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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. -
Cambrian Ordovician
Open File Report LXXVI the shale is also variously colored. Glauconite is generally abundant in the formation. The Eau Claire A Summary of the Stratigraphy of the increases in thickness southward in the Southern Peninsula of Michigan where it becomes much more Southern Peninsula of Michigan * dolomitic. by: The Dresbach sandstone is a fine to medium grained E. J. Baltrusaites, C. K. Clark, G. V. Cohee, R. P. Grant sandstone with well rounded and angular quartz grains. W. A. Kelly, K. K. Landes, G. D. Lindberg and R. B. Thin beds of argillaceous dolomite may occur locally in Newcombe of the Michigan Geological Society * the sandstone. It is about 100 feet thick in the Southern Peninsula of Michigan but is absent in Northern Indiana. The Franconia sandstone is a fine to medium grained Cambrian glauconitic and dolomitic sandstone. It is from 10 to 20 Cambrian rocks in the Southern Peninsula of Michigan feet thick where present in the Southern Peninsula. consist of sandstone, dolomite, and some shale. These * See last page rocks, Lake Superior sandstone, which are of Upper Cambrian age overlie pre-Cambrian rocks and are The Trempealeau is predominantly a buff to light brown divided into the Jacobsville sandstone overlain by the dolomite with a minor amount of sandy, glauconitic Munising. The Munising sandstone at the north is dolomite and dolomitic shale in the basal part. Zones of divided southward into the following formations in sandy dolomite are in the Trempealeau in addition to the ascending order: Mount Simon, Eau Claire, Dresbach basal part. A small amount of chert may be found in and Franconia sandstones overlain by the Trampealeau various places in the formation. -
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. -
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). -
Geoloaic District. Subsequent Stratigraphic Studies in This Area
DEVONIAN STRATA AND PALEOENVIRONMENTS: CHAUTAUQUA COUNTY REGION: NEW YORK STATE GORDON C. BAIRD and GARY G. LASH Department of Geosciences State University of New York College at Fredonia Fredonia, New York 14063 INTRODUCTION The history of the study of the Paleozoic stratigraphic divisions in New York State spans, at least, two centuries, and it records the early development of important concepts centrally germane to the study of sedimentary basins worldwide (see Tesmer, 1989). The works of James Hall, John Clarke, HenryS. Williams, Joseph Barrell, and George Chadwick are well known to most sedimentary workers, as are those of numerous subsequent workers. In particular, the sedimentary sequences of the Allegheny Plateau Region (••southern Tier" region) served as important sources of information for refinement of the fac ies concept ar.d for the widespread recognition of the westwardly prograding Catskill Delta Complex which is the primary Paleozoic story recorded in Southern Tier bedrock deposits (see Chadwick, 1924, 1933; Cooper, et al., 1942; Caster, 1934; Woodrow, 1985). ---- The first significant geologic work relating to the Chautauqua County region was presented in James Hall's (1843) Survey of the Fourth Geoloaic District. Subsequent stratigraphic studies in this area inclu e Clarke (1903), Chadwick (1923, 1924), Caster (1934), Pepper and de Witt (1950, 1951) and de Witt and Colton (1953). In northwest Pennsylvania, significant synthetic contributions include I.C. White (1881), Butts (1906-1908), Chadwick (1925), Caster ·(1934), Pepper et al. (1954). In Ohio, deposits equivalent to parts of the New York and - Pennsylvania Upper Devonian section (Chagrin Shale) have been the subject of recent paleoenvironmental studies (see Weidner and Feldmann, 1983; Schwimmer and Feldmann, 1990). -
Geologic Cross Section
Geologic Cross Section I–I′ Through the Appalachian Basin from the Eastern Margin of the Illinois Basin, Jefferson County, Kentucky, to the Valley and Ridge Province, Scott County, Virginia By Robert T. Ryder, Michael H. Trippi, and Christopher S. Swezey Pamphlet B to accompany Scientific Investigations Map 3343 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, Acting Director U.S. Geological Survey, Reston, Virginia: 2015 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copy- righted items must be secured from the copyright owner. Suggested citation: Ryder, R.T., Trippi, M.H., and Swezey, C.S., 2015, Geologic cross section I–I′ through the Appalachian basin from the eastern margin of the Illinois basin, Jefferson County, Kentucky, to the Valley and Ridge province, Scott County, Virginia: U.S. Geological Survey Scientific Investigations Map 3343, 2 sheets and pamphlet A, 41 p.; pamphlet B, 102 p., http://dx.doi.org/10.3133/sim3343. -
Upper Carboniferous–Lower Permian Buildups of the Carnic Alps, Austria–Italy 201 Upper Carboniferous–Lower Permian Buildups of the Carnic Alps, Austria–Italy
Published in "SEPM Special Publication No. 78: 201-217, 2003" which should be cited to reference this work. UPPER CARBONIFEROUS–LOWER PERMIAN BUILDUPS OF THE CARNIC ALPS, AUSTRIA–ITALY 201 UPPER CARBONIFEROUS–LOWER PERMIAN BUILDUPS OF THE CARNIC ALPS, AUSTRIA–ITALY ELIAS SAMANKASSOU Université de Fribourg, Département de Géosciences, Géologie et Paléontologie, Pérolles, CH-1700 Fribourg, Switzerland e-mail: [email protected] ABSTRACT: A variety of buildup types occur in the upper Paleozoic Auernig and Rattendorf Groups, Carnic Alps, at the present-day Austrian–Italian border, including coral, diverse algal (Anthracoporella, Archaeolithophyllum, Rectangulina, and phylloid green), bryozoan, brachiopod, and sponge buildups. Thin mounds and banks have a diverse fossil association (e.g., Archaeolithophyllum–bryozoan– brachiopod mounds) and occur in siliciclastic-dominated intervals, as do coral buildups. Some of the biodiverse thin mounds occur in strata that were deposited in cooler water. However, the thickest mounds are nearly monospecific (e.g., Anthracoporella mounds) and grew in carbonate-dominated, warm-water environments. Most of the mounds considered in this paper, particularly algal mounds, grew in quiet-water environments below wave base but within the photic zone. Mound growth was variously stopped by siliciclastic input, e.g., auloporid coral mounds, sea-level rise, e.g., the drowning of Anthracoporella mounds of the Rattendorf Group, influence of cool water, e.g., algal mounds of the Auernig Group overlain by limestone of cool-water biotic association, or sea-level fall, e.g., phylloid algal mounds that were subsequently exposed subaerially. There is no indication of ecological succession during mound growth. Growth, dimensions, biotic association, and termination of mounds seem to have been controlled by extrinsic factors, mainly sea level and water temperature. -
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. -
CIRRICULUM VITAE May 2009 BAIRD, GORDON CARDWELL
CIRRICULUM VITAE May 2009 BAIRD, GORDON CARDWELL BIRTHPLACE AND DATE: Rochester, New York, October 6, 1946 CITIZENSHIP: U.S.A. EDUCATION: B.A. - Earlham College, 1969 M.S. (Geology) - University of Nebraska, 1971 Ph.D. (Geology) - University of Rochester, 1975 AREA OF SPECILIZATION: Paleontology, chronostratigraphy, sedimentology, basin history and basin evolution. POSITIONS: State University of New York at Binghamton: postdoctoral research associate, 1975-1976. Field Museum of Natural History: Assistant Curator of Fossil Invertebrates, Aug. 1976-Dec. 1981. State University College, Fredonia, New York: Assistant Professor of Geology, 1982-1988; promoted to Associate Professor (9/88) and to Full Professor (9/95). GRANTS: NSF GRANT 257-029 (with E.S. Richardson, Jr.) Paleoecology of the Mazon Creek biota. Total grant $50,000 for two years (1/1/79- 1/11/81). Principal investigator. American Chemical Society (Petroleum Research Fund) Summer Fellowship. Part of Grant (PRF 141-71-G2) received by Carlton Brett (University of Rochester). Fellowship total $4,000 for two years (11/82-11/84). NSF grant accepted (with C.E. Brett: principal investigator) Episodic sedimentary events in the Middle Devonian Hamilton Group of Western and Central New York. Total grant $115,000 for two years 8/1/84-7/31/86). NSF grant EAR 88 16856 accepted (with C.E. Brett: principal investigator) 6/88. Small-scale depositional sequences in a Middle Devonian 1 foreland basin. Total grant $99,000 for two years - $7,860 summary salary for Baird. American Chemical Society (Petroleum Research Fund) summer fellowship. Part of grant received by Carlton Brett and David Lehmann (University of Rochester). -
U.S. Department of the Interior U.S. Geological Survey
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Prepared in cooperation with New Mexico Bureau of Mines and Mineral Resources 1997 MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American 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. Cover: View looking south to the east side of the northeastern Organ Mountains near Augustin Pass, White Sands Missile Range, New Mexico. Town of White Sands in distance. (Photo by Susan Bartsch-Winkler, 1995.) MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO By SUSAN BARTSCH-WINKLER, Editor ____________________________________________________ U. S GEOLOGICAL SURVEY OPEN-FILE REPORT 97-521 U.S. Geological Survey Prepared in cooperation with New Mexico Bureau of Mines and Mineral Resources, Socorro U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Mark Shaefer, Interim Director For sale by U.S. Geological Survey, Information Service Center Box 25286, Federal Center Denver, CO 80225 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 MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO Susan Bartsch-Winkler, Editor Summary Mimbres Resource Area is within the Basin and Range physiographic province of southwestern New Mexico that includes generally north- to northwest-trending mountain ranges composed of uplifted, faulted, and intruded strata ranging in age from Precambrian to Recent. -
Geothermometry of Selected Montana Hot Spring Waters by Michael
Geothermometry of selected Montana hot spring waters by Michael Bernard Kaczmarek A thesis submitted to the Graduate Faculty in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE with concentration in Geology Montana State University © Copyright by Michael Bernard Kaczmarek (1974) Abstract: The base temperature of hot-water dominated hydro-thermal systems can be quantitatively estimated using two different methods. One method uses the concentration of dissolved silica in the discharge wasters in equilibrium with respect to quarts. The other method is based on the ha, K, and Ca concentrations in the discharge waters in equilibrium with solid mineral phases in the wall rocks. Experimental studies and practical applications of these two hydrogeothermometers have been largely limited to the temperature range of 200 to 360°C. This paper presents some results of application of both methods in the temperature range 15 to 150°C. Dissolved silica calculated base temperatures are reliable for undiluced thermal waters in the temperature range studied. Sources of error are cold water dilution of thermal waters and assimilation of silica from amorphous silica in wall rocks. Base temperatures calculated from Na, K, and Ca concentrations in discharge waters are generally inaccurate. Errors in the calculated temperatures result from the fact that net water/rock reactions in the temperature range 15 to 150°C may be significantly different from those in the range 200 to 360°C, Net water/ rock reactions for the temperature range 15 to 150°C are presented here and the importance of E-mica versus kaolinite mineral phase stability is discussed.