Mid- dle Jurassic, Late Jurassic, Early Cretaceous, Late Cretaceous, Early Eocene, Late Miocene and Recent condition. Regional tectonically there are at least three important events in NW Shelf: Middle Triassic-Jurassic NNE–SSW extension phase, Late Jurassic NE–SW ex- tension phase and the Neogen collision phase; the Neogen collision effects on Northwest Shelf Australia. These three events contributed in forming and disturbing the Paleozoic and Mesozoic petroleum system in Bonaparte basin especially. Keywords: Neogene collision · Basin evolution · Palispatic model · Petroleum system · Australian northwest self. 1I NTRODUCTION blocks and horst. -
Total Petroleum Systems Of
TOTAL PETROLEUM SYSTEMS OF THE BONAPARTE GULF BASIN AREA, AUSTRALIA: JURASSIC, EARLY CRETACEOUS-MESOZOIC; KEYLING, HYLAND BAY- PERMIAN; MILLIGANS-CARBONIFEROUS, PERMIAN by Michele G. Bishop1 Open-File Report 99-50-P 1999 This report is preliminary and has not been reviewed for conformity with the U. S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade names is for descriptive purposes only and does not imply endorsements by the U. S. government. U. S. Department of the Interior U. S. Geological Survey 1Consultant, Wyoming PG-783, contracted to U. S. Geological Survey, Denver, Colorado FOREWORD This report was prepared as part of the World Energy Project of the U.S. Geological Survey. In this project, the world was divided into 8 regions and 937 geologic provinces, which were then ranked according to the discovered oil and gas volumes within each (Klett and others, 1997). Then, 76 "priority" provinces (exclusive of the U.S. and chosen for their high ranking) and 26 "boutique" provinces (exclusive of the U.S. and chosen for their anticipated petroleum richness or special regional economic importance) were selected for appraisal of oil and gas resources. Portions of numerous additional "boutique" provinces were eventually included. The petroleum geology of these priority and boutique provinces is described in this series of reports. The purpose of the World Energy Project is to assess the quantities of oil, gas, and natural gas liquids that have the potential to be added to reserves within the next 30 years. These volumes either reside in undiscovered fields whose sizes exceed the stated minimum- field-size cutoff value for the assessment unit (variable, but must be at least 1 million barrels of oil equivalent) or occur as reserve growth of fields already discovered. -
Pinnacle Features at the Base of Isolated Carbonate Buildups Marking Point Sources of Fluid Offshore Northwest Australia
Van Tuyl et al. Pinnacle features at the base of isolated carbonate buildups marking point sources of fluid offshore Northwest Australia James Van Tuyl†, Tiago M. Alves, and Lesley Cherns 3D Seismic Laboratory, School of Earth and Ocean Sciences, Cardiff University, Main Building, Park Place, CF10 3AT Cardiff, UK ABSTRACT of the North West Shelf after the early Oligo GEOLOGICAL SETTING cene (RosleffSoerensen et al., 2012; Belde We investigated pinnacle features at the et al., 2017; Rankey, 2017). To understand what Mesozoic–Cenozoic Evolution of base of late Oligocene–Miocene isolated controls carbonate growth on equatorial mar the Browse Basin carbonate buildups using three-dimensional gins, it is important to explain the onset of iso seismic and borehole data from the Browse lated carbonate buildup growth in the Browse The Browse Basin is an offshore sedimentary Basin, Northwest Australia. Brightened seis- Basin, and in similar carbonate sequences basin on Australia’s North West Shelf, a north mic reflections, dim spots, and other evidence in the Browse Basin. eaststriking passive continental margin devel of fluid accumulation occur below most pin- Locally, Howarth and Alves (2016) mapped oped from the Late Jurassic to the present day nacle features. An important observation is clustered fluidflow features above late Oligo (Fig. 1; Stephenson and Cadman, 1994; Rosleff- that all pinnacles generated topography on cene–Miocene karst systems and within iso Soerensen et al., 2012, 2016). Located on the successive late Oligocene–Miocene paleo- lated carbonate buildups. These fluidflow fea southeast edge of the Timor Sea, the Browse seafloors, therefore forming preferential tures were interpreted as being associated with Basin exhibits a marginparallel, landwarddip zones for the settlement of reef-building or- a salt diapir at depth, despite: (1) the absence ping halfgraben geometry (Fig. -
Ü Structural Landforms
S3 STRUCTURAL ü LANDFORMS C. R. Twidale S&v * ' - NN . ^ . - % - ia w sT4C! P^% „ * * * a i t V - W**5uM ■ fS-T fc: 'r. Jjgg* • r_-i •'.-« g w Up to the end of last century, landforms were viewed largely as expressions of the structure of the earth’s underlying crust. But such interpretations were concerned for the most part with generalities and broad effects; the subtleties of structural factors became overshadowed first by cyclic ex planations and then by the modern emphasis on process and climatic geomorphology. This book arose from the neglect of struc tural factors in geomorphological interpre tation. Nowadays it is recognised that details of jointing and faulting, both past and present, of the stresses in folds, of past conditions of sedimentation, all play an important part in the determination of present landforms. Moreover, today’s geo morphologists must think in terms not only of distribution—length and breadth—but also in terms of vertical and temporal change. The author brings this new thinking into Structural Landforms and the result is a book of great interest and importance to students of geography and geology, to teachers and professional geomorphologists. It is particularly rich in photographs and line figures, and includes an excellent biblio graphy. Price in Australia $5.00 This book was published by ANU Press between 1965–1991. This republication is part of the digitisation project being carried out by Scholarly Information Services/Library and ANU Press. This project aims to make past scholarly works published by The Australian National University available to a global audience under its open-access policy. -
Bonaparte Basin
Department of Industry Tourism and Resources Geoscience Australia Australian Petroleum Accumulations Report 5 – 2nd Edition BONAPARTE BASIN NORTHERN TERRITORY (NT) WESTERN AUSTRALIA (WA) TERRITORY OF ASHMORE & CARTIER ISLANDS ADJACENT AREA (AC) JOINT PETROLEUM DEVELOPMENT AREA (JPDA) S.J.Cadman and P.R.Temple Petroleum Greenhouse Gas and Advice Group 2003 Copyright Commonwealth of Australia, 2003. This work is copyright. Apart from any fair dealing for the purpose of study, research, criticism or review, as permitted under the Copyright Act 1968, no part may be reproduced without prior written permission of the Executive Director, Geoscience Australia. ISBN 0 642 46782 X Preferred way to cite this publication : Cadman, S.J. and Temple, P.R., 2003. Bonaparte Basin, NT, WA, AC & JPDA, Australian Petroleum Accumulations Report 5, 2nd Edition, Geoscience Australia, Canberra. Other reports in the Australian Petroleum Accumulations series : 1. Amadeus Basin, Northern Territory, 1986. 2. Bass Basin, Victoria and Tasmania, 1987. 3. Gippsland Basin, Victoria, 1987. 4. Adavale Basin, Queensland, 1988. 5. Bonaparte Basin, Northern Territory and Western Australia, 1st Edition, 1989. 6. Otway Basin, Victoria and South Australia, 1990. 7. Browse Basin, Western Australia, 1991. 8. Carnarvon Basin, Western Australia, 1993. 9. Canning Basin, Western Australia, 1993. 10. Perth Basin, Western Australia, 1994. 11. Bowen and Surat Basins, Clarence-Moreton Basin, Sydney Basin, Gunnedah Basin and other minor onshore basins, Queensland, NSW and NT, 1998. CONTENTS -
Basin Evolution Palispatic Model of Bonaparte Basin, Australia Northwest Shelf
Journal of Applied Geology, vol. 2(2), 2017, pp. 94–108 DOI: http://dx.doi.org/10.22146/jag.39988 Basin Evolution Palispatic Model of Bonaparte Basin, Australia Northwest Shelf Nomensen Ricardo,∗ Hendra Amijaya, and Salahuddin Husein Department of Geological Engineering, Faculty of Engineering, Gadjah Mada University, Yogyakarta, Indonesia ABSTRACT. This research area is located on the Australian NW Shelf close to the western edge of the Sahul Platform. This research is aimed to generate the palispatic basin model of Bonaparte Basin, Australian Northwest Shelf. It is to predict the impact of Neogene col- lision on the petroleum system distribution on Australian Northwest Shelf. The main data used in this research are seismic data using qualitative method analysis. The well data is used to well-seismic tied. After data acquisition, the seismic data are interpreted based on the horizon and structure interpretation. These interpretation are to reconstruct the basin evolution thorough geologic time. According to data analysis, the basin evolution pal- ispatic model are divided into Paleo-proterozoic, Paleozoic, Triassic, Early Jurassic, Mid- dle Jurassic, Late Jurassic, Early Cretaceous, Late Cretaceous, Early Eocene, Late Miocene and Recent condition. Regional tectonically there are at least three important events in NW Shelf: Middle Triassic-Jurassic NNE–SSW extension phase, Late Jurassic NE–SW ex- tension phase and the Neogen collision phase; the Neogen collision effects on Northwest Shelf Australia. These three events contributed in forming and disturbing the Paleozoic and Mesozoic petroleum system in Bonaparte basin especially. Keywords: Neogene collision · Basin evolution · Palispatic model · Petroleum system · Australian northwest self. 1I NTRODUCTION blocks and horst. -
Bonaparte Basin. In
Geology and mineral resources of the Northern Territory Ahmad M and Munson TJ (compilers) Northern Territory Geological Survey Special Publication 5 Chapter 36: Bonaparte Basin BIBLIOGRAPHIC REFERENCE: Ahmad M and Munson TJ, 2013. Chapter 36: Bonaparte Basin: in Ahmad M and Munson TJ (compilers). ‘Geology and mineral resources of the Northern Territory’. Northern Territory Geological Survey, Special Publication 5. Disclaimer While all care has been taken to ensure that information contained in this publication is true and correct at the time of publication, changes in circumstances after the time of publication may impact on the accuracy of its information. The Northern Territory of Australia gives no warranty or assurance, and makes no representation as to the accuracy of any information or advice contained in this publication, or that it is suitable for your intended use. You should not rely upon information in this publication for the purpose of making any serious business or investment decisions without obtaining independent and/or professional advice in relation to your particular situation. The Northern Territory of Australia disclaims any liability or responsibility or duty of care towards any person for loss or damage caused by any use of, or reliance on the information contained in this publication. Bonaparte Basin Current as of November 2012 Chapter 36: BONAPARTE BASIN M Ahmad and TJ Munson INTRODUCTION onshore coastal areas along the NT–Western Australia border northward into the Timor Sea across Australia’s The Bonaparte Basin (previously referred to as Bonaparte continental margin. The basin covers an area of Gulf Basin, Figure 36.1) is a large, predominantly offshore, approximately 270 000 km2, with the onshore portion being composite polyphase sedimentary basin, extending from about 20 000 km2. -
Helium in the Australian Liquefied Natural Gas Economy
The APPEA Journal 2018, 58, 209–237 Peer reviewed paper https://doi.org/10.1071/AJ17049 Helium in the Australian liquefied natural gas economy Christopher J. Boreham A,D, Dianne S. Edwards A, Robert J. Poreda B, Thomas H. Darrah C, Ron Zhu A, Emmanuelle Grosjean A, Philip Main A, Kathryn Waltenberg A and Paul A. Henson A AGeoscience Australia, GPO Box 378, Canberra, ACT 2601, Australia. BUniversity of Rochester, Rochester, NY 14627, USA. CSmart Gas Sciences, HCR 67, Box 3, Wilburton, PA 17888, USA. DCorresponding author. Email: [email protected] Abstract. Australia is about to become the premier global exporter of liquefied natural gas (LNG), bringing increased opportunities for helium extraction. Processing of natural gas to LNG necessitates the exclusion and disposal of non- hydrocarbon components, principally carbon dioxide and nitrogen. Minor to trace hydrogen, helium and higher noble gases in the LNG feed-in gas become concentrated with nitrogen in the non-condensable LNG tail gas. Helium is commercially extracted worldwide from this LNG tail gas. Australia has one helium plant in Darwin where gas (containing 0.1% He) from the Bayu-Undan accumulation in the Bonaparte Basin is processed for LNG and the tail gas, enriched in helium (3%), is the feedstock for helium extraction. With current and proposed LNG facilities across Australia, it is timely to determine whether the development of other accumulations offers similar potential. Geoscience Australia has obtained helium contents in ~800 Australian natural gases covering all hydrocarbon-producing sedimentary basins. Additionally, the origin of helium has been investigated using the integration of helium, neon and argon isotopes, as well as the stable carbon (13C/12C) isotopes of carbon dioxide and hydrocarbon gases and isotopes (15N/14N) of nitrogen.