Facies Analysis and Depositional Environments of the Saints & Sinners Quarry in the Nugget Sandstone of Northeastern Utah Jesse Dean Shumway Brigham Young University
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Geological Processes and Evolution
GEOLOGICAL PROCESSES AND EVOLUTION J.W. HEAD1, R. GREELEY2, M.P. GOLOMBEK3, W.K. HARTMANN4, E. HAUBER5, R. JAUMANN5, P. MASSON6, G. NEUKUM5, L.E. NYQUIST7 and M.H. CARR8 1Department of Geological Sciences, Brown University, Providence, RI 02912 USA 2Department of Geology, Arizona State University, Tempe, AZ 85287 USA 3Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91109 USA 4Planetary Science Institute, Tucson, AZ 85705 USA 5DLR Institute of Space Sensor Technology and Planetary Exploration, Rutherfordstrasse 2, 12484 Berlin-Aldershof, Germany 6University of Paris-Sud, 91405, Orsay Cedex France 7Johnson Space Center, Houston TX 77058 USA 8US Geological Survey, Branch of Astrogeological Studies, 345 Middlefield Road, Menlo Park, CA 94025 USA Received:14 February 2001; accepted:12 March 2001 Abstract. Geological mapping and establishment of stratigraphic relationships provides an overview of geological processes operating on Mars and how they have varied in time and space. Impact craters and basins shaped the crust in earliest history and as their importance declined, evidence of extensive regional volcanism emerged during the Late Noachian. Regional volcanism characterized the Early Hesperian and subsequent to that time, volcanism was largely centered at Tharsis and Elysium, con- tinuing until the recent geological past. The Tharsis region appears to have been largely constructed by the Late Noachian, and represents a series of tectonic and volcanic centers. Globally distributed structural features representing contraction characterize the middle Hesperian. Water-related pro- cesses involve the formation of valley networks in the Late Noachian and into the Hesperian, an ice sheet at the south pole in the middle Hesperian, and outflow channels and possible standing bodies of water in the northern lowlands in the Late Hesperian and into the Amazonian. -
Surface Geology Wind/Bighorn River Basin Wyoming and Montana
WYOMING STATE GEOLOGICAL SURVEY Plate I Thomas A. Drean, State Geologist Wind/Bighorn Basin Plan II - Available Groundwater Determination Technical Memorandum Surface Geology - Wind/Bighorn River Basin SWEET GRASS R25E R5E R15E R30E R10E R20E MONTANA Mm PM Jsg T7S KJ !c Pp Jsg KJ water Qt Surface Geology Ti ! Red Lodge PM DO PM PM Ts Ts p^r PM N ^r DO KJ DO !c Wind/Bighorn River Basin Tts Mm water Mm Ti Ti ^r DO Kmt Ti LOCATION MAP p^r ^r ^r Qt WYOMING Wyoming and Montana Kf Qt Ti p^r !c p^r PM 0 100 250 Miles Tts ^r PM DO Ti Jsg MD Ts Ti MzPz Kmv !Pg Qt compiled DO DO Tts Ts Taw DO DO DO water Qt Kc PM ^r Twl Qt Ob O^ by ^r Mm DO !c MD MONTANA Thr Ti Kc Qr Klc p^r Kmv Kc : # Ts ^r : O^ Nikolaus Gribb, Brett Worman, # Ts # water : PM Taw # Kf : PM !cd : Ket Qb Taw Qu Twp Thr # Ki Twl 345 P$Ma : Thr O^ Qa KJg Tfu : Jsg ^r Qu : :: # Kl (! KJk : Qr Qls Tomas Gracias, and Scott Quillinan Qb : Thr Ts Taw # Tfu 37 PM Kft: : # :: T10S Qls # Thr : # ^r Kc (! Kft Kmt # :::::: p^r :: : Qu KJk Kc MD Taw DO Qu # p^r Qg :: Km KJ WYOMING Taw Ti : Kl 2012 Thr : Qb # # # Qg : water DO Qls ::: !c !Pg !cd MDO water water Kc Qa :::::: :: Kmt ::: : Twl 90 : Ti Ts Qu Qa Qg Kmv !Pcg Mm KJk : Qg : 212 : Qu Qg £¤ Kmv KJ ¨¦§ Tts Taw p^r ^r # Kl : Kf Kf 338 Ob !cd Qu Qu Ttp # (! : : : p^r ::: !Pg O^ MD P$Ma Thr : Qa # DO Km Qls 343 ^r Qls Taw : Qb Qg Qls Qa Km Jsg water (! : Qb # !cd ^r Kc BighornLake : MD # Taw Qa Qls Qt MD A′ MD MD Qg Twl !Pg Qu Qb Tii # Twp ^r water MzPz Qg Tfu Kl ::: Taw Taw Twp Qls : Qt Kmv Qa Ob P$Ma : Thr Qa # Tcr ^r water Qa Kft # Qt O^ -
Dinotracks.Indb 358 1/22/16 11:23 AM Dinosaur Tracks in Eolian Strata: New Insights Into Track Formation, Walking Kinetics and Trackmaker Behavior 18
358 DinoTracks.indb 358 1/22/16 11:23 AM Dinosaur Tracks in Eolian Strata: New Insights into Track Formation, Walking Kinetics and Trackmaker Behavior 18 David B. Loope and Jesper Milàn Dinosaur tracks are abundant in wind-blown hooves of the bison deformed soft, laminated sediment – the Mesozoic deposits, but the nature of loose eolian sand perfect medium to preserve recognizable tracks. The next makes it difficult to determine how they are preserved. This windstorm buried the tracks. Today, the thick cover of grasses also raises the questions: Why would dinosaurs be walking protects the land surface so well that there are no soft, lami- around in dune fields in the first place? And, if they did go nated sediments for cattle to step on. And, if any tracks were, there, why would their tracks not be erased by the next wind somehow, to get formed, no moving sediment would be avail- storm? able to bury them. Mesozoic eolian sediments around the world, which have been the focus of a number of case studies Introduction in recent years, preserve the tracks of dinosaurs that walked on actively migrating sand dunes. This chapter summarizes Most dunes today form only in deserts and along shore- the known occurrences of dinosaur tracks in Mesozoic eo- lines – the only sandy land surfaces that are nearly devoid of lian strata and discusses their unique modes of preservation plants. Normally plants slow the wind at the ground surface and the anatomical and behavioral information about the enough that sand will not move even when the plant cover trackmakers that can be deduced from them. -
Appendix 1 – Environmental Predictor Data
APPENDIX 1 – ENVIRONMENTAL PREDICTOR DATA CONTENTS Overview ..................................................................................................................................................................................... 2 Climate ......................................................................................................................................................................................... 2 Hydrology ................................................................................................................................................................................... 3 Land Use and Land Cover ..................................................................................................................................................... 3 Soils and Substrate .................................................................................................................................................................. 5 Topography .............................................................................................................................................................................. 10 References ................................................................................................................................................................................ 12 1 OVERVIEW A set of 94 potential predictor layers compiled to use in distribution modeling for the target taxa. Many of these layers derive from previous modeling work by WYNDD1, 2, but a -
What Is the Zuni Sandstone Today
What is the ZuniSandstone Today -- 100 Years AfterDutton? A Discussion andReview of JurassicStratigraphy in West-Central New Mexico NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCES OPEN-FILE REPORT 174 by Orin J. Anderson New MexicoBureau of Minesand Mineral Resources 1983 Contents Introduction P. 1 Discussion P. 3 Todilto Limestone - Navajo Sandstone P- 5 San Rafael Group Defined P. 8 Glen CanyonGroup Defined P. 9 MorrisonFormation Subdivided p. 14 Cow SpringsSandstone p. 17 1956 Memorandum from C. H. Dane p. 22 Zuni Sandstone Redefined p. 26 Summary p. 28 ReferencesCited p. 30 Figures Fig. 1 Index map of study area Fig. 2 Stratigraphic nomenclature and correlationchart- 1885 to present Fig. 3 Measured section at type locality of Zuni Sandstone (inside back cover) Fig. 4 Stratigraphiccross-section-Dakota and Zuni sandstones, showing southward thinning of Zuni Sandstone (inside back cover) WHAT IS THE ZUNISANDSTONE TODAY -- 100 YEARS AFTER DUTTON? A DISCUSSION AND REVIEW OF JURASSICSTRATIGRAPHY IN WEST-CENTRAL NEW MEXICO Introduction The massivesequence(s) of light colored, cross bedded sandstonesthat underliethe Dakota Sandstone (Upper Cretaceous) in west-central New Mexico and northeasternArizona were first described and namedby CaptainClarence E. Dutton ofthe U. S. Army Ordinance Corps. His reportentitled "Mount Taylor and the Zuni Plateau"(Dutton, 1885) contains an account of the stratigraphy and structure of those two areas and theimmediately surrounding region(the Zuni Plateau is thepresent day Zuni uplift). In thereport he described a "massive bright redsandstone" that overlies the "basal Triassediments" (the present day ChinleFormation) in theFort Wingate area; this unit henamed "provisionally"the Wingate Sandstone. Overlyingthe Wingate Dutton recognized "a series ofsandstones and sandy shales ..... -
Characterization of Hydraulic Properties Of
Final Report for Award No. DE-FG03-94ER14462 1 Structural Heterogeneities and Paleo Fluid Flow in an Analog Sandstone Reservoir 2001-2004 By David Pollard and Atilla Aydin Department of Geological and Environmental Sciences Stanford University Stanford, California DOE, BES, and Chemical Sciences, Geosciences, and Biosciences Division Final Report for Award No. DE-FG03-94ER14462 2 TABLE OF CONTENTS TABLE OF CONTENTS ............................................................................................................................................2 EXECUTIVE SUMMARY.........................................................................................................................................3 INTRODUCTION AND BACKGROUND ...............................................................................................................4 GEOLOGIC AND STRUCTURAL SETTING .....................................................................................................................4 Regional Geology.................................................................................................................................................4 Principal Structural Elements of the Aztec Sandstone.........................................................................................5 SUMMARY RESULTS FROM THE GRANT PERIOD ........................................................................................6 1. CHEMICAL CHARACTERIZATION OF COLORED ALTERATION BANDS AND PALEO FLUID FLOW .................................6 2. CHARACTERIZING -
Sequence Stratigraphic Expression of Flexural Subsidence: Middle
SEQUENCE STRATIGRAPHIC EXPRESSION OF FLEXURAL SUBSIDENCE: MIDDLE JURASSIC TWIN CREEK LIMESTONE, WYOMING, U.S.A. by BOLTON HOWES (Under the Direction of Steve Holland) ABSTRACT In southwestern Wyoming, the Bajocian to Callovian Twin Creek Limestone records the incipient deposition on a foreland basin in the Sundance Seaway. The sequence stratigraphy of the Twin Creek Limestone is described in the Wyoming Range of southwestern Wyoming, and the geometry of the foreland basin is described mathematically based on estimates flexural rigidity of the underlying crust and the subsidence caused by a thrust load in central Idaho. Four depositional sequences are described. These sequences are correlated to the Bighorn Basin based on existing biostratigraphic correlations and descriptions of the sequence stratigraphic architecture of Middle Jurassic strata in the Bighorn Basin. Modeling of the flexural subsidence of the foreland basin indicates that to account for the geometry of the foreland basin some form of long-wavelength subsidence must be superimposed on the flexural subsidence associated with the thrust load in central Idaho. INDEX WORDS: carbonate rocks; Jurassic; foreland basin; sequence stratigraphy SEQUENCE STRATIGRAPHIC EXPRESSION OF FLEXURAL SUBSIDENCE: MIDDLE JURASSIC TWIN CREEK LIMESTONE, WYOMING, U.S.A. By BOLTON HOWES B.A., Macalester College, 2015 A Thesis Submitted to the Graduate Faculty of The University of Georgia in Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE ATHENS, GEORGIA 2017 © 2017 Bolton Howes All Rights Reserved SEQUENCE STRATIGRAPHIC EXPRESSION OF FLEXURAL SUBSIDENCE: MIDDLE JURASSIC TWIN CREEK LIMESTONE, WYOMING, U.S.A. by BOLTON HOWES Major Professor: Steven M. Holland Committee: L. Bruce Railsback David S. -
Earliest Jurassic U-Pb Ages from Carbonate Deposits in the Navajo Sandstone, Southeastern Utah, USA Judith Totman Parrish1*, E
https://doi.org/10.1130/G46338.1 Manuscript received 3 April 2019 Revised manuscript received 10 July 2019 Manuscript accepted 11 August 2019 © 2019 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. Published online 4 September 2019 Earliest Jurassic U-Pb ages from carbonate deposits in the Navajo Sandstone, southeastern Utah, USA Judith Totman Parrish1*, E. Troy Rasbury2, Marjorie A. Chan3 and Stephen T. Hasiotis4 1 Department of Geological Sciences, University of Idaho, P.O. Box 443022, Moscow, Idaho 83844, USA 2 Department of Geosciences, Stony Brook University, Stony Brook, New York 11794, USA 3 Department of Geology and Geophysics, University of Utah, 115 S 1460 E, Room 383, Salt Lake City, Utah 84112-0102, USA 4 Department of Geology, University of Kansas, 115 Lindley Hall, 1475 Jayhawk Boulevard, Lawrence, Kansas 66045-7594, USA ABSTRACT with the lower part of the Navajo Sandstone New uranium-lead (U-Pb) analyses of carbonate deposits in the Navajo Sandstone in across a broad region from southwestern Utah southeastern Utah (USA) yielded dates of 200.5 ± 1.5 Ma (earliest Jurassic, Hettangian Age) to northeastern Arizona (Blakey, 1989; Hassan and 195.0 ± 7.7 Ma (Early Jurassic, Sinemurian Age). These radioisotopic ages—the first re- et al., 2018). The Glen Canyon Group is under- ported from the Navajo erg and the oldest ages reported for this formation—are critical for lain by the Upper Triassic Chinle Formation, understanding Colorado Plateau stratigraphy because they demonstrate that initial Navajo which includes the Black Ledge sandstone (e.g., Sandstone deposition began just after the Triassic and that the base of the unit is strongly Blakey, 2008; Fig. -
Stratigraphy and Sedimentology of a Dry to Wet Eolian Depositional System, Burns Formation, Meridiani Planum, Mars
Earth and Planetary Science Letters 240 (2005) 11–72 www.elsevier.com/locate/epsl Stratigraphy and sedimentology of a dry to wet eolian depositional system, Burns formation, Meridiani Planum, Mars J.P. Grotzinger a,*, R.E. Arvidson b, J.F. Bell III c, W. Calvin d, B.C. Clark e, D.A. Fike a, M. Golombek f, R. Greeley g, A. Haldemann f, K.E. Herkenhoff h, B.L. Jolliff b, A.H. Knoll i, M. Malin j, S.M. McLennan k, T. Parker e, L. Soderblom g, J.N. Sohl-Dickstein b, S.W. Squyres b, N.J. Tosca k, W.A. Watters a a Massachusetts Inst. of Technology, Earth, Atmos. and Planetary Sci., Cambridge, MA 02139, USA b Department Earth and Planetary Sciences, Washington University, St. Louis, MO 63130, USA c Department of Astronomy, Space Sciences Bldg. Cornell University, Ithaca, NY 14853, USA d University of Nevada, Reno, NV 89501, USA e Lockheed Martin Corporation, Littleton, CO 80127, USA f Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA g Department Geological Sciences, Arizona State University, Box 871404, Tempe, AZ 85287-1404, USA h U.S. Geological Survey, Flagstaff, AZ 86001, USA i Botanical Museum, Harvard University, Cambridge MA 02138, USA j Malin Space Science Systems, Inc., San Diego, CA 92191, USA k Department of Geosciences, State University of New York, Stony Brook, NY 11794-2100, USA Accepted 22 September 2005 Editor: A.N. Halliday Abstract Outcrop exposures of sedimentary rocks at the Opportunity landing site (Meridiani Planum) form a set of genetically related strata defined here informally as the Burns formation. -
Geologic Map of Alaska
Geologic Map of Alaska Compiled by Frederic H. Wilson, Chad P. Hults, Charles G. Mull, and Susan M. Karl Pamphlet to accompany Scientific Investigations Map 3340 2015 U.S. Department of the Interior U.S. Geological Survey Front cover. Color shaded relief map of Alaska and surroundings. Sources: 100-meter-resolution natural image of Alaska, http://nationalmap.gov/small_scale/mld/nate100.html; rivers and lakes dataset, http://www.asgdc.state.ak.us/; bathymetry and topography of Russia and Canada, https://www.ngdc.noaa.gov/mgg/global/global.html. Back cover. Previous geologic maps of Alaska: 1906—Brooks, A.H., Abbe, Cleveland, Jr., and Goode, R.U., 1906, The geography and geology of Alaska; a summary of existing knowledge, with a section on climate, and a topographic map and description thereof: U.S. Geological Survey Professional Paper 45, 327 p., 1 sheet. 1939—Smith, P.S., 1939, Areal geology of Alaska: U.S. Geological Survey Professional Paper 192, 100 p., 18 plates. 1957—Dutro, J.T., Jr., and Payne, T.G., 1957, Geologic map of Alaska: U.S. Geological Survey, scale 1:2,500,000. 1980—Beikman, H.M., 1980, Geologic map of Alaska: U.S. Geological Survey Special Map, scale 1:2,500,000, 2 sheets. Geologic Map of Alaska Compiled by Frederic H. Wilson, Chad P. Hults, Charles G. Mull, and Susan M. Karl Pamphlet to accompany Scientific Investigations Map 3340 2015 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Director U.S. -
Ichnology As a Tool in Carbonate Reservoir Characterization, Khuff Formation Gulf Petrolink, Bahrain
GeoArabia, v. 14, no. 3, 2009, p. 17-38 Ichnology as a tool in carbonate reservoir characterization, Khuff Formation Gulf PetroLink, Bahrain Ichnology as a tool in carbonate reservoir characterization: A case study from the Permian – Triassic Khuff Formation in the Middle East Dirk Knaust ABSTRACT In the Upper Permian to Lower Triassic Khuff Formation in the Arabian Gulf, a vast shallow-marine carbonate platform developed broad facies belts with little significant changes in the lithofacies. However, trace fossil assemblages and ichnofabrics, in combination with sedimentological observations, serve in subdividing this platform and in distinguishing sub-environments. From proximal to distal, these are sabkha and salina, tidal flat, restricted lagoon, open lagoon, platform margin, shoreface/inner ramp, slope/outer ramp and basin/deeper intra-shelf. In this way, changes in relative sea level can be better reconstructed and guide the sequence stratigraphic interpretation. Meter- scale shallowing-upward cycles dominate the succession and, in addition to conventional methods, bioturbation, trace fossil assemblages and tiering patterns aid in interpreting subtidal, lower and upper intertidal and supratidal portions of these peritidal cycles. Bioturbation (and cryptobioturbation) have an impact on the primary reservoir quality before diagenetic processes overprint the deposits. For instance, deposit-feeders (such as vermiform organisms) introduce a certain amount of mud and decrease porosity and permeability considerably, whereas others like the Zoophycos-producers fill their dwellings with ooid grains and turn a mudstone from a barrier to a flow unit. This novel study demonstrates the value of ichnological information in carbonate reservoir characterization and the significance of trace fossil analysis in facies interpretation, reservoir zonation and the impact of bioturbation on the reservoir quality. -
The Cambrian-Ordovician Siliciclastic Platform of the Balcarce Formation
Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España Poiré, D.G.; Spalletti, L.A.; Del Valle, A. The Cambrian-Ordovician siliciclastic platform of the Balcarce Formation (Tandilia System, Argentina): Facies, trace fossils, palaeoenvironments and sequence stratigraphy Geologica Acta: an international earth science journal, vol. 1, núm. 1, 2003, pp. 41-60 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50510105 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Geologica Acta, Vol.1, Nº1, 2003, 41-60 Available online at www.geologica-acta.com The Cambrian-Ordovician siliciclastic platform of the Balcarce Formation (Tandilia System, Argentina): Facies, trace fossils, palaeoenvironments and sequence stratigraphy D.G. POIRÉ 1 L.A. SPALLETTI 1 and A. DEL VALLE 1 Centro de Investigaciones Geológicas. UNLP-CONICET calle 1 n° 644, 1900 La Plata, Argentina. E-mail: [email protected] ABSTRACT The Lower Palaeozoic sedimentary cover of the Tandilia (Balcarce Formation) is made up of thick quartz are- nite beds together with kaolinitic claystones and thin fine-grained conglomerates. The Balcarce Formation was formed in the nearshore and inner shelf environments of a tide-dominated and storm influenced open platform. It shows many features suggesting tidal sedimentation. Coarse-grained facies were formed by sand bar migra- tion and accretion. Heterolithic packages are interpreted as interbar (swale) deposits.