Seal Quality and Distribution in the Southern Taranaki Basin Late Cretaceous to Eocene Section and Implications for Hydrocarbon Trapping

Total Page:16

File Type:pdf, Size:1020Kb

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 ...................................................................................................... 9 2.1 Structural Overview ................................................................................................................ 9 2.2 Cretaceous Early Basin Development 103-82 Ma ................................................................. 10 2.3 Late Cretaceous - Paleocene; Syn Rift 82–56 Ma ................................................................. 11 2.4 Paleocene – Early Oligocene; Passive Margin 56-34 Ma ...................................................... 11 2.5 Oligocene – Early Miocene; Transitional Phase 34-19 Ma .................................................... 15 2.6 Miocene - Present; Convergence 19-0 Ma ........................................................................... 15 2.7 North Cape Formation .......................................................................................................... 16 2.8 Farewell Formation ............................................................................................................... 16 2.9 North Cape and E Shales ....................................................................................................... 19 2.10 Biostratigraphic Ages of North Cape and E Shale ................................................................. 19 2.11 Transgressive Depositional Model ........................................................................................ 21 3. Seal Rocks ...................................................................................................................................... 24 3.1 Introduction .......................................................................................................................... 24 3.2 Previous Research on the Influences on Seal Quality ........................................................... 25 3.2.1 Mercury Injection Capillary Testing and Capillary Pressure ......................................... 27 3.2.2 Clay Minerals and Their Effect on Seal Rocks ............................................................... 29 3.3 North Cape Shale Properties ................................................................................................. 31 3.4 E Shale Properties ................................................................................................................. 34 3.5 Results and Discussion .......................................................................................................... 36 4. Seal Quality Estimates from Petroleum Wells .............................................................................. 39 4.1 Introduction .......................................................................................................................... 39 4.2 Relevant Wells for Study ....................................................................................................... 39 4.3 Log Acquisition ...................................................................................................................... 40 4.4 Overview of Log Types .......................................................................................................... 42 4.5 Well Correlation Panel .......................................................................................................... 43 I 4.6 Volume of Clay (Vcl) .............................................................................................................. 46 4.7 Neutron / Density Cross-plots ............................................................................................... 47 4.8 Discussion and Conclusions .................................................................................................. 48 5. Seismic Reflection Interpretation ................................................................................................. 51 5.1 Introduction .......................................................................................................................... 51 5.2 Geological to Seismic Modelling ........................................................................................... 51 5.3 Data Utilised .......................................................................................................................... 51 5.4 Seismic to Well Ties............................................................................................................... 52 5.5 Seismic Interpretation Workflow .......................................................................................... 56 5.6 Interpreted Horizons ............................................................................................................. 59 5.6.1 T40 (base Oligocene) ..................................................................................................... 60 5.6.2 T15 top E Shale equivalent (early Eocene, Waipawan Stage) ....................................... 62 5.6.3 T11 top Farewell Formation (Paleocene, Teurian Stage) .............................................. 62 5.6.4 K95 top North Cape Shale (Latest Cretaceous, Latest Haumurian Stage) .................... 62 5.6.5 K91 near top North Cape Formation (Late Cretaceous, Latest Haumurian Stage) ....... 62 5.6.6 Basement ...................................................................................................................... 62 5.7 E Shale Interpretation (T15 – T11) ........................................................................................ 63 5.7.1 Discussion by Sub Regions ............................................................................................ 65 5.8 North Cape Shale Interpretation (K95 – K91) ....................................................................... 65 5.8.1 Discussion by Sub-Regions ............................................................................................ 66 5.9 Amplitude and Variance Seismic Extractions ........................................................................ 69 5.10 Faulting.................................................................................................................................. 71 6. Paleogeography ............................................................................................................................ 72 6.1 Introduction .......................................................................................................................... 72 6.2 Inputs from Previous Chapters ............................................................................................. 72 6.3 Paleoenvironments from Biostratigraphy............................................................................. 72 6.4 Modern Analogues for Interpretation of Paleoenvironments .............................................. 73 6.5 Results and Discussion .......................................................................................................... 76 6.5.1 E Shale Maximum Flooding Surface, Waipawan, 55 Ma .............................................. 76 6.5.2 North Cape Shale Max Flooding Surface, Latest Haumuraian (66 Ma) ........................ 79 6.6 Summary and Conclusions .................................................................................................... 82 7. Summary and Conclusions ............................................................................................................ 83 7.1 Project Outcomes ................................................................................................................. 83 7.2 Conclusions ........................................................................................................................... 83 7.3 Implications for Future Exploration in the Southern Taranaki Basin .................................... 84 7.4 Future Work .......................................................................................................................... 86 II References ...........................................................................................................................................
Recommended publications
  • 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
    [Show full text]
  • 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).
    [Show full text]
  • Vulnerable Marine Ecosystems – Processes and Practices in the High Seas Vulnerable Marine Ecosystems Processes and Practices in the High Seas
    ISSN 2070-7010 FAO 595 FISHERIES AND AQUACULTURE TECHNICAL PAPER 595 Vulnerable marine ecosystems – Processes and practices in the high seas Vulnerable marine ecosystems Processes and practices in the high seas This publication, Vulnerable Marine Ecosystems: processes and practices in the high seas, provides regional fisheries management bodies, States, and other interested parties with a summary of existing regional measures to protect vulnerable marine ecosystems from significant adverse impacts caused by deep-sea fisheries using bottom contact gears in the high seas. This publication compiles and summarizes information on the processes and practices of the regional fishery management bodies, with mandates to manage deep-sea fisheries in the high seas, to protect vulnerable marine ecosystems. ISBN 978-92-5-109340-5 ISSN 2070-7010 FAO 9 789251 093405 I5952E/2/03.17 Cover photo credits: Photo descriptions clockwise from top-left: Acanthagorgia spp., Paragorgia arborea, Vase sponges (images courtesy of Fisheries and Oceans, Canada); and Callogorgia spp. (image courtesy of Kirsty Kemp, the Zoological Society of London). FAO FISHERIES AND Vulnerable marine ecosystems AQUACULTURE TECHNICAL Processes and practices in the high seas PAPER 595 Edited by Anthony Thompson FAO Consultant Rome, Italy Jessica Sanders Fisheries Officer FAO Fisheries and Aquaculture Department Rome, Italy Merete Tandstad Fisheries Resources Officer FAO Fisheries and Aquaculture Department Rome, Italy Fabio Carocci Fishery Information Assistant FAO Fisheries and Aquaculture Department Rome, Italy and Jessica Fuller FAO Consultant Rome, Italy FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2016 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • The Age and Origin of Miocene-Pliocene Fault Reactivations in the Upper Plate of an Incipient Subduction Zone, Puysegur Margin
    RESEARCH ARTICLE The Age and Origin of Miocene‐Pliocene Fault 10.1029/2019TC005674 Reactivations in the Upper Plate of an Key Points: • Structural analyses and 40Ar/39Ar Incipient Subduction Zone, Puysegur geochronology reveal multiple fault reactivations accompanying Margin, New Zealand subduction initiation at the K. A. Klepeis1 , L. E. Webb1 , H. J. Blatchford1,2 , R. Jongens3 , R. E. Turnbull4 , and Puysegur Margin 5 • The data show how fault motions J. J. Schwartz are linked to events occurring at the 1 2 Puysegur Trench and deep within Department of Geology, University of Vermont, Burlington, VT, USA, Now at Department of Earth Sciences, University continental lithosphere of Minnesota, Minneapolis, MN, USA, 3Anatoki Geoscience Ltd, Dunedin, New Zealand, 4Dunedin Research Centre, GNS • Two episodes of Late Science, Dunedin, New Zealand, 5Department of Geological Sciences, California State University, Northridge, Northridge, Miocene‐Pliocene reverse faulting CA, USA resulted in short pulses of accelerated rock uplift and topographic growth Abstract Structural observations and 40Ar/39Ar geochronology on pseudotachylyte, mylonite, and other Supporting Information: fault zone materials from Fiordland, New Zealand, reveal a multistage history of fault reactivation and • Supporting information S1 uplift above an incipient ocean‐continent subduction zone. The integrated data allow us to distinguish • Table S1 true fault reactivations from cases where different styles of brittle and ductile deformation happen • Figure S1 • Table S2 together. Five stages of faulting record the initiation and evolution of subduction at the Puysegur Trench. Stage 1 normal faults (40–25 Ma) formed during continental rifting prior to subduction. These faults were reactivated as dextral strike‐slip shear zones when subduction began at ~25 Ma.
    [Show full text]
  • 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.
    [Show full text]
  • The Gondwana Margin: Proterozoic to Mesozoic
    CORE Metadata, citation and similar papers at core.ac.uk Provided by EPrints Complutense The Gondwana margin: Proterozoic to Mesozoic The longevity and extent of the oceanic southern of '--'H��'.JAJ.J.'u., E. I.M. Gonzalez-Casado and I.A. Dahlquist Gondwana have made it the of intense study for more on "The Maz terrane: a Mesoproterozoic domain in the western than 70 years. It was one of the cradles of terrane and Sierras equivalent to the remains a proving ground for theories of Antofalla block of southern Peru? for West LL.L�""".LE, """'.LJL.LU''-'H and Investigation on this Gondwana evolution" sheds new light on the Middle margin, such as accretionary orogenesis and terrane analysis, is and Late Proterozoic evolution of the western Amazonia margin vital to our understanding of the Proterozoic and Phanerozoic that preceded final amalgamation of West Gondwana in the Late evolution of the continental crust. In this issue of Cambrian. The Maz terrane Gondwana Research, entitled "The West Gondwana Margin: Sierras Pampeanas) is recognised as a new continental terrane Proterozoic to Mesozoic", we have assembled 9 research papers that underwent Grenvillian-age orogeny and was thoroughly various of the evolution of the West the Ordovician Famatinian orogeny. Nd- and Gondwana margin, frrst at the international .L.Ln-''-'�'J.�F. allows correlation of Maz metasedi­ 'Gondwana 12 (Geological and Biological Heritage of Gond- rnp'nt�n"\T rocks with the Mesoproterozoic northern part of the wana)', held in in November 2005. Many -'-'J.�V.L<-"HU craton, of pre-Andean basement in concern southern South which has a continuous southern Peru.
    [Show full text]
  • 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.
    [Show full text]
  • Paper Is Divided Into Two Parts
    Earth-Science Reviews 140 (2015) 72–107 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Geologic and kinematic constraints on Late Cretaceous to mid Eocene plate boundaries in the southwest Pacific Kara J. Matthews a,⁎, Simon E. Williams a, Joanne M. Whittaker b,R.DietmarMüllera, Maria Seton a, Geoffrey L. Clarke a a EarthByte Group, School of Geosciences, The University of Sydney, NSW 2006, Australia b Institute for Marine and Antarctic Studies, University of Tasmania, TAS 7001, Australia article info abstract Article history: Starkly contrasting tectonic reconstructions have been proposed for the Late Cretaceous to mid Eocene (~85– Received 25 November 2013 45 Ma) evolution of the southwest Pacific, reflecting sparse and ambiguous data. Furthermore, uncertainty in Accepted 30 October 2014 the timing of and motion at plate boundaries in the region has led to controversy around how to implement a Available online 7 November 2014 robust southwest Pacific plate circuit. It is agreed that the southwest Pacific comprised three spreading ridges during this time: in the Southeast Indian Ocean, Tasman Sea and Amundsen Sea. However, one and possibly Keywords: two other plate boundaries also accommodated relative plate motions: in the West Antarctic Rift System Southwest Pacific fi Lord Howe Rise (WARS) and between the Lord Howe Rise (LHR) and Paci c. Relevant geologic and kinematic data from the South Loyalty Basin region are reviewed to better constrain its plate motion history during this period, and determine the time- Late Cretaceous dependent evolution of the southwest Pacific regional plate circuit. A model of (1) west-dipping subduction Subduction and basin opening to the east of the LHR from 85–55 Ma, and (2) initiation of northeast-dipping subduction Plate circuit and basin closure east of New Caledonia at ~55 Ma is supported.
    [Show full text]