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The University of Sydney
THE UNIVERSITY OF SYDNEY Copyright and use of this thesis This thesis must be used in accordance with the provisions of the Copyright Act 1968. Reproduction of material protected by copyright may be an infringement of copyright and copyright owners may be entitled to take legal action against persons who infringe their copyright. Section 51 (2) of the Copyright Act permits an authorized officer of a university library or archives to provide a copy (by communication or otherwise) of an unpublished thesis kept in the library or archives, to a person who satisfies the authorized officer that he or she requires the reproduction for the purposes of research or study. The Copyright Act grants the creator of a work a number of moral rights, specifically the right of attribution, the right against false attribution and the right of integrity. You may infringe the author’s moral rights if you: - fail to acknowledge the author of this thesis if you quote sections from the work - attribute this thesis to another author -subject this thesis to derogatory treatment which may prejudice the author’s reputation For further information contact the University’s Copyright Service. sydney.edu.au/copyright A STRUCTURAL ANALYSIS OF THE SOUTHERN HORNSBY PLATEAU, SYDNEY BASIN, NEW SOUTH WALES by Anthony Richard Norman, B.Sc. (Hons) A thesis submitted in fulfilment of the requirements for the degree of Master of Science DEPARTMENT OF GEOLOGY AND GEOPHYSICS UNIVERSITY OF SYDNEY September, 1986 ABSTRACT The Hornsby Plateau rises north of Sydney. Aerial photo interpretation of an area north of Hornsby and south of the Hawkesbury River revealed two well defined extensive traces. -
Background Paper on New South Wales Geology with a Focus on Basins Containing Coal Seam Gas Resources
Background Paper on New South Wales Geology With a Focus on Basins Containing Coal Seam Gas Resources for Office of the NSW Chief Scientist and Engineer by Colin R. Ward and Bryce F.J. Kelly School of Biological, Earth and Environmental Sciences University of New South Wales Date of Issue: 28 August 2013 Our Reference: J083550 CONTENTS Page 1. AIMS OF THE BACKGROUND PAPER .............................................................. 1 1.1. SIGNIFICANCE OF AUSTRALIAN CSG RESOURCES AND PRODUCTION ................... 1 1.2. DISCLOSURE .................................................................................................... 2 2. GEOLOGY AND EVALUATION OF COAL AND COAL SEAM GAS RESOURCES ............................................................................................................. 3 2.1. NATURE AND ORIGIN OF COAL ........................................................................... 3 2.2. CHEMICAL AND PHYSICAL PROPERTIES OF COAL ................................................ 4 2.3. PETROGRAPHIC PROPERTIES OF COAL ............................................................... 4 2.4. GEOLOGICAL FEATURES OF COAL SEAMS .......................................................... 6 2.5. NATURE AND ORIGIN OF GAS IN COAL SEAMS .................................................... 8 2.6. GAS CONTENT DETERMINATION ........................................................................10 2.7. SORPTION ISOTHERMS AND GAS HOLDING CAPACITY .........................................11 2.8. METHANE SATURATION ....................................................................................12 -
Exceptional Fossil Preservation During CO2 Greenhouse Crises? Gregory J
Palaeogeography, Palaeoclimatology, Palaeoecology 307 (2011) 59–74 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Exceptional fossil preservation during CO2 greenhouse crises? Gregory J. Retallack Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403, USA article info abstract Article history: Exceptional fossil preservation may require not only exceptional places, but exceptional times, as demonstrated Received 27 October 2010 here by two distinct types of analysis. First, irregular stratigraphic spacing of horizons yielding articulated Triassic Received in revised form 19 April 2011 fishes and Cambrian trilobites is highly correlated in sequences in different parts of the world, as if there were Accepted 21 April 2011 short temporal intervals of exceptional preservation globally. Second, compilations of ages of well-dated fossil Available online 30 April 2011 localities show spikes of abundance which coincide with stage boundaries, mass extinctions, oceanic anoxic events, carbon isotope anomalies, spikes of high atmospheric carbon dioxide, and transient warm-wet Keywords: Lagerstatten paleoclimates. Exceptional fossil preservation may have been promoted during unusual times, comparable with fi Fossil preservation the present: CO2 greenhouse crises of expanding marine dead zones, oceanic acidi cation, coral bleaching, Trilobite wetland eutrophication, sea level rise, ice-cap melting, and biotic invasions. Fish © 2011 Elsevier B.V. All rights reserved. Carbon dioxide Greenhouse 1. Introduction Zeigler, 1992), sperm (Nishida et al., 2003), nuclei (Gould, 1971)and starch granules (Baxter, 1964). Taphonomic studies of such fossils have Commercial fossil collectors continue to produce beautifully pre- emphasized special places where fossils are exceptionally preserved pared, fully articulated, complex fossils of scientific(Simmons et al., (Martin, 1999; Bottjer et al., 2002). -
Coal Resource Recovery Plan
Tahmoor Coal Pty Ltd COAL RESOURCE RECOVERY PLAN Tahmoor North Western Domain Longwalls West 1 and West 2 July 2019 simecgfg.com This page has been left blank intentionally. 2 | Tahmoor North Western Domain LW W1-W2 – Coal Resource Recovery Plan TAH-HSEC-243 (July 2019 Ver1) This page has been left blank intentionally. 4 | Tahmoor North Western Domain LW W1-W2 – Coal Resource Recovery Plan TAH-HSEC-243 (July 2019 Ver1) Table of Contents Table of Contents ....................................................................................................................... 5 List of Figures ............................................................................................................................. 7 List of Tables .............................................................................................................................. 7 1 Introduction ........................................................................................................................ 9 Background ............................................................................................................................... 9 Purpose ..................................................................................................................................... 9 Scope ......................................................................................................................................... 9 2 Regulatory Requirements ................................................................................................. -
Strategic Assessment Report, Heathcote Ridge, West Menai
STRATEGIC ASSESSMENT REPORT HEATHCOTE RIDGE, WEST MENAI November 2012 Prepared for Gandangara Local Aboriginal Land Council By Cumberland Ecology with input from BBC Consulting Planners and 1. PURPOSE AND DESCRIPTION .......................................................................... 3 1.1 Introduction ........................................................................................................ 3 1.1.1 Background........................................................................................................... 3 1.2 The Program ..................................................................................................... 4 1.2.1 Background........................................................................................................... 4 1.2.2 Proposed Development Concept ..................................................................... 5 1.3 Regional Context ............................................................................................. 12 1.4 Land Use Planning .......................................................................................... 13 1.4.1 Land to Which the SEPP Amendment will Apply ............................................ 13 1.4.2 Proposed Land Use Zones ................................................................................. 13 1.4.3 Principal Development Standards ................................................................... 14 1.4.4 Consent Authority .............................................................................................. -
Sydenham to Bankstown Environmental Impact Statement
SYDENHAM TO BANKSTOWN ENVIRONMENTAL IMPACT STATEMENT > Technical Paper 9 - Biodiversity assessment report Transport for NSW Sydney Metro City & Southwest Sydenham to Bankstown upgrade Environmental Impact Statement Technical Paper 9 – Biodiversity Assessment Report August 2017 Table of contents 1. Introduction..................................................................................................................................... 1 1.1 Overview .............................................................................................................................. 1 1.2 The project ........................................................................................................................... 2 1.3 Purpose and scope of this report ....................................................................................... 12 1.4 Secretary’s environmental assessment requirements ....................................................... 13 1.5 Legislation and policy......................................................................................................... 14 2. Methodology ................................................................................................................................. 17 2.1 Approach ............................................................................................................................ 17 2.2 Desktop research ............................................................................................................... 17 2.3 Field survey ....................................................................................................................... -
The Geology of NSW
The Geology of NSW The geological characteristics and history of NSW with a focus on coal seam gas (CSG) resources A report commissioned for the NSW Chief Scientist’s Office, May, 2013. Authors: Dr Craig O’Neill1, [email protected] Dr Cara Danis1, [email protected] 1Department of Earth and Planetary Science, Macquarie University, Sydney, NSW, 2109. Contents A brief glossary of terms i 1. Introduction 01 2. Scope 02 3. A brief history of NSW Geology 04 4. Evolution of the SydneyGunnedahBowen Basin System 16 5. Sydney Basin 19 6. Gunnedah Basin 31 7. Bowen Basin 40 8. Surat Basin 51 9. ClarenceMoreton Basin 60 10. Gloucester Basin 70 11. Murray Basin 77 12. Oaklands Basin 84 13. NSW Hydrogeology 92 14. Seismicity and stress in NSW 108 15. Summary and Synthesis 113 ii A brief Glossary of Terms The following constitutes a brief, but by no means comprehensive, compilation of some of the terms used in this review that may not be clear to a non‐geologist reader. Many others are explained within the text. Tectonothermal: The involvement of either (or both) tectonics (the large‐scale movement of the Earth’s crust and lithosphere), and geothermal activity (heating or cooling the crust). Orogenic: pertaining to an orogen, ie. a mountain belt. Associated with a collisional or mountain‐building event. Ma: Mega‐annum, or one million years. Conventionally associated with an age in geochronology (ie. million years before present). Epicratonic: “on the craton”, pertaining to being on a large, stable landmass (eg. -
Bringelly Shale
AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS Lovering, J. F., 1954. The stratigraphy of the Wianamatta Group Triassic System, Sydney Basin. Records of the Australian Museum 23(4): 169–210, plate xii. [25 June 1954]. doi:10.3853/j.0067-1975.23.1954.631 ISSN 0067-1975 Published by the Australian Museum, Sydney naturenature cultureculture discover discover AustralianAustralian Museum Museum science science is is freely freely accessible accessible online online at at www.australianmuseum.net.au/publications/www.australianmuseum.net.au/publications/ 66 CollegeCollege Street,Street, SydneySydney NSWNSW 2010,2010, AustraliaAustralia THE STRATIGRAPHY OF THE WIANAMATTA GROUP TRIASSIC SYSTEM, SYDNEY BASIN BY J. F. LOVERING, M.Sc. Assistant Curator of Minerals and Rocks, The Australian Museum, Sydney. (Plate xii, ten text-figures; eight maps.) Introduction. Methods of Mapping. Stratigraphy. A. General Definition. B. Liverpool Sub-group: (i) Ashfield Shale: (ii) Minchinbury Sandstone: (iii) Bringelly Shale. C. Camden Sub-group : (i) Potts Hill Sandstone; (ii) Annan Shale; (iii) Razorback Sandstone; (iv) Picton Formation; (v) PrndhQe Shale. Sedimentary Petrology and Petrography of the Sandstone 'Formations. The Sedimentary Environment and Sedimentary Tectonics. Post-Depositional Tectonics. SYNOPSIS. The Wianamatta Group has been divided into two Sub-groups-The Liverpool Sub-group (lower. approximately 400 feet thick, predominantly shale lithology) and the Camden Sub-group (upper, approximately 350 feet thick, sandstone lit.hology prominent with shale). The Uverpool Sub-group includes three formations (Ashfield Shale, Minchinbury Sandstone, Bringelly Shale). The Camden Sub-group includes five formations (Potts Hill Sandstone, Annan Shale, Razorback Sandstone, Picton Formation, Prudhoe Shale). The sedimentary petrology of the graywacke-type .sandstones and the relation of the lithology to the sedimentary environment and tectonics is discussed. -
Tectonic Control of Cenozoic Deposition in the Cumberland Basin, Penrith/ Hawkesbury Region, New South Wales
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Research Online University of Wollongong Research Online Faculty of Science, Medicine & Health - Honours Theses University of Wollongong Thesis Collections 2011 Tectonic Control of Cenozoic Deposition in the Cumberland Basin, Penrith/ Hawkesbury Region, New South Wales Lewis Carter University of Wollongong Follow this and additional works at: https://ro.uow.edu.au/thsci University of Wollongong Copyright Warning You may print or download ONE copy of this document for the purpose of your own research or study. The University does not authorise you to copy, communicate or otherwise make available electronically to any other person any copyright material contained on this site. You are reminded of the following: This work is copyright. Apart from any use permitted under the Copyright Act 1968, no part of this work may be reproduced by any process, nor may any other exclusive right be exercised, without the permission of the author. Copyright owners are entitled to take legal action against persons who infringe their copyright. A reproduction of material that is protected by copyright may be a copyright infringement. A court may impose penalties and award damages in relation to offences and infringements relating to copyright material. Higher penalties may apply, and higher damages may be awarded, for offences and infringements involving the conversion of material into digital or electronic form. Unless otherwise indicated, the views expressed in this thesis are those of the author and do not necessarily represent the views of the University of Wollongong. Recommended Citation Carter, Lewis, Tectonic Control of Cenozoic Deposition in the Cumberland Basin, Penrith/Hawkesbury Region, New South Wales, Bachelor of Science (Honours), School of Earth & Environmental Sciences, University of Wollongong, 2011. -
This Article Appeared in a Journal Published by Elsevier
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Palaeogeography, Palaeoclimatology, Palaeoecology 308 (2011) 233–251 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Multiple Early Triassic greenhouse crises impeded recovery from Late Permian mass extinction Gregory J. Retallack a,⁎, Nathan D. Sheldon b, Paul F. Carr c, Mark Fanning d, Caitlyn A. Thompson a, Megan L. Williams c, Brian G. Jones c, Adrian Hutton c a Department of Geological Sciences, University of Oregon, Eugene, OR, USA 97403-1272 b Department of Geological Sciences, University of Michigan, Ann Arbor, MI, USA 48109-1005 c School of Geosciences, University of Wollongong, New South Wale, Australia, 2522 d Research School of Earth Sciences, Australian National University, Canberra, ACT, Australia 0200 article info abstract Article history: The Late Permian mass extinction was not only the most catastrophic known loss of biodiversity, but was Received 11 February 2010 followed by unusually prolonged recovery through the Early Triassic. -
Engineering Performance of Bringelly Shale
CHAPTER 3 SAMPLING AND MINERALOGY OF BRINGELLY SHALE §3.1. INTRODUCTION The objectives of this chapter are to present details of the Bringelly shale from the four sites used in this study. This includes the location of the sites, their lithology and the techniques of sampling from these sites. An examination of the mineralogy and micro-structure of Bringelly shale is also included. These were investigated using a variety of techniques including x-ray diffraction, optical microscopy, and scanning electron microscopy. Laboratory characterisation studies of this shale have been limited to the claystone-siltstone materials which are the predominant lithology in Bringelly shale. Outcomes of the study in this chapter will be linked to the engineering and physical properties of Bringelly shale in the following chapters. §3.2 LOCATION AND ACCESSIBILITY Within the south west of the Sydney Metropolitan area, four separate sites were selected for sampling and field study. A location map including the general geology of the area is shown in Fig.3.1. The sites are active clay shale quarries and major current sources of brick clay and fill material in the Sydney region. A network of 79 Figure 3.1 Geological map showing the location of the study area well-paved roads traverses all localities as shown by the topographic map of the Sydney area shown in Figure 3A.1 in Appendix 3A. Access to the sites is further facilitated by numerous property tracks. All sites required entry permission from the owners, and compliance with site safety precautions. The location of each site can be determined from its grid reference on the Penrith 1:100,000 sheet. -
ON the PRINCIPLES of GLOBAL CORRELATION of the CONTINENTAL TRIASSIC on the TETRAPODS the Triassic Was a Time of Transition From
Acta Palaeontologica Polonica Vol. 34, No. 2 pp. 149-173 Warszawa, 1989 V. G. OCHEV and M. A. SHISHKIN ON THE PRINCIPLES OF GLOBAL CORRELATION OF THE CONTINENTAL TRIASSIC ON THE TETRAPODS OCHEV, V. G. and SHISHKIN, M. A.: On the principles of global correlation af the continental Triassic on the tetsapods. Acta Palaeont. Polonica, 34, 2, 143--173, 1989. History of the Triassic land vertebrates comprises three successive global epoches referred to as proterosuchian, kannemeyeroid and dinosaur ones. The earliest and the middle epoches are typified by the regional faunal sequence of East Europe. The proterosuchian time spaas here the Neorhachitome and Paroto- suchus faunas, the former being directly correlated with the Induan-Lower Olenekian, and the latter with the Upper Olenekian (Spathian). The Eryosuchus and Mastodonsaurus faunas of the kannemeyeroid epoch in East Europe are Middle Triassic in age and correspond to the Muschelkalk and Lettenkohle respectively. An evidence is brought for contemporaneity of the protero- suchian-kannemeyeroid biotic replacement in Laurasia and Gondwana. This implies the Middle Triassic age of the Cynognathus Zone of South Africa and its equivalents in South America. The bulk of Lystrosausus fauna in Gondwana is suggested to range over the most of, or the whole, Early Triassic. K e y w 0 r d s: Triassic tetrapods, biotic epoches, correlation. V. G. Ochev, Saratov State University, Saratov, USSR; M. A. Shtshktn, PaUleontologtcal Institute, Academy of Sciences of the USSR, Profsoyuznaya, 123 Moscow, USSR. Received: December 1988. INTRODUCTION The Triassic was a time of transition from the late Palaeozoic (the- rapsid) to the true Mesozoic (archosaur) stage of the tetrapod faunal evolution.