An Exhumed Fineâ••Grained Meandering Channel in the Lower
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A 3D Forward Stratigraphic Model of Fluvial Meander-Bend Evolution for Prediction of Point-Bar Lithofacies Architecture
This is a repository copy of A 3D forward stratigraphic model of fluvial meander-bend evolution for prediction of point-bar lithofacies architecture. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/116031/ Version: Accepted Version Article: Yan, N orcid.org/0000-0003-1790-5861, Mountney, NP orcid.org/0000-0002-8356-9889, Colombera, L et al. (1 more author) (2017) A 3D forward stratigraphic model of fluvial meander-bend evolution for prediction of point-bar lithofacies architecture. Computers & Geosciences, 105. pp. 65-80. ISSN 0098-3004 https://doi.org/10.1016/j.cageo.2017.04.012 © 2017 Elsevier Ltd. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/ Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. 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/ Author’s Accepted Manuscript A 3D forward stratigraphic model of fluvial meander-bend evolution for prediction of point-bar lithofacies architecture Na Yan, Nigel P. -
Precise Age and Biostratigraphic Significance of the Kinney Brick Quarry Lagerstätte, Pennsylvanian of New Mexico, USA
Precise age and biostratigraphic significance of the Kinney Brick Quarry Lagerstätte, Pennsylvanian of New Mexico, USA Spencer G. Lucas1, Bruce D. Allen2, Karl Krainer3, James Barrick4, Daniel Vachard5, Joerg W. Schneider6, William A. DiMichele7 and Arden R. Bashforth8 1New Mexico Museum of Natural History, 1801 Mountain Road N.W., Albuquerque, New Mexico, 87104, USA email: [email protected] 2New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, New Mexico, 87801, USA email: [email protected] 3Institute of Geology and Paleontology, University of Innsbruck, Innsbruck, A-6020, Austria email: [email protected] 4Department of Geosciences, Texas Tech University, Box 41053, Lubbock, Texas, 79409, USA email: [email protected] 5Université des Sciences et Technologies de Lille, UFR des Sciences de la Terre, UPRESA 8014 du CNRS, Laboratoire LP3, Bâtiment SN 5, F-59655 Villeneuve d’Ascq, Cédex, France email: [email protected] 6TU Bergakademie Freiberg, Cottastasse 2, D-09596 Freiberg, Germany email:[email protected] 7Department of Paleobiology, NMNH Smithsonian Institution, Washington, DC 20560 email: [email protected] 8Geological Museum, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark email: [email protected] ABSTRACT: The Kinney Brick Quarry is a world famous Late Pennsylvanian fossil Lagerstätte in central New Mexico, USA. The age assigned to the Kinney Brick Quarry (early-middle Virgilian) has long been based more on its inferred lithostratigraphic position than on biostratigraphic indicators at the quarry. We have developed three datasets —-stratigraphic position, fusulinids and conodonts— that in- dicate the Kinney Brick Quarry is older, of middle Missourian (Kasimovian) age. -
1 Running Head: SEQUENCE STRATIGRAPHY of TEXAS
Running Head: SEQUENCE STRATIGRAPHY OF TEXAS MIDDLE PERMIAN PLATFORM CARBONATES OUTCROP-BASED CHARACTERiZATION OF LEONARDIAN PLATFORM CARBONATE IN WEST TEXAS: IMPLICATIONS FOR SEQUENCE STRATIGRAPHIC STYLES IN TRANSITIONAL ICEHOUSE-GREENHOUSE SETTINGS Stephen C. Ruppel, W. Bruce Ward1, and Eduardo E. Ariza Bureau of Economic Geology The University of Texas at Austin 1 Current address: Earthworks LLC, P.O. Box 178, Newtown, CT 06470-0178 1 ABSTRACT The Sierra Diablo Mountains of West Texas contain world class exposures of lower and middle Permian platform carbonates. As such these outcrops offer key insights into the products of carbonate deposition in the transitional icehouse/greenhouse setting of the early-mid Permian that are available in few other places in the world. They also afford an excellent basis for examing how styles of facies and sequence development vary between platform tops and platform margins. Using outcrop data and observations from over 2 mi (3 km) of continuous exposure, we collected detailed data on the facies composition and architecture of high frequency (cycle-scale) and intermediate frequency (high frequency sequence scale) successions within the Leonardian. We used these data to define facies stacking patterns along depositional dip across the platform in both low and high accommodation settings and to document how these patterns vary systematically between and within sequences . These data not only provide a basis for interpreting similar Leonardian platform successions from less well constrained outcrop and subsurface data sets but also point out some important caveats that should be considered serve as an important model for understanding depositional processes during the is part of the Permian worldwide. -
Theuniversityoftexasbul
THEUNIVERSITYOFTEXASBULLETIN No. 3027: July 15, 1930 THE GEOLOGY OF STONEWALL COUNTY, TEXAS By L. T. PATTON Bureau of Economic Geology J. A. Udden, Director £. H. Sellards, Associate Director PUBLISHED BY TOE UNIVERSITY OF TEXAS AUSTIN Publications of The University of Texas Publications Committees GENERAL: Frederic Duncalf Mrs.F. A. Perry J. F.Dobie C. H. Slover J. L.Henderson G. W. Stumberg H. J.Muller A.P. Winston official E. J. Mathews Killis Campbell C. F. Arrowood C.D.Simmons E. C.H.Bantel Bryant Smith The University publishes bulletins four times a month, so numbered that the first two digits of the number show the year of issue and the last two the position in the yearly series. (For example, No. 3001is the first bulletin of the year 1930.) These bulletins comprise the official publica- tions of the University, publications on humanistic and scientific subjects, and bulletins issued from time to time by various divisions of the University. The following bureaus and divisions distribute bulletins issued by them; communications concerning bulletins in these fields should be addressed to TheUniversity of Texas,Austin,Texas,care of the bureau or division issuing the bulletin: Bureau of Business Research, Bureau of Economic Geology, Bureau of Engineering Research, Interscholastic League Bureau, andDivision of Extension. Communications concerning all other publications of the University should be addressed to University Publications,TheUniversity of Texas,Austin. Additionalcopies of this publicationmaybeprocuredfrom the Bureau of Economic Geology, The University of Texas, Austin, Texas THE UNIVERSITY OFTEXAS PREM, AUSTUI THEUNIVERSITYOF TEXASBULLETIN No. 3027: July 15, 1930 THE GEOLOGY OF STONEWALL COUNTY, TEXAS By L. -
The Lower Permian Abo Formation in the Fra Cristobal and Caballo Mountains, Sierra County, New Mexico Spencer G
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/63 The Lower Permian Abo Formation in the Fra Cristobal and Caballo Mountains, Sierra County, New Mexico Spencer G. Lucas, Karl Krainer, Dan S. Chaney, William A. DiMichele, Sebastian Voigt, David S. Berman, and Amy C. Henrici, 2012, pp. 345-376 in: Geology of the Warm Springs Region, Lucas, Spencer G.; McLemore, Virginia T.; Lueth, Virgil W.; Spielmann, Justin A.; Krainer, Karl, New Mexico Geological Society 63rd Annual Fall Field Conference Guidebook, 580 p. This is one of many related papers that were included in the 2012 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. -
Tobey-Dawn-Msc-ERTH-September
Water and Wind: The Fluvial and Eolian Forces Behind the Pennsylvanian-Permian Halgaito Formation, Utah By Dawn E. Tobey Submitted in partial fulfillment of the requirements for the degree of Masters of Science at Dalhousie University Halifax, Nova Scotia September 2020 © Copyright by Dawn E. Tobey, 2020 Table Of Contents List of Tables ............................................................................................................................... v List of Figures ........................................................................................................................... vi Abstract ..................................................................................................................................... vii List of Abbreviations Used ................................................................................................. viii Acknowledgements .................................................................................................................ix Chapter 1: Introduction .......................................................................................................... 1 1.1 Statement of Problem................................................................................................................ 1 1.2 Objectives ....................................................................................................................................... 6 1.3 Contributions of the Author .................................................................................................. -
STRATEGIC STONE STUDY a Building Stone Atlas of NORTH-EAST YORKSHIRE
STRATEGIC STONE STUDY A Building Stone Atlas of NORTH-EAST YORKSHIRE Published May 2012 Derived from BGS digital geological mapping at 1:625,000 scale, British Geological Survey © NE Yorkshire Bedrock Geology NERC. All rights reserved Click on this link to visit NE Yorkshire’s geology and their contribution to known building stones, stone structures and building stone quarries (Opens in new window http://maps.bgs.ac.uk/buildingstone?County=North-EastYorkshire ) NE Yorkshire Strategic Stone Study 1 Stratigraphical column of the Permian (in part),Triassic, Jurassic and Cretaceous rocks and Quaternary deposits in North-east Yorkshire showing the common buildings stones (bold) and alternative stone names. The oldest rocks are at the bottom of the table. Gp., Group; Fm., Formation; Mbr., Member. North East Yorkshire: Permian, Triassic, Jurassic, Cretaceous & Quaternary Building Stones PERIOD GROUP FORMATION MEMBER Common/alternative Stone Name Calcareous Tufa; Aquarium Stone Till (Boulder Clay) and Fluvio-glacial sand Quaternary and gravel; boulders Tertiary Cleveland Dyke Whinstone Flamborough Chalk Fm. Flamborough Chalk; White Chalk Burnham Chalk Fm. Burnham Chalk; White chalk Chalk Group Welton ChalkFm. Cretaceous Ferriby Chalk Fm. Grey chalk ungrouped Hunstanton Fm. Speeton Clay Kimmeridge Clay ungrouped Ampthill Clay North Grimston Upper Calcareous Grit Upper Calcareous Grit Cementstone North Grimston Cementstone Formation Coral Rag Member Coral Rag Malton Oolite Member Malton Oolite; Hildenley Limestone; Corallian Hildenley Stone Group Middle Calcareous Grit Middle Calcareous Grit Coralline Oolite Formation Member Birdsall Calcareous Grit Birdsall Calcareous Grit Member Hambleton Oolite Hambleton Oolite Member Yedmandale Member Passage Beds; Wallstone Lower Calcareous Grit Fm. Lower Calcareous Grit Oxford Clay Fm. -
TMS-01 04 Butler (To D) 14/10/05 10:42 Am Page 43
TMS-01 04 Butler (to_d) 14/10/05 10:42 am Page 43 The Ravenscar Group: a coeval analogue for the Middle Jurassic reservoirs of the North Sea and offshore Mid-Norway N. BUTLER1, M. A. CHARNOCK2, K. O. HAGER2,3 & C. A. WATKINS1 1Robertson Research International Ltd., Llanrhos, Llandudno LL30 1SA, UK (e-mail [email protected]) 2Norsk Hydro AS, Research Centre, N-5020, Bergen, Norway 3Norsk Hydro AS, N-0246, Oslo, Norway Abstract: A palynostratigraphical study of the Middle Jurassic Ravenscar Group, Cleveland Basin, northern England involving the integration of miospore and microplank- ton data with sedimentary facies data has resulted in improvements in the stratigraphical resolution of offshore hydrocarbon-bearing strata in the North Viking Graben and Mid- Norway. The Dogger Formation is of ‘earliest’ Aalenian age and is correlative with the uppermost Dunlin Group, Drake Formation and Båt Group, Ror Formation. The overly- ing Aalenian Saltwick and Eller Beck formations correlate with the Brent Group, Broom–Rannoch–Etive–Ness and the Fangst Group, Ile–Not–‘lower’ Garn genetic packages. The Cloughton Formation is either unrepresented or condensed in the Brent Province and Mid-Norway due to a regional unconformity, which truncates lower Bajocian sediments. The Scarborough Formation is of ‘latest’ early to ‘earliest’ late Bajocian age and correlative with the older part of the Tarbert–Heather and the ‘upper’ Garn–Melke genetic packages. These interpretations contrast markedly with the majority of those published. Despite their maturity of exploration and Methodology and techniques development, Middle Jurassic sandstones of the North Sea and offshore Mid-Norway still repre- The analyses were concentrated on three key sent some of the most prolific hydrocarbon sections near Whitby, Ravenscar and Scar- reservoirs in northwest Europe. -
Preliminary Geologic Map of the Albuquerque 30' X 60' Quadrangle
Preliminary Geologic Map of the Albuquerque 30’ x 60’ Quadrangle, north-central New Mexico By Paul L. Williams and James C. Cole Open-File Report 2005–1418 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2006 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Williams, Paul L., and Cole, James C., 2006, Preliminary Geologic Map of the Albuquerque 30’ x 60’ quadrangle, north-central New Mexico: U.S. Geological Survey Open-File Report 2005-1418, 64 p., 1 sheet scale 1:100,000. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. ii Contents Abstract.................................................................................................................1 Introduction ...........................................................................................................2 Geography and geomorphology.........................................................................3 -
Dinosaur-Plant Interactions Within a Middle Jurassic Ecosystem—Palynology of the Burniston Bay Dinosaur Footprint Locality, Yorkshire, UK
Palaeobio Palaeoenv (2018) 98:139–151 https://doi.org/10.1007/s12549-017-0309-9 ORIGINAL PAPER Dinosaur-plant interactions within a Middle Jurassic ecosystem—palynology of the Burniston Bay dinosaur footprint locality, Yorkshire, UK Sam M. Slater1,2 & Charles H. Wellman2 & Michael Romano3 & Vivi Vajda 1 Received: 3 July 2017 /Revised: 18 September 2017 /Accepted: 25 October 2017 /Published online: 20 December 2017 # The Author(s) 2017. This article is an open access publication Abstract Dinosaur footprints are abundant in the Middle dominated by Araucariacites australis (probably produced by Jurassic Ravenscar Group of North Yorkshire, UK. Footprints Brachyphyllum mamillare), Perinopollenites elatoides and are particularly common within the Bathonian Long Nab Classopollis spp., with additional bisaccate pollen taxa. Member of the Scalby Formation and more so within the so- Abundant Ginkgo huttonii in the macroflora suggests that much called ‘Burniston footprint bed’ at Burniston Bay. The of the monosulcate pollen was produced by ginkgoes. The di- Yorkshire Jurassic is also famous for its exceptional plant mac- verse vegetation of the Cleveland Basin presumably represent- rofossil and spore-pollen assemblages. Here we investigate the ed an attractive food source for herbivorous dinosaurs. The spore-pollen record from the dinosaur footprint-bearing succes- dinosaurs probably gathered at the flood plains for fresh-water sions in order to reconstruct the vegetation and assess possible and also used the non-vegetated plains and coastline as path- dinosaur-plant interactions. We also compare the spore-pollen ways. Although assigning specific makers to footprints is diffi- assemblages with the macroflora of the Scalby Ness Plant Bed, cult, it is clear that a range of theropod, ornithopod and sauro- which occurs within the same geological member as the pod dinosaurs inhabited the area. -
CONTENTS Marl Slate and Basal Permian Breccia at Middridge, Co
CONTENTS BECKINSALE, R. D. see Wadge et al. BELL, J., HOLDEN, J., PETTIGREW, T. H. and SEDMAN, K. W. The Marl Slate and Basal Permian Breccia at Middridge, Co. Durham ... BERTENSHAW, M. p. Temperature time-lags in limestone groundwaters of the southern Pennines: a discussion BRASIER, c. j. see Brasier, M. D. BRASIER, M. D. and BRASIER, C. J. Littoral and fluviatile facies in the 'Kellaways Beds' on the Market Weighton swell CATT, j. A. see Madgett and Catt CREANEY, S. Petrographic textures and vitrinite reflectance variation on the Alston Block, north-east England ... FERGUSON, j. Some aspects of the ecology and growth of the Carboniferous gigantoproductids FLETCHER, B. N. see Knox and Fletcher GALE, N. H. see Wadge et al. GEORGE, T. N. Eustacy and tectonics: sedimentary rhythms and stratigraphical units in British Dinantian corre• lation GREENSMITH, J. T., RAWSON, P. F. and SHALABY, S. E. An association of minor fining-upward cycles and aligned gutter marks in the Middle Lias (Lower Jurassic) of the Yorkshire coast ... HAMILTON, G. Calcareous nannofossils from the Upper Callovian and Lower Oxfordian (Jurassic) of Staffin Bay Isle of Skye, Scotland HIGGINS, A. c. see Varker and Higgins HOLDEN, j. see Bell et al. HOLLIDAY, D. w., NEVES, R. and OWENS, B. Stratigraphy and palynology of early Dinantian (Carboniferous) strata in shallow boreholes near Ravenstonedale, Cumbria ... JEFFERSON, D. p. Cyclic sedimentation in the Holkerian (Mid• dle Visean) north of Settle, Yorkshire JONES, j. M. and SCOTT, P. W. Progress report on fossil fuels - exploration and exploitation KENT, p. E. Subsidence and uplift in East Yorkshire and Lincolnshire: a double inversion KNOX, R. -
Catalogueoftypes22brun.Pdf
UNIVERSITY OF ILLINOIS LIBRARY AT URBANACHAMPAIGN GEOLOGY JUL 7 1995 NOTICE: Return or renew all Library Materials! The Minimum Fee for •adi Lost Book is $50.00. The person charging this material is responsible for its return to the library from which it was withdrawn on or before the Latest Date stamped below. Thett, mutilation, and underlining of books are reasons for discipli- nary action and may result in dismissal from the University. To renew call Telephone Center, 333-8400 UNIVERSITY OF ILLINOIS LIBRARY AT URBANA-CHAMPAIGN &S.19J6 L161—O-1096 'cuLUuy LIBRARY FIELDIANA Geology NEW SERIES, NO. 22 A Catalogue of Type Specimens of Fossil Vertebrates in the Field Museum of Natural History. Classes Amphibia, Reptilia, Aves, and Ichnites John Clay Bruner October 31, 1991 Publication 1430 PUBLISHED BY FIELD MUSEUM OF NATURAL HISTORY Information for Contributors to Fieldiana General: Fieldiana is primarily a journal for Field Museum staff members and research associates, althouj. manuscripts from nonaffiliated authors may be considered as space permits. The Journal carries a page charge of $65.00 per printed page or fraction thereof. Payment of at least 50% of pag< charges qualifies a paper for expedited processing, which reduces the publication time. Contributions from staff, researcl associates, and invited authors will be considered for publication regardless of ability to pay page charges, however, the ful charge is mandatory for nonaffiliated authors of unsolicited manuscripts. Three complete copies of the text (including titl< page and abstract) and of the illustrations should be submitted (one original copy plus two review copies which may b machine-copies).