Index to the Geologic Names of North America
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Stratigraphy of the Tuerto and Ancha Formations (Upper Santa Fe Group), Hagan and Santa Fe Embayments, North-Central New Mexico
NMBMMR 454B STRATIGRAPHY OF THE TUERTO AND ANCHA FORMATIONS (UPPER SANTA FE GROUP), HAGAN AND SANTA FE EMBAYMENTS, NORTH-CENTRAL NEW MEXICO DANIEL J. KONING 14193 Henderson Dr., Rancho Cucamonga, CA 91739 SEAN D. CONNELL N.M. Bureau of Mines and Mineral Resources-Albuquerque Office, New Mexico Institute of Mining and Technology, 2808 Central Ave., SE, Albuquerque, NM 87106 FRANK J. PAZZAGLIA Lehigh University, Department of Earth and Environmental Sciences, 31 Williams Dr., Bethlehem, PA 18015 WILLIAM C. MCINTOSH New Mexico Bureau of Mines and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM 87801 INTRODUCTION which we correlate to most of their type section. The upper quarter of their type Ancha section contains Geologic studies and 40Ar/39Ar dating of basalt flows and basaltic tephra of the Cerros del Rio subhorizontally bedded strata of the upper Santa Fe volcanic field, which was emplaced between 2.8 and Group in the vicinity of the Santa Fe and Hagan 1.4 Ma (David Sawyer, personal commun., 2001), embayments (Fig. 1) indicate that revision of the with the most voluminous activity occurring between Ancha and Tuerto formations are necessary. The 2.3-2.8 Ma (Woldegabriel et al., 1996; Bachman and Ancha and Tuerto formations are included in the Mehnert, 1978; Sawyer et al., 2001). Beneath the youngest strata of the Santa Fe Group, as defined by upper volcanic flows and volcaniclastics is 12-17(?) Spiegel and Baldwin (1963), and consist of broad, m of strata, containing 1-5% quartzite clasts, that is thin alluvial aprons of Plio-Pleistocene age derived similar to a Pliocene deposit (unit Ta) mapped by from local uplands along the eastern margins of the Dethier (1997) that interfingers with Pliocene basalt Albuquerque and Española basins, Rio Grande rift, tephra of the Cerros del Rio volcanic field. -
1 Paleobotanical Proxies for Early Eocene Climates and Ecosystems in Northern North 2 America from Mid to High Latitudes 3 4 Christopher K
https://doi.org/10.5194/cp-2020-32 Preprint. Discussion started: 24 March 2020 c Author(s) 2020. CC BY 4.0 License. 1 Paleobotanical proxies for early Eocene climates and ecosystems in northern North 2 America from mid to high latitudes 3 4 Christopher K. West1, David R. Greenwood2, Tammo Reichgelt3, Alexander J. Lowe4, Janelle M. 5 Vachon2, and James F. Basinger1. 6 1 Dept. of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, 7 Saskatchewan, S7N 5E2, Canada. 8 2 Dept. of Biology, Brandon University, 270-18th Street, Brandon, Manitoba R7A 6A9, Canada. 9 3 Department of Geosciences, University of Connecticut, Beach Hall, 354 Mansfield Rd #207, 10 Storrs, CT 06269, U.S.A. 11 4 Dept. of Biology, University of Washington, Seattle, WA 98195-1800, U.S.A. 12 13 Correspondence to: C.K West ([email protected]) 14 15 Abstract. Early Eocene climates were globally warm, with ice-free conditions at both poles. Early 16 Eocene polar landmasses supported extensive forest ecosystems of a primarily temperate biota, 17 but also with abundant thermophilic elements such as crocodilians, and mesothermic taxodioid 18 conifers and angiosperms. The globally warm early Eocene was punctuated by geologically brief 19 hyperthermals such as the Paleocene-Eocene Thermal Maximum (PETM), culminating in the 20 Early Eocene Climatic Optimum (EECO), during which the range of thermophilic plants such as 21 palms extended into the Arctic. Climate models have struggled to reproduce early Eocene Arctic 22 warm winters and high precipitation, with models invoking a variety of mechanisms, from 23 atmospheric CO2 levels that are unsupported by proxy evidence, to the role of an enhanced 24 hydrological cycle to reproduce winters that experienced no direct solar energy input yet remained 25 wet and above freezing. -
Bull. Geol. Soc. Am. Vol. 46, 1935, Pl. 33
BULL. GEOL. SOC. AM. VOL. 46, 1935, PL. 33 F ig u r e 2. E a stern F a ce o f t h e Q uarry DUNDEE-ANDERDON CONTACT IN SIBLEY QUARRY Downloaded from http://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/46/3/425/3415212/BUL46_3-0425.pdf by guest on 01 October 2021 BULLETIN OF THE GEOLOGICAL SOCIETY CfF A M E R IC A VOL. 46, PP. 428-462, PLS. 33-39, 1 FIG. MARCH 31. 1935 PROCEEDINGS OF THE PALEONTOLOGICAL SOCIETY STRATIGRAPHY AND PALEONTOLOGY OF THE DUNDEE LIMESTONE OF SOUTHEASTERN MICHIGAN* BY CHARLES FERNANDO BASSETT (Presented before the Paleontological Society, December SO, 193S) CONTENTS Page Introduction............................................................................................................. 425 Statement of the problem................................................................................ 425 Acknowledgments............................................................................................. 427 Stratigraphy of the Dundee limestone................................................................... 427 Distribution....................................................................................................... 427 Previous classification...................................................................................... 427 Description of sections..................................................................................... 428 Sibley quarry............................................................................................. 428 Christiancy or Macon quarry................................................................. -
OGS 1962 RI-42.Pdf
·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·i i STATE CE OHIO • MICHAEL V. DISALLI, eo-- DD'AU'MEHT CE NATIJl\AL llES<XmCES Ilo IElllEl\T a, EAGON, Dlncllor In'ISION OF GEOLOGICAL SURVEY l\AJ.PH J. KIUIHACEN, Chief Ii I• lo I REPORT OF INVESTIGATIONS NO. 42 LOWER AND MIDDLE DEVONIAN LIMESTONES IN NORTHEASTERN OHIO • I • AND ADJACENT AREAS I i• I ~ ~ By i John W. Dow i II • I • I • I I • i I . • I I COLUMBUS ~ . 1962 I I • • I• I I • • I I ~-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-· STATE OF OHIO Michael V. DiSalle Governor DEPARTMENT OF NATURAL RESOURCES Herbert B. Eagon Director NATURAL RESOURCES COMMISSION Herbert B. Eagon Lawrence Kimble Byron Frederick Roy M. Kottman Forrest G. Hall Demas L. Sears William Hoyne Myron T.· Sturgeon Joseph E. Hurst DIVISION OF GEOLOGICAL SURVEY Ralph J. Bernhagen Chief The F . J . Heer Printing Company Columbus 16, Ohio 1962 Bound by the State of Ohio ;-·-·-·-·-·-·-·-·-·-~-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·i i• i I ~Of~ I• 0 MICHAEL V. DI SALLE, Governor lo DEPAR1MENT Of NATURAL RESOURCES I HERBERT II. EAGON, Director I DIVISION OF GEOLOGICAL SURVEY RALPH J. BERNHAGEN, Chief • I • I.. I REPORT OF INVESTIGATIONS NO. 42 i i;. ! .I .I I LOWER AND MIDDLE DEVONIAN LIMESTONES . IN NORTHEASTERN OHIO I • AND ADJACENT AREAS .I I• I.. I By i• John W. Dow I ! ! ! I • I • I • .I .I .I I I COLUMBUS • . 1962 I I • . I.. I For sale l::ry Ohio Division of Geological Survey, Columbus, Ohio I • Price 97 cents plus 3 cents tax in Ohio • I ~ ...... _...... ··-.- .- ·-.- .- .- .- .- .- .- .- .- .- .- ._,,. -.- .- .- .- .- .- . BLANK PAGE CONTENTS Page Introduction. 1 Purpose of study 1 Previous studies 1 Methods of investigation. -
Abstracts of REU Student Reports (SAGE 2012)
Abstracts of REU Student Reports (SAGE 2012): Evaluating Galvanic Distortion: A Comparison of Phase Tensors and Polar Diagrams Diana Brown Abstract: Galvanic distortions result from conductivity gradients. This is a fundamental concept in magnetotellurics (MT). However, distortions from shallow, small-scale heterogeneities can lead to statically shifted data. MT sites taken from a geophysical study of the Caja del Rio region of New Mexico, were analyzed for the presence of galvanic distortion. Utilizing phase tensors and polar diagrams, a comparative study was completed. Comparing the dimensionality represented by polar diagrams to that of phase tensors provides a qualitative indicator of distortion. Sites with opposing dimensionalities were those with statically shifted data. Conversely, sites with diagrams in agreement were distortion free. 1D inversion models were run from both pre and post static shift corrected sounding curves. This direct comparison of inversions illustrates how distortions can be manifested in a geologic model. Seismic Reflection: Velocity Analysis using Constant Velocity Stacks Emily Butler Abstract: The Caja del Rio area is characterized with volcanics near the surface. The goal of the seismic reflection line is to be able to determine the depth and thickness of the volcanics as well as any other significant formations. Specifically, applying an appropriate velocity analysis is key in determining the correct reflectors and reflector depth. The goal of velocity analysis using constant velocity stacks is to flatten out as many reflectors as possible by applying the correct velocity function in order to produce a stack that can be interpreted. Velocity analysis using constant velocity stacking involves developing many stacks, all with different constant velocities and determining where each reflector flattens out and at which velocity. -
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. -
Physiographic Subdivisions of the San Luis Valley, Southern Colorado
113 PHYSIOGRAPHIC SUBDIVISIONS OF THE SAN LUIS VALLEY, SOUTHERN COLORADO by J. E. UPsolvf University of Idaho Moscow, Idaho EDITOR'S NOTE: The New Mexico Geological Society v is grateful to the Journal of Geology for permission to re- print this classic article. After 32 years the work still re- WVO. • mains the most quoted reference in its field on the basin. AP.. _ AC . I The photographs were retaken under Mr. Upson's direc- / tion and duplicate the originals as closely as possible, with –rt 1 the exception of Figure 5, which was taken a short distance ,0 "north" of the mouth of the Rio Costilla. Slight editorial /y .R changes in punctuation and capitalization were made on p 3, the article to conform to present day usage. Denver 70 0 0) INTRODUCTION 3 , CID The San Luis Valley, forming the upper end of the u) great valley of the Rio Grande, is one of the most impres- sive topographic features of southern Colorado. As orig- inally outlined by Siebenthal, 1 it is a great lowland about 150 miles long and 50 miles in maximum width, flanked on the east by the linear Sangre dc Cristo Range and on 0 7/, / the west by the eastern portion of the more extensive San 3 0 0N405 Juan Mountains. It is, in a sense, part of the chain of in- t4 •O 4. SP O V4 / termontane basins, or parks,2 lying west of the Southern ` 1,1‘0 AN Rocky Mountain front ranges, but is unlike the others in Llt IS q` having no southern mountain border. -
UNIVERSITY of CALIFORNIA RIVERSIDE a New
UNIVERSITY OF CALIFORNIA RIVERSIDE A New Species of an Enigmatic Fossil Taxon: Ischadites n. sp., a Middle Ordovician Receptaculitid From the Great Basin, Western USA A Thesis submitted in partial satisfaction of the requirements for the degree of Master of Science in Geological Sciences by Sara E Henry June 2014 Thesis Committee: Dr. Mary L. Droser, Chairperson Dr. Nigel C. Hughes Dr. Richard Minnich Copyright by Sara E Henry 2014 The Thesis of Sara E Henry is approved: Committee Chairperson University of California, Riverside ACKNOWLEDGEMENTS First and foremost, I would like to express my sincere gratitude to my advisor, Dr. Mary L. Droser, for her continuous support throughout my graduate studies, field work, and research. I’d additionally like to thank the rest of my committee: Dr. Nigel C. Hughes and Dr. Richard Minnich for their encouragement, insight, and guidance. Dr. Ganqing Jiang of the University of Nevada, Las Vegas, assisted with stratigraphic measurements and provided valuable consultation on sedimentological interpretation in the field. Illustrations of Ischadites n. sp. were produced by my very talented brother, Mr. Keith R. Henry. Several field assistants allowed for large bulk sampling of fossils over multiple field work excursions: T. Beck, M. Nonu, R. Theroux, and J. Minor. Special thanks to L. Graham and T. Beck for lab work assistance. Field work required for this project was funded by the Geological Society of America, the Society for Sedimentary Geology, and the Gulf Coast Section of the Society for Sedimentary Geology. Lastly, I have to thank my parents, Kim and Susan Henry, for their unwavering support, patience, and encouragement. -
Universidad Autónoma De Nuevo León Facultad De Ciencias De La Tierra
UNIVERSIDAD AUTÓNOMA DE NUEVO LEÓN FACULTAD DE CIENCIAS DE LA TIERRA "ANÁLISIS DE MICROFACIES Y PALEOICTIOLOGÍA DE LA FORMACIÓN AGUA NUEVA (CRETÁCICO SUPERIOR) EN LA SIERRA DE SAN CARLOS, TAMAULIPAS, MÉXICO" TESIS QUE COMO REQUISITO PARCIAL PARA OBTENER EL GRADO DE MAESTRO EN CIENCIAS GEOLÓGICAS PRESENTA: LAURA ALEJANDRA SANTANA SALAS LINARES, NUEVO LEÓN JUNIO 2012 UNIVERSIDAD AUTÓNOMA DE NUEVO LEÓN FACULTAD DE CIENCIAS DE LA TIERRA HDA. DE GUADALUPE, CARR. A CERRO PRIETO KM 8, A.P. 104 67700 LINARES, NUEVO LEÓN, MÉXICO TELS. Y FAX (821) 214 20 10, 214 20 20 Y 214 20 30 “ANÁLISIS DE MICROFACIES Y PALEOICTIOLOGÍA DE LA FORMACIÓN AGUA NUEVA (CRETÁCICO SUPERIOR) EN LA SIERRA DE SAN CARLOS, TAMAULIPAS, MÉXICO” PRESENTA: LAURA ALEJANDRA SANTANA SALAS HA SIDO ACEPTADA COMO REQUISITO PARCIAL PARA OBTENER EL GRADO DE: MAESTRO EN CIENCIAS GEOLÓGICAS Vo. Bo. DIRECTOR DE TESIS ___________________________________ Dr. José Guadalupe López Oliva LINARES, NUEVO LEÓN JUNIO 2012 UNIVERSIDAD AUTÓNOMA DE NUEVO LEÓN FACULTAD DE CIENCIAS DE LA TIERRA HDA. DE GUADALUPE, CARR. A CERRO PRIETO KM 8, A.P. 104 67700 LINARES, NUEVO LEÓN, MÉXICO TELS. Y FAX (821) 214 20 10, 214 20 20 Y 214 20 30 “ANÁLISIS DE MICROFACIES Y PALEOICTIOLOGÍA DE LA FORMACIÓN AGUA NUEVA (CRETÁCICO SUPERIOR) EN LA SIERRA DE SAN CARLOS, TAMAULIPAS, MÉXICO” PRESENTA: LAURA ALEJANDRA SANTANA SALAS HA SIDO ACEPTADA COMO REQUISITO PARCIAL PARA OBTENER EL GRADO DE: MAESTRO EN CIENCIAS GEOLÓGICAS COMITÉ DE REVISIÓN Vo. Bo. ___________________________________ Dr. José Guadalupe López Oliva Director de Tesis ____________________________ ________________________ Dr. Juan Alonso Ramírez Fernández M. C. Andres Ramos Ledezma Co-Director de Tesis Co-Director de Tesis ______________________________ Dra. -
La Brea and Beyond: the Paleontology of Asphalt-Preserved Biotas
La Brea and Beyond: The Paleontology of Asphalt-Preserved Biotas Edited by John M. Harris Natural History Museum of Los Angeles County Science Series 42 September 15, 2015 Cover Illustration: Pit 91 in 1915 An asphaltic bone mass in Pit 91 was discovered and exposed by the Los Angeles County Museum of History, Science and Art in the summer of 1915. The Los Angeles County Museum of Natural History resumed excavation at this site in 1969. Retrieval of the “microfossils” from the asphaltic matrix has yielded a wealth of insect, mollusk, and plant remains, more than doubling the number of species recovered by earlier excavations. Today, the current excavation site is 900 square feet in extent, yielding fossils that range in age from about 15,000 to about 42,000 radiocarbon years. Natural History Museum of Los Angeles County Archives, RLB 347. LA BREA AND BEYOND: THE PALEONTOLOGY OF ASPHALT-PRESERVED BIOTAS Edited By John M. Harris NO. 42 SCIENCE SERIES NATURAL HISTORY MUSEUM OF LOS ANGELES COUNTY SCIENTIFIC PUBLICATIONS COMMITTEE Luis M. Chiappe, Vice President for Research and Collections John M. Harris, Committee Chairman Joel W. Martin Gregory Pauly Christine Thacker Xiaoming Wang K. Victoria Brown, Managing Editor Go Online to www.nhm.org/scholarlypublications for open access to volumes of Science Series and Contributions in Science. Natural History Museum of Los Angeles County Los Angeles, California 90007 ISSN 1-891276-27-1 Published on September 15, 2015 Printed at Allen Press, Inc., Lawrence, Kansas PREFACE Rancho La Brea was a Mexican land grant Basin during the Late Pleistocene—sagebrush located to the west of El Pueblo de Nuestra scrub dotted with groves of oak and juniper with Sen˜ora la Reina de los A´ ngeles del Rı´ode riparian woodland along the major stream courses Porciu´ncula, now better known as downtown and with chaparral vegetation on the surrounding Los Angeles. -
Reservoir Geology of the Dundee Limestone, West Branch Field, Michigan
Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 12-1990 Reservoir Geology of the Dundee Limestone, West Branch Field, Michigan Brendan Ciaran Curran Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Curran, Brendan Ciaran, "Reservoir Geology of the Dundee Limestone, West Branch Field, Michigan" (1990). Master's Theses. 1053. https://scholarworks.wmich.edu/masters_theses/1053 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. RESERVOIR GEOLOGY OF THE DUNDEE LIMESTONE, WEST BRANCH FIELD, MICHIGAN by Brendan Ciaran Curran A Thesis Submitted to the Faculty of The Graduate College in partial fulfillment of the requirements for the Degree of Master of Science Department of Geology Western Michigan University Kalamazoo, Michigan December 1990 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. RESERVOIR GEOLOGY OF THE DUNDEE LIMESTONE, WEST BRANCH FIELD, MICHIGAN Brendan Ciaran Curran, M.S. W estern Michigan University, 1990 West Branch field is a low-relief, NW-SE-trending anticline near the center of the Michigan basin. Since 1934, the Dundee Limestone (Middle Devonian) has produced over 12 million barrels of oil from this field. From core studies, six depositional facies types were recognized in the Dundee. These are dominated by bioclastic carbonate sand facies deposited in normal- marine shelf settings. Although burial cements have occluded some porosity, carbonate sand facies have retained significant primary interparticle porosity and are the most important reservoir rocks. -
Detroit River Group in the Michigan Basin
GEOLOGICAL SURVEY CIRCULAR 133 September 1951 DETROIT RIVER GROUP IN THE MICHIGAN BASIN By Kenneth K. Landes UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Washington, D. C. Free on application to the Geological Survey, Washington 25, D. C. CONTENTS Page Page Introduction............................ ^ Amherstburg formation................. 7 Nomenclature of the Detroit River Structural geology...................... 14 group................................ i Geologic history ....................... ^4 Detroit River group..................... 3 Economic geology...................... 19 Lucas formation....................... 3 Reference cited........................ 21 ILLUSTRATIONS Figure 1. Location of wells and cross sections used in the study .......................... ii 2. Correlation chart . ..................................... 2 3. Cross sections A-«kf to 3-G1 inclusive . ......................;.............. 4 4. Facies map of basal part of Dundee formation. ................................. 5 5. Aggregate thickness of salt beds in the Lucas formation. ........................ 8 6. Thickness map of Lucas formation. ........................................... 10 7. Thickness map of Amherstburg formation (including Sylvania sandstone member. 11 8. Lime stone/dolomite facies map of Amherstburg formation ...................... 13 9. Thickness of Sylvania sandstone member of Amherstburg formation.............. 15 10. Boundary of the Bois Blanc formation in southwestern Michigan.