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Depositional Systems in the Paluxy Formation (Lower Cretaceous), Northeast Texas- Oil,Gas, and Groundwater Resources by Charles A
Geological Circular 77-8 Depositional Systems in the Paluxy Formation (Lower Cretaceous), Northeast Texas- Oil,Gas, and Groundwater Resources BY Charles A. Caughey BUREAU OF ECONOMIC GEOLOGY THE UNIVERSITY OF TEXAS AT AUSTIN AUSTIN, TEXAS 78712 W.L. FISHER, DIRECTOR 1977 Second Printing, 1985 GEOLOGICAL CIRCULAR 77-8 Depositional Systems in thePaluxy Formation (Lower Cretaceous), Northeast Texas- Oil,Gas, and Groundwater Resources BY Charles A. Caughey BUREAU OF ECONOMIC GEOLOGY THE UNIVERSITY OF TEXAS AT AUSTIN AUSTIN, TEXAS 78712 W.L. FISHER, DIRECTOR 1977 SecondPrinting, 1985 Contents Abstract 1 Dispersal patterns 28 Introduction 1 Structural influence 28 Structural framework 3 Resources 28 Stratigraphicrelationships 4 Groundwater 29 Sedimentary facies 5 Outcrop 29 Depositions!systems 8 Subsurface 29 Fluvial system 8 South area 30 Channel-fill and floodbasin facies 9 Meanderbelt facies 11 Central area 31 Fluvial model 12 North area 34 Delta system 13 Conclusions 35 Coastal barrier facies 14 Oil and gas 35 Proximal subfacies 14 Minor producingareas 38 Distal subfacies 16 South Bosque field 38 Lagoon facies 17 Updip trend 38 Deltamodel 19 Major producingareas 41 Classification 19 Fault zone trend 41 Holocene analog 19 Downdipproduction 42 Strandplain system 22 Proximal trend 42 Strandplain facies 22 Distal trend 43 Strandplainmodel 26 Summary 45 Sediment dispersal 27 References 47 Source areas 27 Appendix .. 50 Figures 1. Location map 2 6. Depositional systemsand facies,Paluxy 2. Major structural features of northeast Formationand equivalent lithostrati- Texas 3 graphic units,northeast Texas 7 3. Distribution of Paluxy Formation and 7. Representativeelectric logpatternand related stratigraphic units,surface and shale content of channel sequencesin the subsurface,northeast Texas 4 channel-fill and floodbasin facies,Paluxy fluvial system 9 4. -
Aptian–Albian) of Texas and Oklahoma
Reappraisal of the tribosphenidan mammals from the Trinity Group (Aptian–Albian) of Texas and Oklahoma BRIAN M. DAVIS and RICHARD L. CIFELLI Davis, B.M. and Cifelli, R.L. 2011. Reappraisal of the tribosphenidan mammals from the Trinity Group (Aptian–Albian) of Texas and Oklahoma. Acta Palaeontologica Polonica 56 (3): 441–462. The Trinity therians have long been the focus of attempts to reconstruct the evolutionary history of higher mammals, es− pecially in the context of the development of tribospheny. In this paper, we update the taxonomy of the tribosphenidan taxa known from the Trinity Group and establish with more confidence the premolar/molar count in each. Many isolated specimens can be referred to a specific tooth locus. Additional diversity is revealed within the Deltatheroida, with the de− scription of an additional species of Oklatheridium; Pappotherium is here considered a likely metatherian based on the in− ferred presence of four molars, while Holoclemensia is a basal eutherian (the opposite of some traditional interpretations). The remainder of the genera, Kermackia and Slaughteria, cannot be allied with either of the living groups of tribo− sphenidan mammals using the available data. We identify strong morphological diversity within this assemblage of stem taxa, including modifications to the traditional tribosphenic occlusal pattern in Kermackia. Mammalian evolution at the base of the tribosphenidan radiation was complex, and this underscores the need for caution when interpreting the mor− phology and relationships of taxa known by incomplete material. Key words: Tribosphenida, Metatheria, Eutheria, Deltatheroida, Trinity Group, Early Cretaceous. Brian M. Davis [[email protected]] and Richard L. Cifelli [[email protected]], Department of Zoology and Sam Noble Oklahoma Museum of Natural History, University of Oklahoma, 2401 Chautauqua Ave, Norman, OK, 73072, USA. -
Geology of the Northern Perth Basin, Western Australia
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/233726107 Geology of the northern Perth Basin, Western Australia. A field guide Technical Report · June 2005 CITATIONS READS 15 1,069 4 authors: Arthur John Mory David Haig Government of Western Australia University of Western Australia 91 PUBLICATIONS 743 CITATIONS 61 PUBLICATIONS 907 CITATIONS SEE PROFILE SEE PROFILE Stephen Mcloughlin Roger M. Hocking Swedish Museum of Natural History Geological Survey of Western Australia 143 PUBLICATIONS 3,298 CITATIONS 54 PUBLICATIONS 375 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Lower Permian bryozoans of Western Australia View project Late Palaeozoic palynology of Dronning Maud Land, Antarctica View project All content following this page was uploaded by Stephen Mcloughlin on 05 May 2017. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Department of Industry and Resources RECORD GEOLOGY OF THE NORTHERN PERTH 2005/9 BASIN, WESTERN AUSTRALIA — A FIELD GUIDE by A. J. Mory, D. W. Haig, S. McLoughlin, and R. M. Hocking Geological Survey of Western Australia GEOLOGICAL SURVEY OF WESTERN AUSTRALIA Record 2005/9 GEOLOGY OF THE NORTHERN PERTH BASIN, WESTERN AUSTRALIA — A FIELD GUIDE by A. J. Mory, D. W. Haig1, S. McLoughlin2, and R. M. Hocking 1 School of Earth and Geographical Sciences, The University of Western Australia 2 School of Natural Resource Sciences, Queensland University of Technology Perth 2005 MINISTER FOR STATE DEVELOPMENT Hon. -
L ANDERSON Thinking Is More Important Than Elaborate
Stratigraphy of the Fredericksburg Group, East Texas Basin L ANDERSON thinking is more important than elaborate FRANK PH.D. PROFESSOR OF GEOLOGY BAYLOR UNIVERSITY 1929-1934 Objectives of Geological Training at Baylor The training of a geologist in a university covers but a few years; his education continues throughout his active life. The purposes of train ing geologists at Baylor University are to provide a sound basis of understanding and to foster a truly geological point of view, both of which are essential for continued professional growth. The staff considers geology to be unique among sciences since it is primarily a field science. All geologic research in cluding that done in laboratories must be firmly supported by field observations. The student is encouraged to develop an inquiring ob jective attitude and to examine critically all geological and principles. The development of a mature and professional attitude toward geology and geological research is a principal concern of the department. Cover: Isopach of the Fredericksburg Group. THE BAYLOR PRINTING SERVICE WACO, TEXAS BAYLOR GEOLOGICAL STUDIES BULLETIN NO. 47 Stratigraphy of the Fredericksburg Group, East Texas Basin L. Marlow Anderson BAYLOR UNIVERSITY Department of Geology Waco, Texas Spring 1989 Baylor Geological Studies EDITORIAL STAFF Janet L. Burton, Editor O. T. Hayward, Ph.D., Advisor, Cartographic Editor general and urban geology and what have you Joe C. Yelderman, Jr., Ph.D., Associate Editor hydrogeology Peter M. Allen, Ph.D. urban and environmental geology, hydrology Harold H. Beaver, Ph.D. stratigraphy, petroleum geology Rena Bonem, Ph.D. paleontology, paleoecology Brown, Ph.D. structural tectonics S. -
Mineralogy and Geochemistry of Atypical Reduction Spheroids from the Tumblagooda Sandstone, Western Australia
Sedimentology Mineralogy and geochemistry of atypical reduction spheroids from the Tumblagooda Sandstone, Western Australia Journal: Sedimentology Manuscript ID SED-2019-OM-038.R1 Manuscript Type: Original Manuscript Date Submitted by the 08-Jul-2019 Author: Complete List of Authors: Fox, David; Commonwealth Scientific and Industrial Research Organisation, Mineral Resources; Curtin University, School of Earth and Planetary Sciences Spinks, Sam; Commonwealth Scientific and Industrial Research Organisation, Mineral Resources Thorne, Robert; Commonwealth Scientific and Industrial Research Organisation, Mineral Resources Barham, Milo; Curtin University, Department of Applied Geology Aspandiar, Mehrooz; Curtin University, School of Earth and Planetary Sciences Armstrong, Joseph; University of Aberdeen, Geology and Petroleum Geology; Commonwealth Scientific and Industrial Research Organisation, Mineral Resources Uysal, Tonguc; Commonwealth Scientific and Industrial Research Organisation, Energy Timms, Nick; Curtin University, Department of Applied Geology Pearce, Mark; Commonwealth Scientific and Industrial Research Organisation, Mineral Resources Verrall, Michael; Commonwealth Scientific and Industrial Research Organisation, Mineral Resources Godel, Belinda; Commonwealth Scientific and Industrial Research Organisation, Mineral Resources Whisson, Brad; LabWest Minerals Analysis Pty Ltd Red beds, Diagenesis, Redox, Carnarvon Basin, Metal-reducing bacteria, Keywords: Haematite, Perth Basin, Svanbergite Note: The following files were submitted by the author for peer review, but cannot be converted to PDF. You must view these files (e.g. movies) online. KAL17_1 XRD.svg KAL17_29 XRD.svg 4_SHARP_0017_simple_volume_rendering.mpg 37_SHARP_0018_3D_movie1.mpg Sedimentology Page 54 of 99 1 1 Mineralogy and geochemistry of atypical 2 reduction spheroids from the Tumblagooda 3 Sandstone, Western Australia 4 5 6 David C. M. Fox1,2, Samuel C. Spinks1, Robert L. Thorne1, Milo Barham2,3, Mehrooz 7 Aspandiar2, Joseph G. -
Sedimentary Cycles in a Mesoproterozoic Aeolian Erg-Margin Succession: Mangabeira Formation, Espinhaço Supergroup, Brazil
This is a repository copy of Sedimentary cycles in a Mesoproterozoic aeolian erg-margin succession: Mangabeira Formation, Espinhaço Supergroup, Brazil. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/110242/ Version: Accepted Version Article: Bállico, MB, Scherer, CMS, Mountney, NP orcid.org/0000-0002-8356-9889 et al. (4 more authors) (2017) Sedimentary cycles in a Mesoproterozoic aeolian erg-margin succession: Mangabeira Formation, Espinhaço Supergroup, Brazil. Sedimentary Geology, 349. pp. 1-14. ISSN 0037-0738 https://doi.org/10.1016/j.sedgeo.2016.12.008 © 2016 Elsevier B.V. Licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/ Reuse Unless indicated otherwise, fulltext items are protected by copyright with all rights reserved. The copyright exception in section 29 of the Copyright, Designs and Patents Act 1988 allows the making of a single copy solely for the purpose of non-commercial research or private study within the limits of fair dealing. The publisher or other rights-holder may allow further reproduction and re-use of this version - refer to the White Rose Research Online record for this item. Where records identify the publisher as the copyright holder, users can verify any specific terms of use on the publisher’s website. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ ÅÒ Sedimentary cycles in a Mesoproterozoic aeolian erg-margin succession: Mangabeira Formation, Espinhac¸o Supergroup, Brazil M.B. -
Bioturbation in Aquatic Environments: Linking Past and Present Benthic
Vol. 2: 201–205, 2008 AQUATIC BIOLOGY Printed June 2008 doi: 10.3354/ab00051 Aquat Biol Published online June 19, 2008 OPEN ACCESS THEME SECTION Bioturbation in aquatic environments: linking past and present Idea and coordination: Martin Solan, Liam G. Herringshaw CONTENTS Gingras MK, Dashtgard SE, MacEachern JA, Pemberton SG Herringshaw LG, Solan M Biology of shallow marine ichnology: a modern Benthic bioturbation in the past, present perspective ……………………………………….……… 255–268 and future ………………………………………………… 201–205 White DS, Miller MF Teal LR, Bulling MT, Parker ER, Solan M Benthic invertebrate activity in lakes: linking Global patterns of bioturbation intensity and present and historical bioturbation patterns ……… 269–277 mixed depth of marine soft sediments ……………… 207–218 Maire O, Lecroart P, Meysman F, Rosenberg R, Herringshaw LG, Davies NS Duchêne JC, Grémare A Bioturbation levels during the end-Ordovician Quantification of sediment reworking rates in extinction event: a case study of shallow bioturbation research: a review ……………………… 219–238 marine strata from the Welsh Basin ………………… 279–287 Meysman FJR, Malyuga VS, Boudreau BP, Solan M, Batty P, Bulling MT, Godbold JA Middelburg JJ How biodiversity affects ecosystem processes: Quantifying particle dispersal in aquatic sediments implications for ecological revolutions and at short time scales: model selection ………………… 239–254 benthic ecosystem function …………………….……… 289–301 Resale or republication not permitted without written consent of the publisher Benthic bioturbation in the past, present and future Liam G. Herringshaw1,*, Martin Solan2 1Geology & Petroleum Geology, School of Geosciences, Meston Building, University of Aberdeen, Aberdeen AB24 3UE, UK 2Oceanlab, University of Aberdeen, Main Street, Newburgh, Aberdeenshire AB41 6FL, UK Understanding how ecosystems function at present is trace fossils (ichnology) can provide a wealth of new critical to any assessment of how they functioned in the information for aquatic biologists, ecologists, sedi- past and of how they will function in the future. -
Paleontological Contributions
Paleontological Contributions Number 14 The first giant raptor (Theropoda: Dromaeosauridae) from the Hell Creek Formation Robert A. DePalma, David A. Burnham, Larry D. Martin, Peter L. Larson, and Robert T. Bakker October 30, 2015 Lawrence, Kansas, USA ISSN 1946-0279 (online) paleo.ku.edu/contributions Life restoration by Emily Willoughby of Dakotaraptor steini running with the sparrow-sized birds, Cimolopteryx petra while the mammal, Purgatorius, can be seen in the foreground. Paleontological Contributions October 30, 2015 Number 14 THE FIRST GIANT RAPTOR (THEROPODA: DROMAEOSAURIDAE) FROM THE HELL CREEK FORMATION Robert A. DePalma1,2, David A. Burnham2,*, Larry D. Martin2,†, Peter L. Larson3 and Robert T. Bakker4 1 Department of Vertebrate Paleontology, The Palm Beach Museum of Natural History, Fort Lauderdale, Florida; 2 University of Kansas Bio- diversity Institute, Lawrence, Kansas; 3Black Hills Institute of Geological Research, Hill City, South Dakota; 4Houston Museum of Nature and Science, Houston, Texas; e-mail: [email protected] ABSTRACT Most dromaeosaurids were small- to medium-sized cursorial, scansorial, and arboreal, sometimes volant predators, but a comparatively small percentage grew to gigantic proportions. Only two such giant “raptors” have been described from North America. Here, we describe a new giant dromaeosaurid, Dakotaraptor steini gen. et sp. nov., from the Hell Creek Formation of South Dakota. The discovery represents the first giant dromaeosaur from the Hell Creek Formation, and the most recent in the fossil record worldwide. A row of prominent ulnar papilli or “quill knobs” on the ulna is our first clear evidence for feather quills on a large dromaeosaurid forearm and impacts evolutionary reconstructions and functional morphology of such derived, typically flight-related features. -
Occurrence, Availability, and Chemical Quality of Ground
TEXAS DEPARTMENT OF WATER RESOURCES REPORT 269 OCCURRENCE, AVAILABILITY, AND CHEMICAL QUALITY OF GROUND WATER IN THE CRETACEOUS AQUIFERS OF NORTH-CENTRAL TEXAS VOLUME 1 Phillip L. Nordstrom, Geologist April 1982 TEXAS DEPARTMENT OF WATER RESOURCES Harvey Davis, Executive Director TEXAS WATER DEVELOPMENT BOARD Louis A. Beecherl Jr., Chairman John H. Garrett, Vice Chairman George W. McCleskey W. 0. Bankston Glen E. Roney Lonnie A. “Bo” Pilgrim TEXAS WATER COMMISSION Felix McDonald, Chairman Dorsey B. Hardeman, Commissioner Lee B. M. Biggart, Commissioner Authorization for use or reproduction of any original material contained in this publication, i.e., not obtained from other sources, is freely granted. The Department would appreciate acknowledgement. Published and distributed by the Texas Department of Water Resources Post Office Box 13087 Austin, Texas 78711 ii __ TABLE OF CONTENTS Page SUMMARY AND CONCLUSIONS . 1 INTRODUCTION . .. 3 Purpose and Scope . 3 Location and Extent . 3 Physiography . 3 Climate . 4 Population . 4 Economy . 4 Previous Investigations . 4 Acknowledgements . 7 Method of Investigation . 7 Well-Numbering System . 7 Metric Conversion . 8 GEOLOGY AS RELATED TO THE OCCURRENCE OF GROUND WATER . 9 Geologic History . 9 Paleozoic . 9 Cretaceous . 9 Tertiary and Quaternary . 9 General Stratigraphy . 9 Structure . 10 STRATIGRAPHY OF THE WATER-BEARING FORMATIONS . 12 Paleozoic Rocks . 12 Antlers . 13 iii TABLE OF CONTENTS – Continued Page Twin Mountain Formation . 13 Paluxy Formation . 14 Woodbine Group . 14 Blossom Sand . 15 Nacatoch Sand . 15 CHEMICAL QUALITY OF GROUND WATER AS RELATED TO USE . 15 General Chemical Quality of Ground Water . 15 Quality Criteria or Standards . 16 Municipal . 16 Primary Standards . 20 Secondary Standards . -
The Ontogenetic Osteohistology of Tenontosaurus Tilletti
The Ontogenetic Osteohistology of Tenontosaurus tilletti Sarah Werning*¤ Department of Zoology and Sam Noble Oklahoma Museum of Natural History, University of Oklahoma, Norman, Oklahoma, United States of America Abstract Tenontosaurus tilletti is an ornithopod dinosaur known from the Early Cretaceous (Aptian-Albian) Cloverly and Antlers formations of the Western United States. It is represented by a large number of specimens spanning a number of ontogenetic stages, and these specimens have been collected across a wide geographic range (from central Montana to southern Oklahoma). Here I describe the long bone histology of T. tilletti and discuss histological variation at the individual, ontogenetic and geographic levels. The ontogenetic pattern of bone histology in T. tilletti is similar to that of other dinosaurs, reflecting extremely rapid growth early in life, and sustained rapid growth through sub-adult ontogeny. But unlike other iguanodontians, this dinosaur shows an extended multi-year period of slow growth as skeletal maturity approached. Evidence of termination of growth (e.g., an external fundamental system) is observed in only the largest individuals, although other histological signals in only slightly smaller specimens suggest a substantial slowing of growth later in life. Histological differences in the amount of remodeling and the number of lines of arrested growth varied among elements within individuals, but bone histology was conservative across sampled individuals of the species, despite known paleoenvironmental differences between the Antlers and Cloverly formations. The bone histology of T. tilletti indicates a much slower growth trajectory than observed for other iguanodontians (e.g., hadrosaurids), suggesting that those taxa reached much larger sizes than Tenontosaurus in a shorter time. -
Osteology of a Near-Complete Skeleton of Tenontosaurus Tilletti (Dinosauria: Ornithopoda) from the Cloverly Formation, Montana, USA
Osteology of a Near-Complete Skeleton of Tenontosaurus tilletti (Dinosauria: Ornithopoda) from the Cloverly Formation, Montana, USA A report submitted in partial fulfilment of the requirements for the degree of MEarthSci Geology (Hons.), University of Manchester Jonathan Tennant 70406912 MEarthSci Geology (Hons.) School of Earth, Atmospheric and Environmental Sciences University of Manchester Williamson Building Oxford Road Manchester M13 9PL Osteology of Tenontosaurus tilletti Contents Figures and Tables..............................................................................................................................................3 1.0 Abstract .............................................................................................................................................................6 2.0 Introduction ......................................................................................................................................................7 2.1 Aims and Objectives....................................................................................................................................7 2.2 Institutional Abbreviations ........................................................................................................................9 3.0 Previous Work ............................................................................................................................................... 11 3.1 The Cloverly Formation .......................................................................................................................... -
Kalbarri National Park Management Plan 2015
Kalbarri National Park ‘nature’s window’ management plan 83 2015 Conservation Commission WESTERN AUSTRALIA Department of Parks and Wildlife 17 Dick Perry Avenue KENSINGTON WA 6151 Phone: (08) 9219 9000 Fax: (08) 9334 0498 www.dpaw.wa.gov.au © State Government of Western Australia 2015 August 2015 This work is copyright. You may download, display, print and reproduce this material in unaltered form (retaining this notice) for personal, non-commercial use or use within your organisation. Apart from any other use as permitted under the Copyright Act 1968, all other rights are reserved. Requests and enquiries concerning reproduction and rights should be addressed to the Department of Parks and Wildlife. ISBN 978-1-921703-57-7 (print) ISBN 978-1-921703-58-4 (online) This management plan was prepared by the Conservation Commission of Western Australia through the agency of the Department of Parks and Wildlife. Questions regarding this management plan should be directed to: Planning Branch Department of Parks and Wildlife 17 Dick Perry Avenue, Kensington WA 6151 Locked Bag 104 Bentley Delivery Centre WA 6983 Phone: (08) 9219 9000 Email: [email protected] The recommended reference for this publication is: Department of Parks and Wildlife (2015), Kalbarri National Park management plan 2015. Management plan number 83. Department of Parks and Wildlife, Perth. This document is available in alternative formats on request. Front cover photos Main Nature’s Window at The Loop. Photo – Melissa Loomes/Parks and Wildlife Top right Coastal cliffs. Photo – Rory Chapple/Parks and Wildlife Top left Branching fringe lily (Thysanotus dichotomus). Photo – Rory Chapple/Parks and Wildlife Header photo View of The Loop from Nature’s Window.