Assessment of Undiscovered Oil and Gas Resources of the Cretaceous-Tertiary Composite Total Petroleum System, Taranaki Basin Assessment Unit, New Zealand
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Carbon Capture and Storage: Setting the New Zealand Scene
Carbon capture and storage: Setting the New Zealand scene Brad Field GNS Science Lower Hutt [email protected] GNS Science The mitigation wedges required to meet 2050 emission target (if only 2o in 2100) 60 CCS 50 40 2 O 30 Gt C 20 10 0 2009 2015 2020 2025 2030 2035 2040 2045 2050 CCS 14% (17%) Power generation efficiency and fuel switching 3% (1%) Renewables 21% (23%) End-use fuel switching 12% (12%) Nuclear 8% (8%) End-use energy efficiency 42% (39%) Percentages represent share of cumulative emissions reductions to 2050. Percentages in brackets represent share of emissions reductions in the year 2050. IEA 2012, GCCSI 2012 GNS Science Deep purple… http://www.smh.com.au/environment/weather/temperatures-off-the-charts-as-australia-turns-deep-purple-20130108-2ce33.html GNS Science The carbon capture, transport and storage process Below ~800 m = liquid CO2CRC GNS Science Geological storage of CO2 claystone seal rock sandstone reservoir rock seal reservoir CO2CRC injected CO2 seal CO2 storage sites: natural gas reservoir • Several kilometres below surface • Similar locations to oil and natural gas GNS Science Typical depth ranges for subsurface resources Interactions could include leakage/migration, and pressure effects IEAGHG Technical Report 2013-08 GNS Science Global scene • 16 large CCS projects currently operating or in construction, with a total capture ~ 36 Mtpa of CO2 • 59 large projects being planned: >110 Mtpa Government support for CCS: • UKP 1,000 M government funding • USD 3,400 M government funding • AUD 1,680 M Flagship Project -
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). -
Hello from Todd Energy
Community Update Issue 29, June 2021 View over the Taramoukou Conservation Area looking south west to Taranaki Maunga HELLO FROM TODD ENERGY... This is my first community update since joining Todd All of this work that we do is to help provide an affordable and Energy in January, and it’s certainly been a busy time reliable energy supply to all New Zealanders as we transition – both for me in the role of CEO and also for the wider to a low emissions economy. We are actively finding ways to reduce our emissions and, while this will remain an ongoing Todd team. I hope this update finds you and your families journey, through our initiatives we were able to reduce our well as we move into the winter months. emissions by 660 tCO2 / year in 2020 – the equivalent of taking 144 cars off the road. On top of that, through the various Last month, we completed our scheduled drilling activities projects we’re implementing this year, we will be able to further at the Mangahewa G wellsite in north Taranaki, bringing the reduce our emissions by 4,500 tCO2 / year – the equivalent of second phase of development to a close. As some of our taking almost 1,000 cars off the road. You can find out more neighbours may have noticed, Todd’s ‘Big Ben’ drilling rig about our efforts to reduce our emissions in this update, and has already been demobilised and relocated to our Kapuni J I look forward to sharing more on this topic over the coming wellsite in south Taranaki. -
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. -
Bibliography of Geology and Geophysics of the Southwestern Pacific
UNITED NATIONS ECONOMIC AND SOCIAL COMMISSION FOR ASIA AND THE PACIFIC COMMITTEE FOR CO-ORDINATION OF JOINT PROSPECTING FOR MINERAL RESOURCES IN SOUTH PACIFIC OFFSHORE AREAS (CCOP/SOPAC) TECIThlJCAL BULLETIN No. 5 BIBLIOGRAPHY OF GEOLOGY AND GEOPHYSICS OF THE SOUTHWESTERN PACIFIC Edited by CHRISTIAN JOUANNIC UNDP Marine Geologist, Technical Secretariat ofCCOPjSOPAC, Suva, Fiji and ROSE-MARIE THOMPSON NiZ. Oceanographic Institute. Wellington Ali communications relating to this and other publications of CCOP/SOPAC should he addressed to: Technical Secretariat of CCOP/SOPAC, cio Mineral Resources Department, Private Bag, Suva, Fiji. This publication should he referred to as u.N. ESCAP, CCOP/SOPAC Tech. Bull. 5 The designations employed and presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the United Nations concerning the legal status ofany country or territory or of its authorities, or concerning the delimitation of the frontiers of any country or territory. Cataloguing in Publication BIBLIOGRAPHY of geology and geophysics of the southwestern Pacifie / edited by Christian Jouannic and Rose-Marie Thompson. - [2nd ed/]. - Suva: CCOP/SOPAC. 1983. (Technical bulletin / United Nations Economie and Social Commission for Asia and the Pacifie, Committee for Co-ordination of Joint Prospecting for Mineral Resources in South Pacifie Offshore Areas, ISSN 0378-6447 : 5) ISBN 0-477-06729-8 1. Jouannic, Christian II. Thompson, Rose Marie III. Series UDC 016:55 (93/96) The publication of this 2nd Edition of the Bibliography of the Geology and Geophysics of the Southwestern Pacifie has been funded by the Office de la Recherche Scientifique et Technique Outre-Mer (ORSTOM, 24 Rue Bayard, 75008 Paris, France) as a contri- bution by ORSTOM to the activities of CCOP/SOPAC. -
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. -
A Coherent Middle Pliocene Magnetostratigraphy, Wanganui Basin, New Zealand
Journal of the Royal Society of New Zealand ISSN: 0303-6758 (Print) 1175-8899 (Online) Journal homepage: http://www.tandfonline.com/loi/tnzr20 A coherent middle Pliocene magnetostratigraphy, Wanganui Basin, New Zealand Gillian M. Turner , Peter J. J. Kamp , Avon P. McIntyre , Shaun Hayton , Donald M. McGuire & Gary S. Wilson To cite this article: Gillian M. Turner , Peter J. J. Kamp , Avon P. McIntyre , Shaun Hayton , Donald M. McGuire & Gary S. Wilson (2005) A coherent middle Pliocene magnetostratigraphy, Wanganui Basin, New Zealand, Journal of the Royal Society of New Zealand, 35:1-2, 197-227, DOI: 10.1080/03014223.2005.9517781 To link to this article: http://dx.doi.org/10.1080/03014223.2005.9517781 Published online: 30 Mar 2010. Submit your article to this journal Article views: 89 View related articles Citing articles: 13 View citing articles Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=tnzr20 Download by: [203.118.162.158] Date: 01 February 2017, At: 18:47 197 Journal of the Royal Society of New Zealand Volume 35, Numbers 1 & 2, March/June, 2005, pp 197-227 A coherent middle Pliocene magnetostratigraphy, Wanganui Basin, New Zealand Gillian M. Turner1, Peter J. J. Kamp2*, Avon P. McIntyre2,3, Shaun Hayton2,4, Donald M. McGuire5, and Gary S. Wilson6 Abstract We document magnetostratigraphies for three river sections (Turakina, Ran- gitikei, Wanganui) in Wanganui Basin and interpret them as corresponding to the Upper Gilbert, the Gauss and lower Matuyama Chrons of the Geomagnetic Polarity Timescale, in agreement with foraminiferal biostratigraphic datums. -
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. -
GNS Staff Publications 2008 A
GNS Staff Publications 2008 A Adams, C.J. 2008 Provenance of gold in Mesozoic mesothermal mineral deposits in New Zealand. p. 39 In: Australian Earth Sciences Convention, Perth, 20 July-24 July, 2008 : program & abstract booklet. Abstracts / Geological Society of Australia 89 Adams, C.J. 2008 Provenance of gold in Mesozoic mesothermal mineral deposits in New Zealand. p. 204 In: Wysoczanski, R. (comp.) Geological Society of New Zealand, New Zealand Geophysical Society, New Zealand Geochemical & Mineralogical Society joint annual conference : Geosciences '08 : programme and abstracts. Geological Society of New Zealand miscellaneous publication 125A Adams, C.J.; Campbell, H.J.; Griffin, W.J. 2008 Age and provenance of basement rocks of the Chatham Islands : an outpost of Zealandia. New Zealand journal of geology and geophysics, 51(3): 245-259 Adams, C.J.; Ireland, T.R. 2008 Provenance connections between Late Neoproterozoic and Early Paleozoic sedimentary basins of the Ross Sea region, Antarctica, southeast Australia and southern Zealandia. Extended abstract 064 In: Cooper, A.K.; Barrett, P.; Stagg, H.; Storey, B.; Stump, E.; Wise, W.; 10th ISAES editorial team; Davey, F.J.; Naish, T.R. (eds) Antarctica : a keystone in a changing world : proceedings of the 10th International Symposium on Antarctic Earth Sciences, Santa Barbara, California, August 26 to September 1, 2007. Open-file report / US Geological Survey 2007-1047 Adams, C.J.; Miller, H.; Toselli, A.J.; Griffin, W.L. 2008 The Puncoviscana Formation of northwest Argentina : U-Pb geochronology of detrital zircons and Rb-Sr metamorphic ages and their bearing on its stratigraphic age, sediment provenance and tectonic setting. Neues Jahrbuch fuer Geologie und Palaeontologie. -
Back Matter (PDF)
Index Page numbers in italic denote Figures. Page numbers in bold denote Tables. Abarratia quarry 188, 190, 192 continental rift margins 1, 53–54, 172–176 accommodation space, rifted continental margins Bay of Biscay and Western Pyrenees 176–199 172–173, 174, 175, 181, 182, 192, 193, 197 Iberia–Newfoundland margin 54–84 Adelaide Supergroup 270, 271, 272–273, 273, 288 magma-poor 240, 243 Adria margin 207, 208, 209, 225 Cretaceous, Hegang Basin 91–114 Adriatic ocean–continent transition 205, 224, 230 Curnamona Craton 270, 271, 272 Alentejo Basin 55 Algarve Basin 55 Da’an Formation 92 Alpine Fault, New Zealand 47 Dampier Ridge 10, 11, 14 Alps, hyperextended margin models 2, 243, 246 de Greer Fault 144, 147 Antes black shale 126, 127, 133 Deep Galicia Margin Appalachian Basin 120 Barremian–Albian sediments 64, 67–68, 76,81 Appalachian margin, foreland basins 120–137 crustal thinning 82–83 Aptian, Iberia–Newfoundland margin 80 hyper-extension 57, 58, 63 Arrouy thrust system 190, 191, 192 Tithonian sediments 62, 64, 70, 72 Arzacq–Maule´on Basin 176, 186, 187–192 Valanginian–Hauterivian 62, 64, 67, 71, 74,81 sedimentary evolution 188–189 Deep-water Taranaki 36, 38, 39,46 see also Maule´on Basin Delamerian Fold Belt 270, 271 Avalonian terrane 54 Delamerian–Ross Orogeny 273, 274, 288, 289, 294 Denglouku Formation 92, 111, 112 Barail Group see Disang–Barail Flysch Belt Depotbugt Basin 148, 151, 152, 155, 163, 164–165 Barremian–Albian rift event 67–68, 76–77,81 Dergholm Granite 279 Bay of Biscay Dimboola Igneous Complex 273, 274, 282, 291, 294 geological -
Seismic Structural Investigation and Reservoir Characterization of the Moki Formation in Maar Field, Taranaki Basin, New Zealand
Scholars' Mine Masters Theses Student Theses and Dissertations Fall 2015 Seismic structural investigation and reservoir characterization of the Moki Formation in Maar Field, Taranaki Basin, New Zealand Mohammed Dhaifallah M Alotaibi Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Geophysics and Seismology Commons Department: Recommended Citation Alotaibi, Mohammed Dhaifallah M, "Seismic structural investigation and reservoir characterization of the Moki Formation in Maar Field, Taranaki Basin, New Zealand" (2015). Masters Theses. 7459. https://scholarsmine.mst.edu/masters_theses/7459 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. iii SEISMIC STRUCTURAL INVESTIGATION AND RESERVOIR CHARACTERIZATION OF THE MOKI FORMATION IN MAAR FIELD, TARANAKI BASIN, NEW ZEALAND By MOHAMMED DHAIFALLAH M ALOTAIBI A THESIS Presented to the Faculty of the Graduate School of the MISSOURI UNIVERSITY OF SCIENCE AND TECHNOLOGY In Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE IN GEOLOGY AND GEOPHYSICS 2015 Approved by Dr. Kelly Liu, Advisor Dr. Stephen Gao Dr. Neil Anderson iv 2015 Mohammed Dhaifallah M Alotaibi All Rights Reserved iii ABSTRACT The Maari Field is a large oil field located in the southern part of the Taranaki Basin, New Zealand. The field is bounded by two major structures, the Eastern Mobile Belt and Western Stable Platform. The Maari Field produces 40,000 BOPD (Barrels of Oil per Day) from five wells from reservoirs in the Moki Formation.