Cooper Basin Acreage Release CO2012-A

Total Page:16

File Type:pdf, Size:1020Kb

Cooper Basin Acreage Release CO2012-A Cooper Basin CO2012-A South Australia Acreage Release Bids close APRIL 4 2 0 1 3 Department for Manufacturing, www.petroleum.dmitre.sa.gov.au Energy Resources Division Innovation, Trade, Resources and Energy August 2012 204315 CONTENTS THE OFFER . 3 PRODUCTS AND DATA . 3 INTRODUCTION . 3 PETROLEUM GEOLOGY . 7 Cooper Basin . 7 Eromanga Basin . 7 Lake Eyre . 7 SOURCE ROCKS . 9 Cooper Basin . 9 Eromanga Basin . 9 RESERVOIRS AND SEALS . 10 TRAPS . 10 Warburton Basin . 10 Cooper Basin . 10 Eromanga Basin . 11 EXPLORATION POTENTIAL . 11 Block CO2012-A . 11 Birkhead Channel Play — Eromanga Basin . 11 Conventional four-way dip closures — Cooper Basin . 12 Merrimelia Formation shale play — Cooper Basin . 12 INFRASTRUCTURE AND TRANSPORT . 12 LAND ACCESS . 13 National parks and reserves . 13 Environmental regulation . 13 Heritage and land access . 13 Geothermal Exploration Licences . 16 Associated Activities Licences . 16 CLIMATE AND LAND USE . 16 BIDDING AND AWARD PROCESS . 18 CONTACT INFORMATION . 18 REFERENCES . 18 Cooper Basin CO2012-A 2 South Australia COOPER BASIN Acreage Release Block CO2012-A BIDS CLOSE 4.00 pm Australian Central Standard Time, Thursday 4th April 2013 THE OFFER f PEPS database with production, well, seismic A new petroleum exploration licence (PEL) and engineering data (also downloadable in the Cooper and Eromanga Basins is being from the DMITRE Petroleum website) offered by the South Australian Government f company prospectivity reports (also on the basis of work program bidding (Fig. 1). downloadable from the DMITRE Petroleum Block CO2012-A comprises two areas totalling website via SARIG) 391.8 sq km relinquished from PEL 111 on the SARIG (South Australia Resources Information western margin of the Patchawarra Trough. One Geoserver) can be accessed by selecting SARIG well (Darter 1) has been drilled and 581 line on the DMITRE Petroleum website <www. kilometres of 2D seismic data have been acquired petroleum.dmitre.sa.gov.au>. SARIG provides within the block (Fig. 2). an interactive map window to view, query and download data. The map window is useful for PRODUCTS AND DATA viewing wells, seismic lines, tenements, land A comprehensive summary of the Cooper and access etc over the various Cooper Basin depth, Eromanga basins is available in The Petroleum time and isopach images. Geology of South Australia volumes 2 (Eromanga More information on products and data can be Basin) and 4 (Cooper Basin). These volumes accessed by selecting ‘Products and Data’ on the include chapters on structural and tectonic DMITRE Petroleum website home page. history, litho- and biostratigraphy, source rocks and maturity, reservoirs, seals, trap development, INTRODUCTION discovered reserves, field reviews, undiscovered The Cooper Basin is a Permo-Carboniferous potential, and exploration history. The to Triassic intracratonic basin located 800 km publications can be downloaded via the DMITRE north of Adelaide, extending into southwest Petroleum website, and are also available for Queensland (Gravestock et al., 1998). It is free on the Petroleum and Geothermal in South overlain by the prospective Jurassic to Cretaceous Australia DVD. intracratonic Eromanga Basin which extends Previous exploration data and reports are readily of much of central-eastern Australia (Cotton available from DMITRE in digital format on et al., 2006). The Cooper and Eromanga portable hard drives, including: basins collectively contain up to 3700 m of f well completion reports (also downloadable predominantly fluvial, glaciofluvial, lacustrine from the DMITRE Petroleum website via and deltaic sediment with some Cretaceous SARIG) marine sediments (Fig. 3). Targets are 1200– 3700 m deep. The Cooper and Eromanga basins f GIS datasets including wells, seismic, lie unconformably over early Palaeozoic marine tenements, pipelines sediments of the Warburton Basin and Mid- f seismic survey shot point location data Carboniferous Big Lake Suite granite, which f seismic survey reports and archive stack data is currently being evaluated as a source of (SEGY format) geothermal energy (e.g. Wyborn, et al., 2004; f digital well logs (DLIS/LIS format) Wyborn, 2008). f velocity survey check shot information The Cooper Basin and overlying Eromanga f structure maps and datasets Basin is Australia’s largest and most mature Cooper Basin CO2012-A 3 Cooper and Eromanga Basins, South Australia PETROLEUM LICENCES QUEENSLAND ") Darwin 568 NORTHERN TERRITORY 569 QUEENSLAND WESTERN 87 AUSTRALIA 88 ") Brisbane SOUTH AUSTRALIA NEW SOUTH WALES Perth ") Adelaide ") ") Sydney VIC ACT 1000 km ") 570 Melbourne TAS ") Hobart 424 110 444 290 PL20 ! 90 514 90 100 ! 102 101 !! ! 570 514 182 102 Petroleum tenements !!! CO2012-A 101 ! 101 101! !! Acreage release block 111 ! 101 ! ! 101 ! CO2012-A 570 103 Exploration licence (PEL) 331 ! 102 105 ! ! 514 Exploration licence application (PELA) 512 ! 104 513 91 105 Production licence (PPL) 104 105 PL18 ! Innamincka PL5 Production licence application (PPLA) ! ! )" ! ! ! ! ! 218 Retention licence (PRL) ! ! ! ! ! ! Retention licence application (PRLA) ! ! 106 ! 92 ! !! ! ! ! ! ! ! 513 ! ! 516 115 Petroleum pipelines ! Moomba )" 115 Pipeline licence (PL) – gas ! ! PL17 71 107 ! ! 512 ! 513 516 Pipeline licence (PL) – gas and liquids PL15 Pipeline licence (PL) – liquids 115 115! 516 PL9 516 !! ! Discoveries 2002 – 2012 112 516 114 ! ! !! ! !!! ! ! Oil ! 516 ! !! 115 93 ! ! !! !! ! ! ! !! ! ! ! ! ! 113 ! !115 115 Gas ! 115 515 ! 516 ! 516 !! 115 !! !! 516 516 PLs Cooper Basin subcrop limit 7,8 ! Coongie Lakes control zone – 95 no access 94 515 560 0 25 50 Kilometres Datum GDA 94 - Projection MGA Zone 54 96 575 PL2 PL1 WALES SOUTH NEW 607 146 133 REG 204315-003 Figure 1 Petroleum licences Cooper Basin CO2012-A 4 139°30'E 139°45'E 140°0'E 340000 360000 380000 400000 27°0'S 27°0'S PEL 444 PEL 424 . 7000000 7000000 . 27°15'S 27°15'S CO2012-A 6980000 6980000 PEL 182 PELA 512 . PEL 111 . CO2012-A . Darter 1 6960000 PEL 105 6960000 27°30'S . 27°30'S Hoolendinnie 1 . PEL 514 Darter 1 . PEL 104 . PELA 513 . PEL 91 . PEL 104 . 6940000 6940000 . 27°45'S . PELA 513 . 27°45'S . PEL 106 . 6920000 6920000 . PEL 92 . 340000 360000 380000 400000 REG 204315-008 139°15'E 139°30'E 139°45'E 140°0'E Petroleum tenements Petroleum pipelines Parks with petroleum exploration access Acreage release block Production licence (PPL) Gas Gas and liquids Parks with no petroleum Exploration licence (PEL) Production licence exploration access application (PPLA) Liquids Exploration licence Liquid trunkline Ramsar site application (PELA) Retention licence (PRL) 0 5 10 15 km Gas trunkline GDA 94 – MGA Zone 54 Seismic coverage Petroleum wells . 2 dimension Cooper and Eromanga basins, Dry hole Gas well with oil shows . 3 dimension South Australia Dry hole with oil shows Oil and gas well . Gas shows Oil well Cooper Basin Permian edge ACREAGE RELEASE . Proposed or currently drilling Gas well Top Nappamerri subcrop edge CO2012-A Figure 2 CO2012 acreage release Cooper Basin CO2012-A 5 onshore hydrocarbon province, AGE supplying major south-eastern DEPOSITIONAL ZONE ROCK UNIT Australian gas markets since SERIES STAGE ENVIRONMENT SYSTEM LITHOLOGY 1969 and producing oil since PALYNOLOGICAL 1982. The Cooper Basin Liquids LAKE EYRE BASIN ZOIC Project (1980–84) was initiated CENO- to market the oil and existing gas liquids. A liquids pipeline links Moomba to a processing plant Late Winton Formation Non-marine to and storage and export loading marginal marine Mackunda Formation Marginal marine Oodnadatta Allaru Mudstone Marine facilities at Port Bonython. Formation Restricted marine - stratified and anoxic Toolebuc Fm Regressive marine Coorikiana shoreface Over 2000 exploration and Sandstone WALLUMBILLA Open marine Early Bulldog Shale FORMATION transgressive development wells have been CRETACEOUS Wyandra Sandstone Non-margin to drilled and over 75 829 km Mbr marginal marine Cadna-owie Formation 2 Murta Formation Lacustrine turbidites, 2D and 8882 km 3D seismic deltas. Shoreface facies McKinlay Mbr Braided-meandering recorded. Estimated total Namur Westbourne Fm fluvial Sandstone Adori Sandstone EROMANGA BASIN cumulative product sales to Late Birkhead Fluvio-lacustrine Formation backswamp end June 2012 are: 5.05 tcf Braided fluvial with Sandstone Algebuckina Hutton aeolian influence of sales gas, 77 mmboe of Middle Sandstone condensate, 158.0 mmbbl of oil Poolowanna Meandering- JURASSIC anastomosing fluvial and 78.2 mmboe of LPG. Annual Formation petroleum production and the Early value of sales since 1970 are Norian to PT5 Cuddapan Formation Floodplain. Rhaetian Meandering fluvial Late shown in Figure 4. Oil production Carnian PT4 was declining until 2002 when Sinuous meandering Ladinian PT3 Tinchoo Fm streams. Fluvio-lacust. Middle 100 m new discoveries caused a Anisian Wimma100 m Braided fluvial channel belt and floodplain resurgence of drilling activity and Sandstone PT2 Mbr Paning Arrabury exploration success, while gas TRIASSIC Mbr Early Scythian 150 m Formation sales peaked in 1989 and have Floodplain, lacustrine, PT1 Callamurra palaeosols, Member moderate/sinuosity been declining since 1998. GROUP NAPPAMERRI fluvial channels. PP6 125 m Tatarian Meandering fluvial, Toolachee Formation deltaic in part Exploration drilling has produced PP5 160 m Late Kazanian Daralingie unconformity a steady stream of discoveries Daralingie Ufimian Formation Fluvio-deltaic since the discovery of gas in PP4 Lacustrine 1963 as indicated by the world Kungurian Roseneath Shale Fluvio-deltaic, local class exploration success
Recommended publications
  • Unconventional Gas Production
    Engineering Energy: Unconventional Gas Production A study of shale gas in Australia. FINAL REPORT PROJECT AUSTRALIAN ACADEMY OF THE HUMANITIES AUSTRALIAN ACADEMY OF SCIENCE ACADEMY OF THE SOCIAL SCIENCES IN AUSTRALIA AUSTRALIAN ACADEMY OF TECHNOLOGICAL SCIENCES AND ENGINEERING SECURING EXPERT AUSTRALIA’S WORKING FUTURE GROUP – PROJECT 6 A three-year research Professor Peter Cook CBE, FTSE (Chair) program funded by the Dr Vaughan Beck FTSE (Deputy Chair) Australian Research Professor David Brereton Council and conducted Professor Robert Clark AO, FAA, FRSN Dr Brian Fisher AO, PSM, FASSA by the four Learned Professor Sandra Kentish Academies through Mr John Toomey FTSE the Australian Council Dr John Williams FTSE of Learned Academies for PMSEIC, through AUTHORS the Office of the Chief Professor Peter Cook CBE, FTSE Scientist. Securing Dr Vaughan Beck FTSE Australia’s Future delivers Professor David Brereton research-based evidence Professor Robert Clark AO, FAA, FRSN and findings to support Dr Brian Fisher AO, PSM, FASSA policy development in Professor Sandra Kentish areas of importance to Mr John Toomey FTSE Australia’s future. Dr John Williams FTSE © Australian Council of Learned Academies (ACOLA) ISBN 978 0 9875798 1 2 This work is copyright. Apart from any use permitted under the Copyright Act 1968, no part of it may be reproduced by any process without written permission from the publisher. Requests and inquiries concerning reproduction rights should be directed to the publisher. DATE OF PUBLICATION May 2013 PUBLISHER Australian Council of Learned Academies Level 1, 1 Bowen Crescent Melbourne Victoria 3004 Australia Telephone: +61 (0)3 98640923 www.acola.org.au SUGGESTED CITATION Cook, P, Beck, V, Brereton, D, Clark, R, Fisher, B, Kentish, S, Toomey, J and Williams, J (2013).
    [Show full text]
  • 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]
  • Systematics and Biostratigraphy of Australian Early Cretaceous
    This file is part of the following reference: Williamson, Toni (2006) Systematics and biostratigraphy of Australian early cretaceous belemnites with contributions to the timescale and palaeoenvironmental assessment of the early Australian early cretaceous system derived from stable isotope proxies. PhD thesis, James Cook University. Access to this file is available from: http://eprints.jcu.edu.au/4906 " SECTION!A! ! ! ! ! ! ! Albian"and"Cenomanian"belemnites"of"the"Family"Dimitobelidae" from"Australia" Section!A.!!Albian!and!Cenomanian!Dimitobelidae!from!Australia! Section!A.! Albian!and!Cenomanian!belemnites!of!the!Family!Dimitobelidae! from!Australia" " A.!1!Abstract! Representatives" of" the" Family" Dimitobelidae" (Mollusca:Cephalopoda)! are" abundantly" represented"in"Australian"Early"Cretaceous"shallow"marine"strata,"especially"those"related"to" the"epeiric"sedimentary"record"of"the"Great"Artesian"Basin.""The"taxonomy,"biostratigraphy"and" distribution" of" Albian" and" Cenomanian" Australian" representatives" of" the" family" are" revised," utilising" all" known" collections." " The" genus" Dimitobelus" Whitehouse" (early" Albian" !" mid" Cenomanian)"occurs"in"both"the"Great"Artesian"Basin"of"eastern"Australia"and"the"Carnarvon" Basin" of" Western" Australia." This" genus" embraces" six" named" species:" " D.! diptychus" (McCoy)" (earliest"Albian"!"mid"Cenomanian),"D.!stimulus" Whitehouse"(Albian),"D.!dayi" Doyle"(earliest" Albian" –" early" late" Albian)," D.! liversidgei" Etheridge" (late" Albian)," D.! plautus" sp." nov" (early"
    [Show full text]
  • From the Lower Cretaceous of Lightning Ridge, New South Wales, Australia
    Isolated teeth of Anhangueria (Pterosauria: Pterodactyloidea) from the Lower Cretaceous of Lightning Ridge, New South Wales, Australia Tom Brougham1, Elizabeth T. Smith2 and Phil R. Bell1 1 School of Environmental and Rural Science, University of New England, Armidale, New South Wales, Australia 2 Australian Opal Centre, Lightning Ridge, New South Wales, Australia ABSTRACT The fossil record of Australian pterosaurs is sparse, consisting of only a small number of isolated and fragmentary remains from the Cretaceous of Queensland, Western Australia and Victoria. Here, we describe two isolated pterosaur teeth from the Lower Cretaceous (middle Albian) Griman Creek Formation at Lightning Ridge (New South Wales) and identify them as indeterminate members of the pterodactyloid clade Anhangueria. This represents the first formal description of pterosaur material from New South Wales. The presence of one or more anhanguerian pterosaurs at Lightning Ridge correlates with the presence of `ornithocheirid' and Anhanguera-like pterosaurs from the contemporaneous Toolebuc Formation of central Queensland and the global distribution attained by ornithocheiroids during the Early Cretaceous. The morphology of the teeth and their presence in the estuarine- and lacustrine-influenced Griman Creek Formation is likely indicative of similar life habits of the tooth bearer to other members of Anhangueria. Subjects Paleontology, Taxonomy Keywords Pterosauria, Cretaceous, Australia, Teeth Submitted 11 January 2017 Accepted 31 March 2017 Published 3 May 2017 INTRODUCTION Corresponding author Tom Brougham, Pterosaurs first appeared in the Late Triassic and diversified rapidly into the Jurassic. [email protected] At the peak of their diversity in the Cretaceous, pterosaurs where present on all Academic editor Andrew Farke continents, including Antarctica (Barrett et al., 2008; Upchurch et al., 2015).
    [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]
  • Detrital Zircon Age Constraints for the Winton Formation, Queensland: Contextualizing Australia's Late Cretaceous Dinosaur Faunas
    GR-00968; No of Pages 13 Gondwana Research xxx (2013) xxx–xxx Contents lists available at SciVerse ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr Detrital zircon age constraints for the Winton Formation, Queensland: Contextualizing Australia's Late Cretaceous dinosaur faunas Ryan T. Tucker a,⁎, Eric M. Roberts a,YiHub,1, Anthony I.S. Kemp a,b,c,2, Steven W. Salisbury d a School of Earth and Environmental Sciences, James Cook University, DB34 Discovery Drive, Townsville, Qld 4811, Australia b Advanced Analytical Centre, James Cook University, Townsville, Australia c School of Earth and Environment, University of Western Australia, Crawley, Australia d School of Biological Sciences, The University of Queensland, Brisbane, Qld 4072, Australia article info abstract Article history: The Winton Formation provides an important snapshot of Australia's late Mesozoic terrestrial biota, boasting Received 16 August 2012 a vertebrate fauna that includes dinosaurs, crocodyliforms, aquatic squamates, turtles, lungfish and teleost Received in revised form 14 November 2012 fishes, and a flora that has previously been considered to include some of the world's earliest known Accepted 3 December 2012 flowering plants. Despite its significance, poor age control has thus far prevented precise regional and global Available online xxxx correlations, limiting the depth of paleobiogeographic assessments. The goal of this study was to use U–Pb fi Handling Editor: A.S. Collins isotope dating of detrital zircons by laser ablation to re ne the depositional age range of selected horizons within the Winton Formation. We applied this technique, with refined instrumental tuning protocols, to Keywords: systematically investigate detrital zircon grain ages for five samples from different stratigraphic levels and Winton Formation vertebrate-bearing fossil locations throughout the Winton Formation.
    [Show full text]
  • Technical Appendix for the Geological and Bioregional Assessment: Stage 2
    Hydrogeology of the Cooper GBA region Technical appendix for the Geological and Bioregional Assessment: Stage 2 2020 A scientific collaboration between the Department of Agriculture, Water and the Environment, Bureau of Meteorology, CSIRO and Geoscience Australia The Geological and Bioregional Assessment Program The Geological and Bioregional Assessment Program will provide independent scientific advice on the potential impacts from development of selected unconventional hydrocarbon plays on water and the environment. The geological and environmental data and tools produced by the Program will assist governments, industry, landowners and the community to help inform decision making and enhance the coordinated management of potential impacts. The Program is funded by the Australian Government Department of the Environment and Energy. The Department of the Environment and Energy, Bureau of Meteorology, CSIRO and Geoscience Australia are collaborating to undertake geological and bioregional assessments. For more information, visit http://www.bioregionalassessments.gov.au. Department of the Environment and Energy The Department designs and implements Australian Government policy and programs to protect and conserve the environment, water and heritage, promote climate action, and provide adequate, reliable and affordable energy. For more information visit http://www.environment.gov.au. Bureau of Meteorology The Bureau of Meteorology is Australia’s national weather, climate and water agency. Under the Water Act 2007, the Bureau is responsible for compiling and disseminating Australia's water information. The Bureau is committed to increasing access to water information to support informed decision making about the management of water resources. For more information, visit http://www.bom.gov.au/water/. CSIRO Australia is founding its future on science and innovation.
    [Show full text]
  • Early and “Middle” Cretaceous Iguanodonts in Time and Space
    ISSN (print): 1698-6180. ISSN (online): 1886-7995 www.ucm.es/info/estratig/journal.htm Journal of Iberian Geology 36 (2) 2010: 145-164 doi:10.5209/rev_JIGE.2010.v36.n2.3 Early and “Middle” Cretaceous Iguanodonts in Time and Space Iguanodontes del Cretácico temprano y “medio” en el tiempo y en el espacio K. Carpenter1*, Y. Ishida,2 1USU-CEU Prehistoric Museum, 155 East Main Street, Price, UT 84501, USA 2Department of Natural History Sciences, Hokkaido University, Sapporo 06-0810, Japan *[email protected] Received: 28/11/09 / Accepted: 30/06/10 Abstract Recent discoveries of diverse iguanodonts throughout the Cedar Mountain Formation (Utah, USA) have led us to assess the global diversity of Early Cretaceous iguanodonts. The record in England is more diverse than previously recognized due to Iguanodon being a wastebasket genus throughout the Twentieth Century. Several new taxa, previously recognized as generically distinct by Harry Grovier Seeley, are named. The spatial and temporal distributions of iguanodonts are plotted on global maps as a key to un- derstanding the origin of the Cedar Mountain Formation iguanodonts. Keywords: Early Cretaceous, Iguanodonts, Dinosauria Resumen Los recientes descubrimientos de diversos iguanodontes en la Formación Cedar Mountain (Utah, EE.UU.) nos han llevado a valo- rar la diversidad global de los iguanodontes del Cretácico temprano. El registro en Inglaterra es más diverso de lo que previamente se ha reconocido, debido a que Iguanodon ha sido tratado como un género “cajón de sastre” a lo largo de todo el siglo XX. Varios de los nuevos taxones, previamente reconocidos como genéricamente distintos por Harry Seeley Grovier, se denominan.
    [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]
  • Wq31phone: (07) 3834 3089
    TECHNICAL NOTES WESTERN QUEENSLAND BEST PRACTICE GUIDELINES Road System & Engineering GEOLOGY AND GEOMORPHOLOGY OF WESTERN QUEENSLAND Contact: Lex Vanderstaay Phone: (07) 4931 1657 / Ian Reeves WQ31Phone: (07) 3834 3089 1 Introduction 2 Structure of Technical Note This technical note is one of a series on notes Geological structure - the broad structural elements regarding road construction issues in the three of Western Queensland. western MR Districts of Queensland. Stratigraphy - the geological sequence of the Details of all the notes in the WQ series can be found various rock strata in order from the oldest to in the Preface to the WQ Technical Notes. This note youngest. Only those units which outcrop are and its companion notes on soils and climate are discussed, although a unit which outcrops in one area more in the nature of background documents, may be covered by a younger unit in another area. compared to some of the other notes which are more specific to the physical process of road design and Geological history post-Jurassic - this section construction. provides a more detailed history of the younger, post Jurassic age rocks which cover most of the area. The current note discusses two fundamental aspects of the form of Western Queensland. The geology Geomorphology - this section covers the typical considers the surface rocks of the area, while the land forms which occur in the area and describes geomorphology considers the current surface terrain these land forms in terms of both mode of formation features. and underlying geology. Due to the critical nature of the soils, a separate Materials - this section covers the interrelation of technical note, WQ32, has been prepared on this geology and land forms as sources of various classes subject.
    [Show full text]
  • Stratigraphy, Sedimentation and Age of The
    ResearchOnline@JCU This file is part of the following reference: Tucker, Ryan Thomas (2014) Stratigraphy, sedimentation and age of the upper cretaceous Winton formation, central-western Queensland, Australia: implications for regional palaeogeography, palaeoenvironments and Gondwanan palaeontology. PhD thesis, James Cook University. Access to this file is available from: http://researchonline.jcu.edu.au/34439/ The author has certified to JCU that they have made a reasonable effort to gain permission and acknowledge the owner of any third party copyright material included in this document. If you believe that this is not the case, please contact [email protected] and quote http://researchonline.jcu.edu.au/34439/ Stratigraphy, Sedimentation and Age of the Upper Cretaceous Winton Formation, central-western Queensland, Australia: Implications for regional palaeogeography, palaeoenvironments and Gondwanan palaeontology Thesis Submitted by Ryan Thomas Tucker March 2014 For the degree of: Doctorate of Philosophy In the: SCHOOL OF EARTH AND ENVIRONMENTAL SCIENCES FALCULTY OF SCIENCE AND ENGINEERING JAMES COOK UNIVERSITY Statement of Access I, the undersigned author of this thesis, understand that James Cook University will make this thesis available for use within the university library and allow access in other approved libraries after its submission. All users consulting this thesis will have to sign the following statement: In consulting this thesis I agree not to copy or closely paraphrase it in whole or in part without the written consent of the author; and to make proper public written acknowledgement for any assistance which I have obtained from it. Beyond this, I do not wish to place any restrictions on access to this thesis.
    [Show full text]
  • A New Species from the Lower Cretaceous of Queensland, Australia
    The first record of the ichthyodectiform fish Cladocyclus from eastern Gondwana: A new species from the Lower Cretaceous of Queensland, Australia RODNEY W. BERRELL, JESÚS ALVARADO-ORTEGA, YOSHITAKA YABUMOTO, and STEVEN W. SALISBURY Berrell, R.W., Alvarado-Ortega, J., Yabumoto, Y., and Salisbury, S.W. 2014. The first record of the ichthyodectiform fish Cladocyclus from eastern Gondwana: A new species from the Lower Cretaceous of Queensland, Australia. Acta Palaeontologica Polonica 59 (4): 903–920. Cladocyclus is a genus of ichthyodectiform fish that is best known from fossils found in shallow marine Cretaceous deposits in Brazil and Morocco. Herein, a new species of Cladocyclus is described on the basis of a fossil that comprises an articulated skull and anterior part of the body, preserved as part and counter-part in what was originally a single eroded nodule of fluvially-deposited volcanolithic sandstone from the Lower Cretaceous (upper Albian) portion of the Winton Formation near Isisford, central-western Queensland, Australia. This specimen represents the first record of Cladocyclus in eastern Gondwana, and indicates that species of this fish may also have inhabited freshwater environments. The new species is assigned to the genus Cladocyclus based on the morphology of the cleithrum (the arms are oriented at approx- imately 90° to each other) and a mandibular articular facet that incorporates portions of the angular, the articular and the retroarticular. Cladocyclus geddesi sp. nov. can be distinguished from other congeners based on the possession of a more elongate horizontal arm of the cleithrum and a supraoccipital crest that is gently convex posteriorly. This discovery greatly expands the geographic range of Cladocyclus, and supports the idea of a distinct southern fish fauna in the seas surrounding the fragmenting Gondwanan landmasses during the mid-Cretaceous.
    [Show full text]