Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1973
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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. -
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Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Graduate School of Arts and Sciences COLUMBIA UNIVERSITY 2016 © 2015 Kaori Tsukui All rights reserved ABSTRACT Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui The age of the Bridgerian/Uintan boundary has been regarded as one of the most important outstanding problems in North American Land Mammal “Age” (NALMA) biochronology. The Bridger Basin in southwestern Wyoming preserves one of the best stratigraphic records of the faunal boundary as well as the preceding Bridgerian NALMA. In this dissertation, I first developed a chronological framework for the Eocene Bridger Formation including the age of the boundary, based on a combination of magnetostratigraphy and U-Pb ID-TIMS geochronology. Within the temporal framework, I attempted at making a regional correlation of the boundary-bearing strata within the western U.S., and also assessed the body size evolution of three representative taxa from the Bridger Basin within the context of Early Eocene Climatic Optimum. Integrating radioisotopic, magnetostratigraphic and astronomical data from the early to middle Eocene, I reviewed various calibration models for the Geological Time Scale and intercalibration of 40Ar/39Ar data among laboratories and against U-Pb data, toward the community goal of achieving a high precision and well integrated Geological Time Scale. In Chapter 2, I present a magnetostratigraphy and U-Pb zircon geochronology of the Bridger Formation from the Bridger Basin in southwestern Wyoming. -
DOGAMI Open-File Report O-16-06
Metallic and Industrial Mineral Resource Potential of Southern and Eastern Oregon: Report to the Oregon Legislature APPENDIX B: RELEVANT PUBLISHED MINERAL INVENTORIES AND STUDIES PREVIOUSLY COMPLETED BY DOGAMI This list includes relevant published DOGAMI mineral inventories and studies. It is not a complete publication list. For all DOGAMI publications, visit the DOGAMI Publications Center, Links here will take readers to PDF or .zip formatted files or to web pages. Bulletins B-003 1938 The geology of part of the Wallowa Moun- B-016 1940 Field identification of minerals for Oregon tains, by C. P. Ross. prospectors and collectors, by Ray C. B-004 1938 Quicksilver in Oregon, by C. N. Schuette. Treasher. B-005 1938 Geological report on part of the Clarno Ba- B-017 1942 Manganese in Oregon, by F. W. Libbey, John sin, Wheeler and Wasco Counties, Oregon, Eliot Allen, Ray C. Treasher, and H. K. Lancas- by Donald K. Mackay. ter. B-006 1938 Preliminary report of some of the refractory B-019 1939 Dredging of farmland in Oregon, by F. W. Lib- clays of western Oregon, by Hewitt Wilson bey. and Ray C. Treasher. B-020 1940 Analyses and other properties of Oregon B-007 1938 The gem minerals of Oregon, by Dr. H. C. coals as related to their utilization, by H.F. Dake. Yancey and M. R. Geer. B-008 1938 An investigation of the feasibility of a steel B-023 1942 An investigation of the reported occurrence plant in the Lower Columbia River area near of tin at Juniper Ridge, Oregon, by H. -
Tectonic Features of the Precambrian Belt Basin and Their Influence on Post-Belt Structures
... Tectonic Features of the .., Precambrian Belt Basin and Their Influence on Post-Belt Structures GEOLOGICAL SURVEY PROFESSIONAL PAPER 866 · Tectonic Features of the · Precambrian Belt Basin and Their Influence on Post-Belt Structures By JACK E. HARRISON, ALLAN B. GRIGGS, and JOHN D. WELLS GEOLOGICAL SURVEY PROFESSIONAL PAPER X66 U N IT ED STATES G 0 V ERN M EN T P R I NT I N G 0 F F I C E, \VAS H I N G T 0 N 19 7 4 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 74-600111 ) For sale by the Superintendent of Documents, U.S. GO\·ernment Printing Office 'Vashington, D.C. 20402 - Price 65 cents (paper cO\·er) Stock Number 2401-02554 CONTENTS Page Page Abstract................................................. 1 Phanerozoic events-Continued Introduction . 1 Late Mesozoic through early Tertiary-Continued Genesis and filling of the Belt basin . 1 Idaho batholith ................................. 7 Is the Belt basin an aulacogen? . 5 Boulder batholith ............................... 8 Precambrian Z events . 5 Northern Montana disturbed belt ................. 8 Phanerozoic events . 5 Tectonics along the Lewis and Clark line .............. 9 Paleozoic through early Mesozoic . 6 Late Cenozoic block faults ........................... 13 Late Mesozoic through early Tertiary . 6 Conclusions ............................................. 13 Kootenay arc and mobile belt . 6 References cited ......................................... 14 ILLUSTRATIONS Page FIGURES 1-4. Maps: 1. Principal basins of sedimentation along the U.S.-Canadian Cordillera during Precambrian Y time (1,600-800 m.y. ago) ............................................................................................... 2 2. Principal tectonic elements of the Belt basin reentrant as inferred from the sedimentation record ............ -
Sequence Stratigraphy of the Neoproterozoic Infra Krol Formation and Krol Group, Lesser Himalaya, India
SEQUENCE STRATIGRAPHY OF THE NEOPROTEROZOIC INFRA KROL FORMATION AND KROL GROUP, LESSER HIMALAYA, INDIA GANQING JIANG1, NICHOLAS CHRISTIE-BLICK1, ALAN J. KAUFMAN2, DHIRAJ M. BANERJEE3, AND VIBHUTI RAI4 1 Department of Earth and Environmental Sciences and Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964±8000, U.S.A. 2 Department of Geology, University of Maryland, College Park, Maryland 20742±4211, U.S.A. 3 Department of Geology, University of Delhi, Delhi 110007, India 4 Department of Geology, Lucknow University, Lucknow 226007, India e-mail: [email protected] ABSTRACT: A sequence stratigraphic study of terrigenous and carbonate rocks GEOLOGICAL FRAMEWORK of the Infra Krol Formation and Krol Group in the Lesser Himalaya fold and thrust belt of northern India was undertaken as part of a broader investigation The Infra Krol Formation and Krol Group are part of a Neoproterozoic and Lower of the signi®cance of carbon isotope data in Neoproterozoic successions. Eight Cambrian succession more than 12 km thick, cropping out in the Lesser Himalaya regional stratigraphic discontinuities were traced over a distance of nearly 300 in a series of doubly plunging synclines between Solan in the northwest and Nainital, km, and interpretations were anchored in a series of local studies involving the 280 km to the southeast (Fig. 1; Bhargava 1979; Shanker et al. 1989; Shanker et mapping of key beds and the measurement of closely spaced sections. Three of al. 1993; Shanker et al. 1997; Shanker and Mathur 1992). -
Oregon Geology
ORECiON CiEOLOCiY published by the Oregon Department of Geology and Mineral Industries VOLUME 44 , NUMBER 5 MAY 1982 OREGON GEOLOGY OIL AND GAS NEWS (ISSN 0164-3304) Columbia County: Reichhold Energy Corporation continues to carry out ex VOLUME 44, NUMBER 5 MAY 1982 ploratory drilling in Columbia County, most recently spudding Crown Zellerbach 32-26 about 11 mi southeast of production Published monthly by the State of Oregon Department of Geology and Mineral Industries (Volumes 1 through 40 were en at the Mist Field. This well, projected for 6,500 ft, is located in titled The Ore Bin). sec. 26, T. 5 N., R. 4 W. The company also anticipates redrilling two existing wells at Mist: Columbia County 4 and 13-1. Governing Board C. Stanley Rasmussen . .. Baker Douglas County: Allen P. Stinchfield ........................ North Bend Florida Exploration Company of Houston has begun Donald A. Haagensen ....................... " Portland drilling northwest of Roseburg in Douglas County. A Mont State Geologist. .. Donald A. Hull gomery rig from California spudded the well, Florida Explora tion Company 1-4, on April 6 and is drilling toward a pro Deputy State Geologist ..................... John D. Beaulieu posed depth of 10,000 ft. The well is in sec. 4, T. 21 S., R. 6 W. The operator has also applied to drill a second well in Editor ................................... Beverly F. Vogt Douglas County (see table below). Main Office: 1005 State Office Building, Portland 97201, phone Malheur County: (503) 229-5580. It has been over 20 years since an oil and gas well has been drilled in northern Malheur County, although several of the Baker Field Office: 2033 First Street, Baker 97814, phone (503) earlier wells had shows of gas. -
Introduction to Greater Green River Basin Geology, Physiography, and History of Investigations
Introduction to Greater Green River Basin Geology, Physiography, and History of Investigations U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1506-A Introduction to Greater Green River Basin Geology, Physiography, and History of Investigations By HENRY W. ROEHLER GEOLOGY OF THE EOCENE WASATCH, GREEN RIVER, AND BRIDGER (WASHAKIE) FORMATIONS, GREATER GREEN RIVER BASIN, WYOMING, UTAH, AND COLORADO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1506-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1992 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging in Publication Data Roehler, Henry W. Introduction to greater Green River basin geology, physiography, and history of investigations / by Henry W. Roehler. p. cm. (Geology of the Eocene Wasatch, Green River, and Bridger (Washakie) formations, greater Green River basin, Wyoming, Utah, and Colorado) (U.S. Geological Survey professional paper ; 1506-A) Includes bibliographical references (p. ). Supt. of Docs, no.: I 19.16:1506A 1. Geology, Stratigraphic Eocene. 2. Geology Green River Watershed (Wyo.-Utah). I. Title. II. Series. III. Series: U.S. Geological Survey professional paper ; 1506-A. QE692.2.R625 1992 551.7'84'097925 dc20 91-23181 CIP For sale by Book and Open-File Report Sales, U.S. Geological Survey, Federal Center, Box 25286, Denver, CO 80225 CONTENTS Page Abstract ........................................................................................................................................ Al Purpose and scope of investigation ............................................................................................ 1 Location and accessibility of the greater Green River basin ................................................... 2 Geologic setting ........................................................................................................................... -
Eocene Green River Formation, Western United States
Synoptic reconstruction of a major ancient lake system: Eocene Green River Formation, western United States M. Elliot Smith* Alan R. Carroll Brad S. Singer Department of Geology and Geophysics, University of Wisconsin, 1215 West Dayton Street, Madison, Wisconsin 53706, USA ABSTRACT Members. Sediment accumulation patterns than being confi ned to a single episode of arid thus refl ect basin-center–focused accumula- climate. Evaporative terminal sinks were Numerous 40Ar/39Ar experiments on sani- tion rates when the basin was underfi lled, initially located in the Greater Green River dine and biotite from 22 ash beds and 3 and supply-limited accumulation when the and Piceance Creek Basins (51.3–48.9 Ma), volcaniclastic sand beds from the Greater basin was balanced fi lled to overfi lled. Sedi- then gradually migrated southward to the Green River, Piceance Creek, and Uinta ment accumulation in the Uinta Basin, at Uinta Basin (47.1–45.2 Ma). This history is Basins of Wyoming, Colorado, and Utah Indian Canyon, Utah, was relatively con- likely related to progressive southward con- constrain ~8 m.y. of the Eocene Epoch. Mul- stant at ~150 mm/k.y. during deposition of struction of the Absaroka Volcanic Prov- tiple analyses were conducted per sample over 5 m.y. of both evaporative and fl uctuat- ince, which constituted a major topographic using laser fusion and incremental heating ing profundal facies, which likely refl ects the and thermal anomaly that contributed to a techniques to differentiate inheritance, 40Ar basin-margin position of the measured sec- regional north to south hydrologic gradient. loss, and 39Ar recoil. -
American Journal of Science, Vol
[American Journal of Science, Vol. 318, February, 2018, P. 167–207, DOI 10.2475/02.2018.1] American Journal of Science FEBRUARY 2018 ONE DIAMICTITE AND TWO RIFTS: STRATIGRAPHY AND GEOCHRONOLOGY OF THE GATAGA MOUNTAIN OF NORTHERN BRITISH COLUMBIA ATHENA EYSTER*,§,†, FILIPPO FERRI**, MARK D. SCHMITZ***, and FRANCIS A. MACDONALD* ABSTRACT. Neoproterozoic glacial diamictites and rift-related volcanics are pre- served throughout the North American Cordillera, yet the nature and timing of both glaciation and rifting are poorly constrained. New geochronological, geochemical, and stratigraphic data from the Cryogenian Gataga volcanics and bounding units at Gataga Mountain, in the Kechika Trough of northern British Columbia, better constrain the age of these rift-related volcanics and suggest that they erupted during glaciation. At Gataga Mountain, three informal sequences are exposed; a basal quartzite, the Gataga volcanics, and an overlying mixed carbonate-siliciclastic succession. The basal quartz- ite is dominated by cross-bedded sandstone with an intertidal facies assemblage including bidirectional cross-stratification and mud-cracks, indicative of non-glacial deposition. The overlying Gataga volcanics are over one kilometer thick, comprising both mafic and felsic units, with volcaniclastic breccia and interbedded sedimentary units including iron formation and matrix-supported diamictite with exotic clasts. Magmatic ages in the upper Gataga volcanics span 696.2 ؎ 0.2 to 690.1 ؎ 0.2 Ma, and detrital zircon from the underlying non-glacial quartzite provide a maximum age constraint on the onset of glaciation <735.8 ؎ 0.6 Ma. We interpret interfingering beds of matrix-supported diamictite with exotic clasts within the Gataga volcanics to record sub-ice shelf sedimentation and volcanism during the Sturtian Glaciation. -
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 -
3.12 Paleontological Resources
3.12 PALEONTOLOGICAL RESOURCES 3.12 PALEONTOLOGICAL RESOURCES 3.12.1 Definitions Paleontological resources—or fossils—are the remains of ancient plants and animals that can provide scientifically significant information about the history of life on earth. Paleontological “sensitivity” is defined as the potential for a geologic unit to produce scientifically significant fossils. This sensitivity is determined by rock type, history of the geologic unit in producing significant fossils, and fossil localities that are recorded from that unit. Paleontological sensitivity is assigned based on fossil data collected from the entire geologic unit, not just at a specific site. Paleontological sensitivity ratings are described as follows: High Sensitivity. Indicates fossils are currently observed on site, localities are recorded within the study area, and/or the unit has a history of producing numerous significant fossil remains. Moderate Sensitivity. Fossils within the unit are generally not unique, or are so poorly preserved as to have only moderate scientific significance. Low Sensitivity. Indicates significant fossils are not likely to be found because of a random fossil distribution pattern, extreme youth of the rock unit, and/or the method of rock formation, such as alteration by heat and pressure. Marginal Sensitivity. Indicates the limited probability of the geologic unit composed of either pyroclastic or metasedimentary rocks conducive to the existence and/or preservation of fossils. Zero Sensitivity. Origin of the geologic unit renders it not conducive to the existence of organisms and/or preservation of fossils, such as high‐grade metamorphic rocks, intrusive igneous rocks, and most volcanic rocks. Indeterminate Sensitivity. Unknown or undetermined sensitivity indicates that the geologic unit has not been sufficiently studied, or lacks good exposures to warrant a definitive rating. -
Occurrence of Torvoneustes (Crocodylomorpha, Metriorhynchidae) in Marine Jurassic Deposits of Oaxaca, Mexico
Rev. bras. paleontol. 19(3):415-424, Setembro/Dezembro 2016 © 2016 by the Sociedade Brasileira de Paleontologia doi: 10.4072/rbp.2016.3.07 OCCURRENCE OF TORVONEUSTES (CROCODYLOMORPHA, METRIORHYNCHIDAE) IN MARINE JURASSIC DEPOSITS OF OAXACA, MEXICO JAIR I. BARRIENTOS-LARA Posgrado en Ciencias Biológicas, Instituto de Geología, Universidad Nacional Autónoma de México, Circuito de la Investigación S/N, Ciudad Universitaria, Delegación Coyoacán, Distrito Federal, 04510, México. [email protected] YANINA HERRERA, MARTA S. FERNÁNDEZ División Paleontología Vertebrados, Unidades de Investigación Anexo Museo, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Av. 60 y 122, B1900AVW, La Plata, Argentina. [email protected], [email protected] JESÚS ALVARADO-ORTEGA Instituto de Geología, Universidad Nacional Autónoma de México, Circuito de la Investigación s/n, Ciudad Universitaria, Delegación Coyoacán, Distrito Federal, 04510, México. [email protected] ABSTRACT – IGM 9026 is a singular fossil collected at the beginning of the 20th century in an improperly documented site within the Tlaxiaco Basin, near to Tlaxiaco town, Oaxaca, Mexico. The age of the site was suggested as being early Cretaceous. This specimen is the holotype of Plesiosaurus (Polypticodon) mexicanus, which later was identified as a possible late Jurassic marine crocodylomorph of the family Metriorhynchidae, and consequently it was referred as ?Cricosaurus mexicanus. The present study provides a re-description of this fossil based on a microscopic analysis and the use of white and UV lights; these analyses led to the discovery of peculiar dental characters diagnostic of the genus Torvoneustes. This finding supports the re-classification of IGM 9026 under a new nominal combination asTorvoneustes mexicanus.