Analysis of Groundwater Level Trends in the Hutton Sandstone, Springbok Sandstone and Condamine Alluvium

Total Page:16

File Type:pdf, Size:1020Kb

Analysis of Groundwater Level Trends in the Hutton Sandstone, Springbok Sandstone and Condamine Alluvium Analysis of groundwater level trends in the Hutton Sandstone, Springbok Sandstone and Condamine Alluvium Surat Cumulative Management Area December 2019 Original version, authorised release in December 2019 by Sanjeev Pandey, Executive Director, Office of Groundwater Impact Assessment. This publication has been compiled by the Office of Groundwater Impact Assessment, Department of Natural Resources, Mines and Energy. Bibliographic reference: OGIA, 2019. Analysis of groundwater level trends in the Hutton Sandstone, Springbok Sandstone and Condamine Alluvium – Surat Cumulative Management Area. OGIA, Brisbane. Copyright statement: © State of Queensland, 2019 The Queensland Government supports and encourages the dissemination and exchange of its information. The copyright in this publication is licensed under a Creative Commons Attribution 4.0 International (CC BY 4.0) licence. Under this licence, you are free, without having to seek our permission, to use this publication in accordance with the licence terms. You must keep intact the copyright notice and attribute the State of Queensland as the source of the publication. Note: Some content in this publication may have different licence terms as indicated. For more information on this licence, visit https://creativecommons.org/licenses/by/4.0/. The information contained herein is subject to change without notice. The Queensland Government shall not be liable for technical or other errors or omissions contained herein. The reader/user accepts all risks and responsibility for losses, damages, costs and other consequences resulting directly or indirectly from using this information. Interpreter statement: The Queensland Government is committed to providing accessible services to Queenslanders from all culturally and linguistically diverse backgrounds. If you have difficulty in understanding this document, you can contact us within Australia on 13QGOV (13 74 68) and we will arrange an interpreter to effectively communicate the report to you. 2019 Analysis of groundwater level trends in the Surat CMA Summary The Office of Groundwater Impact Assessment (OGIA) is responsible for undertaking cumulative impact assessment and establishing management arrangements within areas declared as ‘cumulative management areas’ (CMA). Currently there is one CMA in Queensland, the Surat CMA, established in 2011 in response to coal seam gas (CSG) development in the Surat and southern Bowen basins. OGIA’s impact assessment and management arrangements are established in an Underground Water Impact Report (UWIR), which is revised every three years, providing for an adaptive cycle of reporting-monitoring-research-modelling. The UWIR provides an assessment of regional impacts on groundwater pressures, springs and water supply bores, and establishes integrated management arrangements, such as regional monitoring strategies. Groundwater levels and the interpretation of observed trends are key data that underpin the impact assessment. At any given point in time, the observed trends may be influenced by a number of factors, which can be grouped into two categories: water balance (e.g. recharge, discharge, CSG groundwater extraction and non-CSG water use) and non-water balance (e.g. earth tides, barometric pressure and mechanical loading). This report is focussed on unpacking the impacts of CSG groundwater extraction from the Walloon Coal Measures on the observed groundwater level trends in adjacent aquifers – the Springbok Sandstone, Hutton Sandstone and Condamine Alluvium. In order to separate CSG impacts from other water balance factors (i.e. non-CSG water use), it is necessary to establish background aquifer conditions. Once background conditions and trends are established or contextualised, CSG impacts may then be inferred where there is a deviation from background trends. However, there are a number of challenges that make establishing background trends difficult, including the following: Many of the aquifers adjacent to the CSG reservoir have extensive current and historical non- CSG water use for which there is limited metering. The distribution of dedicated monitoring infrastructure prior to CSG commencement is limited to areas where aquifers are generally shallow or at outcrop, reflecting the primary areas of historical non-CSG water use. In the early stages of development, CSG impacts in adjacent aquifers are likely to represent a relatively minor component of the observed trends, and may be within the bounds of uncertainty associated with other more influential factors, such as climatic variations and estimated non-CSG water use. Consequently, OGIA applied a multiple-lines-of-evidence approach, including both qualitative and quantitative methods, to establish the nature of the trends and determine the likely causes of those trends. Specifically, the approach integrates statistical methods (Mann-Kendall and Spearman correlation), sub-regional and local-scale hydrogeological conceptualisation and numerical modelling. The outcomes from these individual methods are then integrated to assess where observed trends are interpreted to be influenced by CSG groundwater extraction. The Walloon Coal Measures is the primary reservoir for CSG development in the Surat Basin. Within the Upper Juandah and Taroom coal measures, groundwater level declines (up to 300 m) are largely restricted spatially to gas fields and the immediately surrounding areas. Drawdowns of greater than 10 m are rarely observed further than 10 km away from active CSG development areas. Office of Groundwater Impact Assessment i 2019 Analysis of groundwater level trends in the Surat CMA In the Springbok Sandstone – overlying the Walloon Coal Measures – variable groundwater level trends are observed. Consistent with previous predictions, there is evidence of CSG impacts at some locations, particularly where connectivity is enhanced due to local geological features such as faults. Three sites – Kenya East GW4, Broadwater GW11 and Isabella 7M – are identified as likely to be affected by CSG groundwater extraction. In the Hutton Sandstone – an aquifer underlying the Walloon Coal Measures – widespread declining groundwater level trends are observed. The observed trends in the available data correlate well with rainfall patterns – particularly in outcrop areas – and with non-CSG water use in the Hutton Sandstone, both inside and outside CSG production areas. There are no discernible changes in the rate of decline that correlate with CSG groundwater extraction. At this stage, there is no evidence to suggest that declining trends in the Hutton Sandstone are due to CSG groundwater extraction. Non-CSG water use from the aquifer itself is likely to be the primary cause of the declining trends. CSG depressurisation may be a contributing factor in some areas, but there is currently no definitive evidence at this stage. Some CSG impacts are predicted in the longer term in the Hutton Sandstone. The Condamine Alluvium is a major water supply aquifer. In some areas, groundwater levels have been depressed by more than 25 m since the 1960s. Groundwater level trends have been analysed along the western flank of the alluvial aquifer, the area closest to existing CSG development areas. In combination with very low head differences (<20 m for most areas), it is unlikely that CSG impacts have occurred in the Condamine Alluvium at this stage. Overall, the analysis suggests that there is definitive evidence of widespread CSG impact in the Walloon Coal Measures. In the overlying Springbok Sandstone, the groundwater level trends are mixed and there is evidence at some sites of CSG impact. In the underlying Hutton Sandstone, pronounced declining trends are observed, but these are likely to be due to increasing non-CSG water use. There is no evidence of significant CSG impact in the Hutton Sandstone at this stage. Ongoing analysis of water level trends is important for understanding groundwater system dynamics, such as flow directions, and for the identification of impacts from CSG and non-CSG development. Analysis of the influences on observed groundwater level trends in aquifers adjacent to CSG reservoirs will continue to be a major focus for OGIA during the next three-year cycle. Office of Groundwater Impact Assessment ii 2019 Analysis of groundwater level trends in the Surat CMA Table of contents 1 Introduction ................................................................................................................................... 1 1.1 Background .................................................................................................................................... 1 1.2 Project purpose .............................................................................................................................. 1 1.3 Report scope .................................................................................................................................. 2 1.4 Study area ...................................................................................................................................... 2 1.5 Relationship with other studies ....................................................................................................... 2 1.6 Report layout .................................................................................................................................. 4 2 Regional context ........................................................................................................................... 6
Recommended publications
  • Geology and Mineral Resources of the Northern Territory
    Geology and mineral resources of the Northern Territory Ahmad M and Munson TJ (compilers) Northern Territory Geological Survey Special Publication 5 Chapter 41: Eromanga Basin BIBLIOGRAPHIC REFERENCE: Munson TJ, 2013. Chapter 41: Eromanga 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. Eromanga Basin Current as of May 2012 Chapter 41: EROMANGA BASIN TJ Munson INTRODUCTION geology and regolith). However, the southwestern margins of the basin are exposed in SA and the northeastern part of The ௘Cambrian±"Devonian Warburton Basin, the basin in central Qld is also exposed and has been eroding Carboniferous±Triassic 3edirNa Basin and Jurassic± since the Late Cretaceous.
    [Show full text]
  • Annual Report for Epc 1031 from April 20
    ANNUAL REPORT FOR EPC 1031 FROM APRIL 20, 2009 TO APRIL 19, 2010 Arrow Energy Limited Arrow Energy Limited ACN 078 521 936 Level 19, AM-60, 42-60 Albert Street BRISBANE QLD 4000 GPO Box 5262, BRISBANE QLD 4001 Telephone: 61-7-3105 3400 Facsimile: 61-7-3105 3401 Email: [email protected] CONTENTS 1.0 INTRODUCTION 1 1.1 Location & Infrastructure 1 1.2 Tenure Details 1 1.3 Exploration Summary 1 2.0 REGIONAL GEOLOGY 4 2.1 Paleozoic basement 4 2.2 Bowen Basin 5 2.3 Jurassic-Cretaceous basins 6 2.4 Surat Basin 7 2.5 Structure 10 3.0 PREVIOUS EXPLORATION 15 4.0 CURRENT PROGRAM 21 5.0 PLANNED EXPLORATION 22 6.0 REFERENCES 23 FIGURES 1 Sub-Block Details and Location Map 2 Regional Location 3 Regional Structure 4 Geology 5 Stratigraphy 6 WCM Stratigraphy 7 Depth to Top WCM 8 Macalister Seam – Net Coal Thickness 9 Juandah Seams – Net Coal Thickness 10 Taroom Seam – Net Coal Thickness 11 Bouguer Gravity Contours 1.0 INTRODUCTION 1.1 Location & Infrastructure EPC 1031 is located within the Surat Basin approximately 300km West of Brisbane, 20km southwest of Dalby, close to major roads and rail links. The Moonie Highway passes through or adjacent to the Northernmost block of the permit. The EPC sits within ATP 683 and PL 198. 1.2 Tenure details EPC 1031 was granted on the 20th of April 2006 for a term of 5 years; comprising 66 sub-blocks. After relinquishment in April 2010, the EPC currently comprises 33 sub- blocks (Figure 1).
    [Show full text]
  • UQ678964 OA.Pdf
    ÔØ ÅÒÙ×Ö ÔØ Investigating the stratigraphy and palaeoenvironments for a suite of newly dis- covered mid-Cretaceous vertebrate fossil-localities in the Winton Formation, Queensland, Australia Ryan T. Tucker, Eric M. Roberts, Vikie Darlington, Steven W. Salis- bury PII: S0037-0738(17)30124-0 DOI: doi:10.1016/j.sedgeo.2017.05.004 Reference: SEDGEO 5195 To appear in: Sedimentary Geology Received date: 23 March 2017 Revised date: 18 May 2017 Accepted date: 21 May 2017 Please cite this article as: Tucker, Ryan T., Roberts, Eric M., Darlington, Vikie, Sal- isbury, Steven W., Investigating the stratigraphy and palaeoenvironments for a suite of newly discovered mid-Cretaceous vertebrate fossil-localities in the Winton Formation, Queensland, Australia, Sedimentary Geology (2017), doi:10.1016/j.sedgeo.2017.05.004 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Investigating the stratigraphy and palaeoenvironments for a suite of newly discovered mid-Cretaceous vertebrate fossil- localities in the Winton Formation, Queensland, Australia Ryan T. Tucker*a,b, Eric M. Robertsb, Vikie Darlingtonb, Steven W. Salisburyc a Department
    [Show full text]
  • The Geology of NSW
    The Geology of NSW The geological characteristics and history of NSW with a focus on coal seam gas (CSG) resources A report commissioned for the NSW Chief Scientist’s Office, May, 2013. Authors: Dr Craig O’Neill1, [email protected] Dr Cara Danis1, [email protected] 1Department of Earth and Planetary Science, Macquarie University, Sydney, NSW, 2109. Contents A brief glossary of terms i 1. Introduction 01 2. Scope 02 3. A brief history of NSW Geology 04 4. Evolution of the Sydney­Gunnedah­Bowen Basin System 16 5. Sydney Basin 19 6. Gunnedah Basin 31 7. Bowen Basin 40 8. Surat Basin 51 9. Clarence­Moreton Basin 60 10. Gloucester Basin 70 11. Murray Basin 77 12. Oaklands Basin 84 13. NSW Hydrogeology 92 14. Seismicity and stress in NSW 108 15. Summary and Synthesis 113 ii A brief Glossary of Terms The following constitutes a brief, but by no means comprehensive, compilation of some of the terms used in this review that may not be clear to a non‐geologist reader. Many others are explained within the text. Tectono­thermal: The involvement of either (or both) tectonics (the large‐scale movement of the Earth’s crust and lithosphere), and geothermal activity (heating or cooling the crust). Orogenic: pertaining to an orogen, ie. a mountain belt. Associated with a collisional or mountain‐building event. Ma: Mega‐annum, or one million years. Conventionally associated with an age in geochronology (ie. million years before present). Epicratonic: “on the craton”, pertaining to being on a large, stable landmass (eg.
    [Show full text]
  • Appendix D Surat Basin Geological Model Surat Basin Stratigraphic Framework April 2012
    Appendix D Surat Basin geological model Surat Basin Stratigraphic Framework April 2012 Surat Basin Stratigraphic Framework April 2012 – Surat Basin Stratigraphic Framework April 2012 Table of Contents 1. Introduction .................................................................................................................................... 4 2. Methodology ................................................................................................................................... 8 2.1. Area of Interest ....................................................................................................................... 8 2.2. Datasets .................................................................................................................................. 8 2.3. Geological Modelling ............................................................................................................ 10 3. Regional Structure ........................................................................................................................ 12 4. Geological Descriptions ................................................................................................................. 17 4.1. Base Jurassic Unconformity .................................................................................................. 17 4.2. Precipice Sandstone .............................................................................................................. 17 4.3. Evergreen Formation ...........................................................................................................
    [Show full text]
  • Wandoan Coal – Appendix 8A
    APPENDIX 8-A KEY TO GEOLOGICAL MAPPING SYMBOLS Geological Group or key Structural Era Period / Epoch Formation Name Lithological Description symbol association Element Valley and Floodplain Cainozoic Quaternary / undifferentiated Qa Alluvium Recent cover Clay, silt, sand, gravel; floodplain alluvium Sediments Valley and Floodplain Cainozoic Quaternary / undifferentiated Qf Floodout Sheets and Small Fans Recent cover Sand, gravel, clay: floodout sheets and small fans Sediments Valley and Floodplain Cainozoic Quaternary / undifferentiated Cz Floodplain Alluvium Recent cover Soil, sand Sediments Valley and Floodplain Cainozoic Pleistocene Qpa Floodplain Alluvium Recent cover Clay, silt, sand, gravel; flood plain alluvium on high terraces Sediments Duricrusted palaeosols at the top of deep weathering profiles, including ferricrete and silcrete; duricrusted old land Cainozoic Tertiary Td Duricrustic Palaeosols surfaces Mesozoic Middle Jurassic - Late Jurassic Ji Injune Creek Group Surat Basin Calcareous lithic sandstone, siltstone, mudstone, coal, conglomerate Pale brown to pale grey, poorly sorted, medium-grained, feldspathic sublabile sandstone (at base) and fine-grained, Mesozoic Middle Jurassic Jh Hutton Sandstone Bundamba Group Surat Basin well-sorted quartzose sandstone (at top); minor dark grey carbonaceous siltstone, mudstone and rare pebble conglomerate Labile and sublabile, fine to medium-grained sandstone, carbonaceous mudstone, siltstone and minor coal; local Mesozoic Early Jurassic Je Evergreen Formation Bundamba Group Surat Basin
    [Show full text]
  • Geodynamic Synthesis of the North Queensland Region and Implications for Metallogeny
    GEOSCIENCE AUSTRALIA Geodynamic Synthesis of the North Queensland Region and Implications for Metallogeny Natalie Kositcin, David C. Champion and David L. Huston Record 2009/30 GeoCat # 69159 APPLYING GEOSCIENCE TO AUSTRALIA’S MOST IMPORTANT CHALLENGES Geodynamic Synthesis of the North Queensland Region and Implications for Metallogeny GEOSCIENCE AUSTRALIA RECORD 2009/30 by N. Kositcin1, D. C. Champion1 and D.L. Huston1 1. Onshore Energy and Minerals Division, Geoscience Australia, GPO Box 378, Canberra ACT 2601 Department of Resources, Energy and Tourism Minister for Resources and Energy: The Hon. Martin Ferguson, AM MP Secretary: John Pierce Geoscience Australia Chief Executive Officer: Dr Neil Williams PSM © Commonwealth of Australia, 2009 This work is copyright. Apart from any fair dealings for the purpose of study, research, criticism, or review, as permitted under the Copyright Act 1968, no part may be reproduced by any process without written permission. Copyright is the responsibility of the Chief Executive Officer, Geoscience Australia. Requests and enquiries should be directed to the Chief Executive Of ficer, Geos cience Australia, GPO Box 378 Canberra ACT 2601. 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 978-1-921672-21-7 web ISBN 978-1-921672-22-4 print GeoCat # 69159 Bibliographic refer ence: Kositcin, N., Champion, D.C. and Huston, D.L. 2009. Geodynamic Synthesis of the North Queensland Region and Implications for Metallogeny.
    [Show full text]
  • Springsure, Eulo, Bourke and Bogan River Supergroups
    Knowledge report Ecological and hydrogeological survey of the Great Artesian Basin springs - Springsure, Eulo, Bourke and Bogan River supergroups Volume 1: history, ecology and hydrogeology This report was commissioned by the Department of the Environment on the advice of the Interim Independent Expert Scientific Committee on Coal Seam Gas and Coal Mining. The review was prepared by UniQuest and revised by the Department of the Environment following peer review. September 2014 Ecological and hydrogeological survey of the Great Artesian Basin springs – Volume 1 Copyright © Copyright Commonwealth of Australia, 2014. Ecological and hydrogeological survey of the Great Artesian Basin springs - Springsure, Eulo, Bourke and Bogan River supergroups, Volume 1: history, ecology and hydrogeology, Knowledge report is licensed by the Commonwealth of Australia for use under a Creative Commons By Attribution 3.0 Australia licence with the exception of the Coat of Arms of the Commonwealth of Australia, the logo of the agency responsible for publishing the report, content supplied by third parties, and any images depicting people. For licence conditions see: http://creativecommons.org/licenses/by/3.0/au/ This report should be attributed as ‘Commonwealth of Australia 2014, Ecological and hydrogeological survey of the Great Artesian Basin springs - Springsure, Eulo, Bourke and Bogan River supergroups. Volume 1: history, ecology and hydrogeology, Knowledge report, prepared by UniQuest for the Department of the Environment, Commonwealth of Australia’. The
    [Show full text]
  • Galilee Energy Limited Glenaras Aquifer Injection Management Plan
    Galilee Energy Limited Glenaras Aquifer Injection Management Plan - Hutton Sandstone 28 July 2020 - RevD RDM Hydro Pty Ltd RDM_GLL_GlenarasHuttonIMP_RevD ABN 83 624 788 870 0 3 February 2020 - RevA www.rdmhydro.com.au Glenaras Aquifer Injection Management Plan - Hutton Sandstone Table of Contents 1. Introduction ............................................................................................................... 2 2. Regulatory Context ................................................................................................... 3 2.1. Petroleum & Gas (Production & Safety) Act 2004 ................................................ 3 2.2. Environmental Protection Act 1994 ...................................................................... 3 2.3. CSG Water Management Policy ........................................................................... 4 2.4. Water Act 2000 ..................................................................................................... 4 2.5. Water (Great Artesian Basin and Other Regional Aquifers) Plan ......................... 5 2.6. Environmental Protection (Water) Policy 2009 ..................................................... 5 2.7. Environment Protection and Biodiversity Conservation Act (1999) ...................... 6 2.8. Great Artesian Basin Sustainability Initiative ........................................................ 7 2.9. GAB Springs Recovery Plan ................................................................................ 7 3. Site location and description ..................................................................................
    [Show full text]
  • UQ-SDAAP | Sequence Stratigraphy of the Precipice Sandstone and Evergreen Formation in the Surat Basin 2
    v The University of Queensland Surat Deep Aquifer Appraisal Project (UQ-SDAAP) Scoping study for material carbon abatement via carbon capture and storage Supplementary Detailed Report Sequence stratigraphy of the Precipice Sandstone and Evergreen Formation in the Surat Basin 30 April 2019 Authors Dr Andrew La Croix, The University of Queensland Mr Jiahao Wang, The University of Queensland Mr Sebastian Gonzalez, The University of Queensland Mr Jianhua He, UQ Energy Initiative Prof Jim Underschultz, The University of Queensland Prof Andrew Garnett, The University of Queensland Acknowledgements This working document was prepared for The University of Queensland Surat Deep Aquifer Appraisal Project (UQ-SDAAP), a 3-year, $5.5 million project funded by the Australian Government through the Carbon Capture and Storage Research Development and Demonstration (CCS RD&D) programme, by Coal 21, and The University of Queensland. Citation La Croix A, Wang J, Gonzalez S, He J, Underschultz J & Garnett A (2019), Sequence stratigraphy of the Precipice Sandstone and Evergreen Formation in the Surat Basin, The University of Queensland Surat Deep Aquifer Appraisal Project – Supplementary Detailed Report, The University of Queensland. Referenced throughout the UQ-SDAAP reports as La Croix et al. 2019b. Publication details Published by The University of Queensland © 2019 all rights reserved. This work is copyright. Apart from any use as permitted under the Copyright Act 1968, no part may be reproduced by any process without prior written permission from The University of Queensland. ISBN: 978-1-74272-247-4 Disclaimer The information, opinions and views expressed in this document do not necessarily represent those of The University of Queensland, the Australian Government or Coal 21.
    [Show full text]
  • Cretaceous Faunas and Events, Northern Eromanga Basin, Queensland
    153 by Alex. G. Cook Cretaceous faunas and events, northern Eromanga Basin, Queensland Queensland Museum, PO Box 3300, South Brisbane, QLD 4101, Australia. E-mail: [email protected] The stratigraphy, sedimentary history and have been supplemented by government sponsored stratigraphic paleontology of the northern Eromanga Basin are wells. The stratigraphy for the northern Eromanga is summarised in reviewed in the light of extensive field effort, searching Figure 2. Identified depositional phases include Early Jurassic for Cretaceous vertebrate fossils, in particular dinosaurs. dominantly coarse-grained fluvial deposition, followed by more Prolonged non-marine deposition throughout the subdued Mid-Upper Jurassic–Lower Cretaceous fluvio-lacustrine Jurassic was followed by Lower Cretaceous marine sedimentation. In the Lower Cretaceous a succession of marine incursions which extended to the late Albian. Whilst transgressions and regressions resulted in a series of shallow marine, varyingly fossiliferous deposits, the youngest of which is late Albian. biostratigraphy is underpinned by microfloral Concomitant volcanism to the east which had been active since the assemblages there are three distinct marine faunas Jurassic was more prevalent in the Lower Cretaceous, and was preserved from the late Aptian, early middle Albian and dominated by the Whitsunday Island Volcanic Province (Bryan et late Albian. Effective regression caused by sediment oversupply in the latest Albian heralded the final phase of non-marine deposition in the Eromanga
    [Show full text]
  • The Warnie Volcanic Province: a Jurassic Volcanic Province in 2 Central Australia
    Non-Peer reviewed preprint submitted to EarthARXiv - Paper currently under review in Gondwana Research (as off 1st December 2018) 1 1 The Warnie Volcanic Province: A Jurassic Volcanic Province in 2 Central Australia 3 Jonathon P.A. Hardman1, Simon P. Holford2, Nick Schofield1, Mark Bunch2 Daniel Gibbins3 4 1Department of Geology and Petroleum Geology, University of Aberdeen, Aberdeen, AB24 3FX, UK 5 2Australian School of Petroleum, University of Adelaide, Adelaide, SA 5005, Australia 6 3Vintage Energy, 58 King William Road, Goodwood SA 5034, Australia 7 8 Abstract 9 The Cooper and Eromanga Basins of South Australia and Queensland are the largest onshore hydrocarbon 10 producing region in Australia. Igneous rocks have been documented infrequently within end of well reports over 11 the past 34 years, with a late Triassic to Jurassic age determined from well data. However, the areal extent and 12 nature of these basaltic rocks were largely unclear. Here, we integrate seismic, well, gravity and magnetic data 13 to clarify the extent and character of igneous rocks preserved within Eromanga Basin stratigraphy overlying the 14 Nappamerri Trough of the Cooper Basin. We recognise mafic monogenetic volcanoes that extend into tabular 15 basalt lava flows, igneous intrusions and, more locally, hydrothermally altered compound lava flows. The volcanic 16 province covers ~7500 km2 and is proposed to have been active between ~180-160 Ma. We deem this Jurassic 17 volcanic province the Warnie Volcanic Province after the Warnie East 1 exploration well, drilled in 1985. The 18 distribution of extrusive and intrusive igneous rocks is primarily controlled by basement structure, with extrusive 19 and intrusive igneous rocks elongate in a NW-SE direction.
    [Show full text]