Western Interior Seaway
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Redalyc.Preliminary Report on a Late Cretaceous Vertebrate Fossil
Boletín de la Sociedad Geológica Mexicana ISSN: 1405-3322 [email protected] Sociedad Geológica Mexicana, A.C. México Rivera-Sylva, Héctor E.; Frey, Eberhard; Palomino-Sánchez, Francisco J.; Guzmán-Gutiérrez, José Rubén; Ortiz-Mendieta, Jorge A. Preliminary Report on a Late Cretaceous Vertebrate Fossil Assemblage in Northwestern Coahuila, Mexico Boletín de la Sociedad Geológica Mexicana, vol. 61, núm. 2, 2009, pp. 239-244 Sociedad Geológica Mexicana, A.C. Distrito Federal, México Available in: http://www.redalyc.org/articulo.oa?id=94316034014 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 Preliminary Report on a Late Cretaceous Vertebrate Fossil Assemblage in Northwestern Coahuila, Mexico 239 BOLETÍN DE LA SOCIEDAD GEOLÓGICA MEXICANA VOLUMEN 61, NÚM. 2, 2009, P. 239-244 D GEOL DA Ó E G I I C C O A S 1904 M 2004 . C EX . ICANA A C i e n A ñ o s Preliminary Report on a Late Cretaceous Vertebrate Fossil Assemblage in Northwestern Coahuila, Mexico Héctor E. Rivera-Sylva1, Eberhard Frey2, Francisco J. Palomino-Sánchez3, José Rubén Guzmán-Gutiérrez4, Jorge A. Ortiz-Mendieta5 1 Departamento de Paleontología, Museo del Desierto. Pról. Pérez Treviño 3745, 25015, Saltillo, Coah., México. 2 Geowissenschaftliche Abteilung,Staatliches Museum für Naturkunde Karlsruhe. Karlsruhe, Alemania. 3 Laboratorio de Petrografía y Paleontología, Instituto Nacional de Estadística, Geografía e Informática, Aguascalientes, Ags., México. 4 Centro para la Conservación del Patrimonio Natural y Cultural de México, Aguascalientes, Ags., México. -
The Petroleum Potential of H Serpentine Plugs" and Associated Rocks, Central and South Texas
BAYLOR FALL 1986 ulletin No. 44 The Petroleum Potential of H Serpentine Plugs" and Associated Rocks, Central and South Texas TRUITT F. MATTHEWS Baylor Geological Studies EDITORIAL STAFF Jean M. Spencer Jenness, M.S., Ed.ttpr environmental and medical geology CONTENTS Page O. T. Hayward, Ph.D., Advisor. Cartographic Editor Abstract .............................................................. 5 general and urban geology and what have you Introduction. .. 5 Peter M. Allen, Ph.D. Purpose ........................................................... 5 urban and environmental geology, hydrology Location .......................................................... 6 Methods .......................................................... 6 Harold H. Beaver, Ph.D. Previous works. .. 7 stratigraphy, petroleum geology Acknowledgments .................................................. 11 Regional setting of "serpentine plugs" ..................................... 11 Rena Bonem, Ph.D. Descriptive geology of "serpentine plugs" .................................. 12 paleontology, paleoecology Northern subprovince ............................................... 13 Middle subprovince ................................................. 15 William Brown, M.S. Southern subprovince ............................................... 18 structural tectonics Origin and history of "serpentine plugs" ................................... 26 Robert C. Grayson, Ph.D. Production histories of "serpentine plugs" ................................. 30 stratigraphy, conodont biostratigraphy -
CRETACEOUS-TERTIARY BOUNDARY Ijst the ROCKY MOUNTAIN REGION1
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA V o l..¿5, pp. 325-340 September 15, 1914 PROCEEDINGS OF THE PALEONTOLOGICAL SOCIETY CRETACEOUS-TERTIARY BOUNDARY IjST THE ROCKY MOUNTAIN REGION1 BY P. H . KNOWLTON (Presented before the Paleontological Society December 31, 1913) CONTENTS Page Introduction........................................................................................................... 325 Stratigraphic evidence........................................................................................ 325 Paleobotanical evidence...................................................................................... 331 Diastrophic evidence........................................................................................... 334 The European time scale.................................................................................. 335 Vertebrate evidence............................................................................................ 337 Invertebrate evidence.......................................................................................... 339 Conclusions............................................................................................................ 340 I ntroduction The thesis of this paper is as follows: It is proposed to show that the dinosaur-bearing beds known as “Ceratops beds,” “Lance Creek bieds,” Lance formation, “Hell Creek beds,” “Somber beds,” “Lower Fort Union,”- Laramie of many writers, “Upper Laramie,” Arapahoe, Denver, Dawson, and their equivalents, are above a major -
Evaluation of the Depositional Environment of the Eagle Ford
Louisiana State University LSU Digital Commons LSU Master's Theses Graduate School 2012 Evaluation of the depositional environment of the Eagle Ford Formation using well log, seismic, and core data in the Hawkville Trough, LaSalle and McMullen counties, south Texas Zachary Paul Hendershott Louisiana State University and Agricultural and Mechanical College, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_theses Part of the Earth Sciences Commons Recommended Citation Hendershott, Zachary Paul, "Evaluation of the depositional environment of the Eagle Ford Formation using well log, seismic, and core data in the Hawkville Trough, LaSalle and McMullen counties, south Texas" (2012). LSU Master's Theses. 863. https://digitalcommons.lsu.edu/gradschool_theses/863 This Thesis is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Master's Theses by an authorized graduate school editor of LSU Digital Commons. For more information, please contact [email protected]. EVALUATION OF THE DEPOSITIONAL ENVIRONMENT OF THE EAGLE FORD FORMATION USING WELL LOG, SEISMIC, AND CORE DATA IN THE HAWKVILLE TROUGH, LASALLE AND MCMULLEN COUNTIES, SOUTH TEXAS A Thesis Submitted to the Graduate Faculty of the Louisiana State University Agricultural and Mechanical College in partial fulfillment of the requirements for degree of Master of Science in The Department of Geology and Geophysics by Zachary Paul Hendershott B.S., University of the South – Sewanee, 2009 December 2012 ACKNOWLEDGEMENTS I would like to thank my committee chair and advisor, Dr. Jeffrey Nunn, for his constant guidance and support during my academic career at LSU. -
A Large Hadrosaurid Dinosaur from Presa San Antonio, Cerro Del Pueblo Formation, Coahuila, Mexico
A large hadrosaurid dinosaur from Presa San Antonio, Cerro del Pueblo Formation, Coahuila, Mexico ROGELIO ANTONIO REYNA-HERNÁNDEZ, HÉCTOR E. RIVERA-SYLVA, LUIS E. SILVA-MARTÍNEZ, and JOSÉ RUBÉN GUZMAN-GUTIÉRREZ Reyna-Hernández, R.A., Rivera-Sylva, H.E., Silva-Martínez, L.E., and Guzman-Gutiérrez, J.R. 2021. A large hadro- saurid dinosaur from Presa San Antonio, Cerro del Pueblo Formation, Coahuila, Mexico. Acta Palae onto logica Polonica 66 (Supplement to x): xxx–xxx. New hadrosaurid postcranial material is reported, collected near Presa San Antonio, Parras de la Fuente municipality, Coahuila, Mexico, in a sedimentary sequence belonging to the upper Campanian of the Cerro del Pueblo Formation, in the Parras Basin. The skeletal remains include partial elements from the pelvic girdle (left ilium, right pubis, ischium, and incomplete sacrum), a distal end of a left femur, almost complete right and left tibiae, right metatarsals II and IV, cervical and caudal vertebrae. Also, partially complete forelimb elements are present, which are still under preparation. The pubis shows characters of the Lambeosaurinae morphotypes, but the lack of cranial elements does not allow us to directly differentiate this specimen from the already described hadrosaurid taxa from the studied area, such as Velafrons coahuilensis, Latirhinus uitstlani, and Kritosaurus navajovius. This specimen, referred as Lambeosaurinae indet., adds to the fossil record of the hadrosaurids in southern Laramidia during the Campanian. Key words: Dinosauria, Hadrosauridae, Lambeosaurinae, Cretaceous, Campanian, Mexico. Rogelio Antonio Reyna-Hernández [[email protected]], Luis E. Silva-Martínez [[email protected]], Laboratorio de Paleobiología, Facultad de Ciencias Biológicas, Universidad Autónoma de Nuevo León, Av. -
Estimating the Evolutionary Rates in Mosasauroids and Plesiosaurs: Discussion of Niche Occupation in Late Cretaceous Seas
Estimating the evolutionary rates in mosasauroids and plesiosaurs: discussion of niche occupation in Late Cretaceous seas Daniel Madzia1 and Andrea Cau2 1 Department of Evolutionary Paleobiology, Institute of Paleobiology, Polish Academy of Sciences, Warsaw, Poland 2 Independent, Parma, Italy ABSTRACT Observations of temporal overlap of niche occupation among Late Cretaceous marine amniotes suggest that the rise and diversification of mosasauroid squamates might have been influenced by competition with or disappearance of some plesiosaur taxa. We discuss that hypothesis through comparisons of the rates of morphological evolution of mosasauroids throughout their evolutionary history with those inferred for contemporary plesiosaur clades. We used expanded versions of two species- level phylogenetic datasets of both these groups, updated them with stratigraphic information, and analyzed using the Bayesian inference to estimate the rates of divergence for each clade. The oscillations in evolutionary rates of the mosasauroid and plesiosaur lineages that overlapped in time and space were then used as a baseline for discussion and comparisons of traits that can affect the shape of the niche structures of aquatic amniotes, such as tooth morphologies, body size, swimming abilities, metabolism, and reproduction. Only two groups of plesiosaurs are considered to be possible niche competitors of mosasauroids: the brachauchenine pliosaurids and the polycotylid leptocleidians. However, direct evidence for interactions between mosasauroids and plesiosaurs is scarce and limited only to large mosasauroids as the Submitted 31 July 2019 predators/scavengers and polycotylids as their prey. The first mosasauroids differed Accepted 18 March 2020 from contemporary plesiosaurs in certain aspects of all discussed traits and no evidence Published 13 April 2020 suggests that early representatives of Mosasauroidea diversified after competitions with Corresponding author plesiosaurs. -
Montana Group and Equivalent Rocks, Montana, Wyoming, and North and South Dakota
GEOLOGY LIBRARY-j 2nd SETi Stratigraphy and Geologic History of the Montana Group and Equivalent Rocks, Montana, Wyoming, and North and South Dakota GEOLOGICAL SURVEY PROFESSION AL PAPER 776 INSTITUTE OF Q / NT \T AU G 27 1973 volt TECHNOLOGY metadc303 96 6 I Stratigraphy and Geologic History of the Montana Group and Equivalent Rocks, Montana, Wyoming, and North and South Dakota By J. R. GILL and W. A. COBBAN GEOLOGICAL SURVEY PROFESSIONAL PAPER 776 Stratigraphic,paleontologic, and radiometric data are N r combined to determine the paleogeography for a part of the upper Upper Cretaceous UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-600136 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 85 cents domestic postpaid or 60 cents GPO Bookstore Stock Number 2401-00342 CONTENTS Page Page Abstract ..................................................................................... 1 Geologic history of the Montana Group ................................ 20 Introduction ................................................................................ 1 Telegraph Creek--Eagle regression..................................20 Geologic setting -......................................................................................................... ........ 2 0 Amm -onitesequence --------------------------------------- Judith -
Preliminary Geologic Map of the Galena Canyon Quadrangle, Lander County, Nevada
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY To accompany the Preliminary Geologic Map of the Galena Canyon Quadrangle, Lander County, Nevada by JeffL.Doebrich1 Open-File Report 94-664 Prepared in cooperation with Santa Fe Pacific Mining Inc. under Cooperative Research and Development Agreement 9300-1-94 1994 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North America Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. !U.S. Geological Survey, Reno Field Office, MS-176, Mackay School of Mines, University of Nevada, Reno, Nevada, 89557-0047 DESCRIPTION OF MAP UNITS Qd Mine dump (Holocene) Present around active and abandoned mining operations in the Copper Canyon, Iron Canyon, an Copper Basin areas Qfp Flood plain deposits (Quaternary) Includes sand, silt, and clay deposits in the flood plain of the Reese River in the southeast corner of the quadrangle. Contacts approximately located using large-scale color aerial photographs Qaf Younger alluvium and fanglomerate deposits (Quaternary) Clay, silt, sand, and gravel primarily in active stream channels but also covering outwash fans at the mouth of major drainages emanating from the range. Contacts of outwash fans approximately located using large-scale color aerial photographs Qc Colluvium (Quaternary) Includes talus, slope wash, and other colluvial deposits Qls Landslide deposits (Quaternary) Qoa Older alluvium (Quaternary) Poorly sorted gravel deposits with a silty to sandy matrix. Includes terrace and valley-fill deposits at higher elevations; dissected by stream channels containing younger alluvium (Qaf). -
Analysis and Correlation of Growth
ANALYSIS AND CORRELATION OF GROWTH STRATA OF THE CRETACEOUS TO PALEOCENE LOWER DAWSON FORMATION: INSIGHT INTO THE TECTONO-STRATIGRAPHIC EVOLUTION OF THE COLORADO FRONT RANGE by Korey Tae Harvey A thesis submitted to the Faculty and Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date __________________________ Signed: ________________________ Korey Harvey Signed: ________________________ Dr. Jennifer Aschoff Thesis Advisor Golden, Colorado Date ___________________________ Signed: _________________________ Dr. Paul Santi Professor and Head Department of Geology and Geological Engineering ii ABSTRACT Despite numerous studies of Laramide-style (i.e., basement-cored) structures, their 4-dimensional structural evolution and relationship to adjacent sedimentary basins are not well understood. Analysis and correlation of growth strata along the eastern Colorado Front Range (CFR) help decipher the along-strike linkage of thrust structures and their affect on sediment dispersal. Growth strata, and the syntectonic unconformities within them, record the relative roles of uplift and deposition through time; when mapped along-strike, they provide insight into the location and geometry of structures through time. This paper presents an integrated structural- stratigraphic analysis and correlation of three growth-strata assemblages within the fluvial and fluvial megafan deposits of the lowermost Cretaceous to Paleocene Dawson Formation on the eastern CFR between Colorado Springs, CO and Sedalia, CO. Structural attitudes from 12 stratigraphic profiles at the three locales record dip discordances that highlight syntectonic unconformities within the growth strata packages. Eight traditional-type syntectonic unconformities were correlated along-strike of the eastern CFR distinguish six phases of uplift in the central portion of the CFR. -
The Dinosaur Park - Bearpaw Formation Transition in the Cypress Hills Region of Southwestern Saskatchewan, Canada Meagan M
The Dinosaur Park - Bearpaw Formation Transition in the Cypress Hills Region of Southwestern Saskatchewan, Canada Meagan M. Gilbert Department of Geological Sciences, University of Saskatchewan; [email protected] Summary The Upper Cretaceous Dinosaur Park Formation (DPF) is a south- and eastward-thinning fluvial to marginal marine clastic-wedge in the Western Canadian Sedimentary Basin. The DPF is overlain by the Bearpaw Formation (BF), a fully marine clastic succession representing the final major transgression of the epicontinental Western Interior Seaway (WIS) across western North America. In southwestern Saskatchewan, the DPF is comprised of marginal marine coal, carbonaceous shale, and heterolithic siltstone and sandstone grading vertically into marine sandstone and shale of the Bearpaw Formation. Due to Saskatchewan’s proximity to the paleocoastline, 5th order transgressive cycles resulted in the deposition of multiple coal seams (Lethbridge Coal Zone; LCZ) in the upper two-thirds of the DPF in the study area. The estimated total volume of coal is 48109 m3, with a gas potential of 46109 m3 (Frank, 2005). The focus of this study is to characterize the facies and facies associations of the DPF, the newly erected Manâtakâw Member, and the lower BF in the Cypress Hills region of southwestern Saskatchewan utilizing core, outcrop, and geophysical well log data. This study provides a comprehensive sequence stratigraphic overview of the DPF-BF transition in Saskatchewan and the potential for coalbed methane exploration. Introduction The Dinosaur Park and Bearpaw Formations in Alberta, and its equivalents in Montana, have been the focus of several sedimentologic and stratigraphic studies due to exceptional outcrop exposure and extensive subsurface data (e.g., McLean, 1971; Wood, 1985, 1989; Eberth and Hamblin, 1993; Tsujita, 1995; Catuneanu et al., 1997; Hamblin, 1997; Rogers et al., 2016). -
TGI Strat Column 2009.Cdr
STRATIGRAPHIC CORRELATION CHART TGI II: Williston Basin Architecture and Hydrocarbon Potential in Eastern Saskatchewan and Western Manitoba EASTERN MANITOBA PERIOD MANITOBA SUBSURFACE SASKATCHEWAN OUTCROP ERA glacial drift glacial drift glacial drift Quaternary Wood Mountain Formation Peace Garden Peace Garden Member Tertiary Member Ravenscrag Formation CENOZOIC Formation Goodlands Member Formation Goodlands Member Turtle Mountain Turtle Mountain Turtle Frenchman Formation Whitemud Formation Boissevain Formation Boissevain Formation Eastend Formation Coulter Member Coulter Member Bearpaw Formation Odanah Member Belly River “marker” Odanah Member Belly River Formation “lower” Odanah Member Millwood Member Lea Park Formation Millwood Member MONTANA GROUP Pembina Member Pembina Member Pierre Shale Pierre Shale Milk River Formation Gammon Ferruginous Member Gammon Ferruginous Member Niobrara Formation Chalky Unit Boyne Member Boyne Member Boyne Calcareous Shale Unit Member Carlile Morden Member Carlile upper Formation Morden Member Formation Morden Member Carlile Formation Assiniboine Marco Calcarenite Assiniboine Member Member CRETACEOUS Second White Specks Laurier Limestone Beds Favel Favel Keld Keld Member Member Formation Formation Belle Fourche Formation Belle Fourche Member MESOZOIC COLORADO GROUP Belle Fourche Member upper Fish Scale Formation Fish Scale Zone upper Base of Fish Scale marker Base of Fish Scale marker Westgate Formation Westgate Member lower Westgate Member Newcastle Formation Newcastle Member lower Viking Sandstone -
CD-C FEIS Chapter 3. Affected Environment
3. AFFECTED ENVIRONMENT 3.0 INTRODUCTION Chapter 3 describes the condition of the human and natural environment in the CD-C project area. Under NEPA, the human environment is the natural and physical environment and the relationship of people to that environment. The affected environment for individual resources was delineated based on the area of potential direct and indirect environmental impacts for the project and associated cumulative effects area. The environmental baseline information summarized in this chapter was obtained from the review of published sources, unpublished data, communication with government agencies, and review of field studies of the area. The level of information provided in this chapter is commensurate with the potential impacts to the resource described. PHYSICAL ENVIRONMENT 3.1 GEOLOGY 3.1.1 Physiography The project area straddles the Continental Divide and lies within the Great Divide and Washakie Basins, subsidiary basins of the Greater Green River Basin of south-central Wyoming (Map 3.1-1). Important natural landmarks in the area and their corresponding elevations are shown in Table 3.1-1. Table 3.1-1. Important natural landmarks in the CD-C project area (north to south) Landmark Location Elevation (feet) Lost Creek Butte NW ¼ Section 24, T23N:R95W 6,745 Stratton Knoll N ½ Section 28, T23N:R91W 6,879 Ruby Knolls Sections 26 and 27, T22N:R92W 7,165 Windy Hill (mesa) Sections 1–5, 7–12, and 18, T21N:R91W 7,125 Latham Point SW ¼ Section 32, T21N:R92W 7,235 Tipton Buttes NE ¼ Section 27, T20N:R96W 7,094 Cow/Horse Butte SE ¼ NE ¼ Section 5, T19N:R91W 7,170 High Point SW ¼ SW ¼ SE ¼ Section 17, T19N:R92W 7,321 Sugarloaf SE ¼ SW ¼ Section 5, T18N:R92W 7,088 Pine Butte Center of NW ¼ Section 10, T17N:R92W 6,808 Baldy Butte SW ¼ NW ¼ SW ¼ Section 12, T17N:R92W 6,920 North Flat Top SW ¼ Section 35 T15N:R93W and NW ¼ Section 2, T14N:R93W 7,822 East Flat Top Center of the E ½ Section 18, T14N:R92W 7,560 Continental Divide-Creston Natural Gas Development Project Final EIS April 2016 3-1 CHAPTER 3—AFFECTED ENVIRONMENT—GEOLOGY Map 3.1-1.