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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). -
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. -
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. -
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. -
Seal Quality and Distribution in the Southern Taranaki Basin Late Cretaceous to Eocene Section and Implications for Hydrocarbon Trapping
SEAL QUALITY AND DISTRIBUTION IN THE SOUTHERN TARANAKI BASIN LATE CRETACEOUS TO EOCENE SECTION AND IMPLICATIONS FOR HYDROCARBON TRAPPING ________________________________________________________________ A thesis submitted in partial fulfilment of the requirements for the Degree of Master of Science in Geology in the University of Canterbury by J. Coyle University of Canterbury 2018 ________________________________________________________________ Contents Abstract ................................................................................................................................................... V Acknowledgments .................................................................................................................................. VI 1. Introduction .................................................................................................................................... 1 1.1 Project Aims and Outline ........................................................................................................ 1 1.2 Geological Overview ............................................................................................................... 4 1.3 Seals ........................................................................................................................................ 5 1.4 Previous and Current Exploration ........................................................................................... 6 2. Overview of the Taranaki Basin ..................................................................................................... -
Megasequence Architecture of Taranaki, Wanganui, and King Country Basins and Neogene Progradation of Two Continental Margin Wedges Across Western New Zealand
Megasequence architecture of Taranaki, Wanganui, and King Country basins and Neogene progradation of two continental margin wedges across western New Zealand Peter JJ Kamp1, Adam J Vonk1, Kyle J Bland1, Angela G Griffin1, Shaun Hayton1&2, Austin JW Hendy1, Avon P McIntyre1, Campbell S. Nelson1, Tim Naish3 1Department of Earth Sciences, The University of Waikato, Private Bag 3105, Hamilton 2001, New Zealand 2Geosphere Exploration Services Ltd, P.O. Box 44 285, Lower Hutt, New Zealand 3Geological and Nuclear Sciences Ltd, P.O. Box 30 368, Lower Hutt Abstract Taranaki, Wanganui and King Country basins (formerly North Wanganui Basin) have been regarded as discrete basins, but they contain a very similar Neogene sedimentary succession and much of their geologi- cal history is held in common. Analysis of the stratigraphic architecture of the fill of each basin reveals the occurrence of four 2nd order megasequences of tectonic origin. The oldest is the early-early Miocene (Otaian Stage) Mahoenui Group/megasequence, followed by the late-early Miocene (Altonian Stage) Mokau Group/megasequence (King Country Basin), both of which correspond to the lower part of the Manganui Formation in Taranaki Basin. The third is the middle to late Miocene Whangamomona Group/megasequence, and the fourth is the latest Miocene-Pleistocene Rangitikei Supergroup/megasequence, both represented in the three basins. Higher order sequences (4th, 5th, 6th), having a eustatic origin, are evident in the Whangamomona and Rangitikei megasequences, particularly those of 5th order with 41 ka periodicity. The distribution of the megasequences are shown in a series of cross-section panels built-up from well -to-well correlations, complemented by time-stratigraphic cross-sections. -
Extensional and Magmatic Nature of the Campbell Plateau and Great South Basin from Deep Crustal Studies
Tectonophysics 472 (2009) 213–225 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Extensional and magmatic nature of the Campbell Plateau and Great South Basin from deep crustal studies J.W.G. Grobys a,⁎, K. Gohl a, G. Uenzelmann-Neben a,B.Davyb, D. Barker b a Alfred Wegener Institute for Polar and Marine Research, PO BOX 120161, 27515 Bremerhaven, Germany b GNS Science, 1 Fairview Drive, Avalon, Lower Hutt 5040, New Zealand ARTICLE INFO ABSTRACT Article history: The Campbell Plateau is one of the largest submarine parts of the microcontinent of New Zealand. Although Received 13 December 2006 the opening of the Great South Basin played an important role in the late Gondwana break-up, the crustal Received in revised form 15 April 2008 structure of the basins and plateaus southeast of New Zealand are unknown to a large extent. Here we Accepted 6 May 2008 present results from a combined gravity, magnetic, multichannel seismic and seismic wide-angle reflection/ Available online 13 May 2008 refraction transect across the Great South Basin and parts of the Campbell Plateau and interpret this on the basis of velocity distribution and crustal thickness. The lower crust exhibits a zone of southeastward Keywords: ≈ – Rift zones increasing P-wave velocities (vp 7.1 7.4 km/s) beneath the central Campbell Plateau. In this area, crustal ∼ Ocean-bottom seismographs thickness averages to 27 km. We interpret this high-velocity zone as underplating beneath a previously Refraction methods extended crust. Our results hint that the extension of the Great South Basin was not accompanied by Crustal thinning widespread magmatic activity, although signs of younger magmatism have been found across the Pukaki Rise Campbell Plateau and within the Great South Basin. -
Tectonic Evolution of the Active Hikurangi Subduction Margin, New Zealand, Since the Oligocene. A
Tectonic evolution of the active Hikurangi subduction margin, New Zealand, since the Oligocene. A. Nicol, C. Mazengarb, Franck Chanier, G. Rait, C. Uruski, L. Wallace To cite this version: A. Nicol, C. Mazengarb, Franck Chanier, G. Rait, C. Uruski, et al.. Tectonic evolution of the active Hikurangi subduction margin, New Zealand, since the Oligocene.. Tectonics, American Geophysical Union (AGU), 2007, Vol.26, pp.TC4002. hal-00350552 HAL Id: hal-00350552 https://hal.archives-ouvertes.fr/hal-00350552 Submitted on 2 Jun 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Copyright TECTONICS, VOL. 26, TC4002, doi:10.1029/2006TC002090, 2007 Tectonic evolution of the active Hikurangi subduction margin, New Zealand, since the Oligocene Andrew Nicol,1 Colin Mazengarb,2 Frank Chanier,3 Geoff Rait,4 Chris Uruski,1 and Laura Wallace1 Received 30 November 2006; revised 21 February 2007; accepted 28 March 2007; published 6 July 2007. [1] Deformation across the active Hikurangi sub- G. Rait, C. Uruski, and L. Wallace (2007), Tectonic evolution of duction margin, New Zealand, including shortening, the active Hikurangi subduction margin, New Zealand, since the extension, vertical-axis rotations, and strike-slip Oligocene, Tectonics, 26, TC4002, doi:10.1029/2006TC002090. -
The Geological History and Hazards of a Long-Lived Stratovolcano, Mt
New Zealand Journal of Geology and Geophysics ISSN: (Print) (Online) Journal homepage: https://www.tandfonline.com/loi/tnzg20 The geological history and hazards of a long-lived stratovolcano, Mt. Taranaki, New Zealand Shane J. Cronin, Anke V. Zernack, Ingrid A. Ukstins, Michael B. Turner, Rafael Torres-Orozco, Robert B. Stewart, Ian E. M. Smith, Jonathan N. Procter, Richard Price, Thomas Platz, Michael Petterson, Vince E. Neall, Garry S. McDonald, Geoffrey A. Lerner, Magret Damaschcke & Mark S. Bebbington To cite this article: Shane J. Cronin, Anke V. Zernack, Ingrid A. Ukstins, Michael B. Turner, Rafael Torres-Orozco, Robert B. Stewart, Ian E. M. Smith, Jonathan N. Procter, Richard Price, Thomas Platz, Michael Petterson, Vince E. Neall, Garry S. McDonald, Geoffrey A. Lerner, Magret Damaschcke & Mark S. Bebbington (2021) The geological history and hazards of a long-lived stratovolcano, Mt. Taranaki, New Zealand, New Zealand Journal of Geology and Geophysics, 64:2-3, 456-478, DOI: 10.1080/00288306.2021.1895231 To link to this article: https://doi.org/10.1080/00288306.2021.1895231 © 2021 The Author(s). Published by Informa Published online: 17 Mar 2021. UK Limited, trading as Taylor & Francis Group Submit your article to this journal Article views: 1817 View related articles View Crossmark data Citing articles: 3 View citing articles Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=tnzg20 NEW ZEALAND JOURNAL OF GEOLOGY AND GEOPHYSICS 2021, VOL. 64, NOS. 2–3, 456–478 https://doi.org/10.1080/00288306.2021.1895231 RESEARCH ARTICLE The geological history and hazards of a long-lived stratovolcano, Mt. -
Māui Field – South Taranaki Basin
Māui Field – South Taranaki Basin Quantitative Spill Modelling Study Prepared by: Prepared for: RPS ERM Suite E1, Level 4 Level 1 140 Bundall Road 60 Leichhardt St Bundall QLD 4217 Spring Hill QLD 4000 T: +61 7 5574 1112 T: +61 7 3839 8393 F: +61 8 9211 1122 F: +61 7 3839 8381 E: [email protected] E: [email protected] W: www.erm.com Client Manager: Nathan Benfer Report Number: MAQ0624J Version / Date: Rev 1 / 19 September 2017 rpsgroup.com.au Māui Field – South Taranaki Basin Quantitative Spill Modelling Study IMPORTANT NOTE Apart from fair dealing for the purposes of private study, research, criticism, or review as permitted under the Copyright Act, no part of this report, its attachments or appendices may be reproduced by any process without the written consent of RPS Australia West Pty Ltd (“RPS” or “we”). All enquiries should be directed to RPS. We have prepared this report for Shell Taranaki Limited (“Client”) for the specific purpose for which it is supplied (“Purpose”). This report is strictly limited to the Purpose including the facts and matters stated within it and is not to be used, directly or indirectly, for any other application, purpose, use or matter. In preparing this report RPS has made certain assumptions. We have assumed that all information and documents provided to us by the Client or as a result of a specific request or enquiry were complete, accurate and up-to-date. Where we have obtained information from a government register or database, we have assumed that the information is accurate. -
The Early Middle Miocene Paleoenvironmental Setting of New Zealand Revista Mexicana De Ciencias Geológicas, Vol
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Field, Brad D.; Crundwell, Martin P.; Kennett, James P.; King, Peter R.; Jones, Craig M.; Scott, George H. The early Middle Miocene paleoenvironmental setting of New Zealand Revista Mexicana de Ciencias Geológicas, vol. 19, núm. 3, 2002, pp. 242-251 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57219311 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative 242 RevistaField etMexicana al. de Ciencias Geológica, v. 19, núm. 3, 2002, p. 242-251 The early Middle Miocene paleoenvironmental setting of New Zealand Brad D. Field1*, Martin P. Crundwell1, James P. Kennett2, Peter R. King1, Craig M. Jones1, and George H. Scott1 1 Institute of Geological and Nuclear Sciences, Box 30368, Lower Hutt, New Zealand 2 Department of Geological Sciences, University of California Santa Barbara, USA * e-mail: [email protected] ABSTRACT New Zealand has a middle Miocene (~16.4-11.2 Ma) sedimentary record that extends from terrestrial through to distal oceanic paleoenvironmental settings available for study in outcrop, petroleum exploration wells and deep sea drillholes. We use this data to establish a new model for the region at the beginning of middle Miocene times on a palinspastic base map, as a starting point for the study of later middle Miocene global cooling and its effects.