Multidisciplinary Work to Determine Hydrology Of
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
UTEP) Geological Sciences
S. Pon1, D. De los Santos1, G. Alvarez-Rodriguez1, F. Enriquez1 S. Terrazas1, S. Terrazas1, J. Ricketts1, J.G. Olgin1,2, 1University of Texas at El Paso – Geological Sciences (500 University, El Paso, TX 79968), 2El Paso Community College – Physics Department (9570 Gateway N. Blvd, El Paso, TX 79924) Sarah Michelle Pon Deandra De Los Santos I am a senior at The University of Texas at El Paso, studying I am a senior at the University of Texas at El Paso (UTEP) Geological Sciences. I am excited to bring ideas and concepts of majoring in Geological Sciences and will graduate May, 2018. Abstract geology and planetary sciences to students. Whether it be During my time at UTEP, I have presented on salt diapirs and students who are pressuring a career in the sciences or students their possible entrainment methods at the Geological Society of just fulfilling their requirements. My goal with EIPS is to engage America conference in San Antonio. I also assisted Kuwanna Future Progress all students and get them asking questions and have them search Dyer-Pietras, a SUNY Binghampton University PhD candidate, The number of underrepresented minorities pursuing for the answers. with her research on boundaries between Eocene rock types For this internship, I have written a lab as an introduction to deposited in the shallow and deeper lake locations of the STEM fields, specifically in the sciences, has declined in remote sensing. I give a quick overview of what remote sensing is, Piceance basin in Rifle, Colorado, this past summer. I am now Furthermore, the Spring and Fall 2018 will include recent times [1]. -
The Cretaceous System in Central Sierra County, New Mexico
The Cretaceous System in central Sierra County, New Mexico Spencer G. Lucas, New Mexico Museum of Natural History, Albuquerque, NM 87104, [email protected] W. John Nelson, Illinois State Geological Survey, Champaign, IL 61820, [email protected] Karl Krainer, Institute of Geology, Innsbruck University, Innsbruck, A-6020 Austria, [email protected] Scott D. Elrick, Illinois State Geological Survey, Champaign, IL 61820, [email protected] Abstract (part of the Dakota Formation, Campana (Fig. 1). This is the most extensive outcrop Member of the Tres Hermanos Formation, area of Cretaceous rocks in southern New Upper Cretaceous sedimentary rocks are Flying Eagle Canyon Formation, Ash Canyon Mexico, and the exposed Cretaceous sec- Formation, and the entire McRae Group). A exposed in central Sierra County, southern tion is very thick, at about 2.5 km. First comprehensive understanding of the Cretaceous New Mexico, in the Fra Cristobal Mountains, recognized in 1860, these Cretaceous Caballo Mountains and in the topographically strata in Sierra County allows a more detailed inter- pretation of local geologic events in the context strata have been the subject of diverse, but low Cutter sag between the two ranges. The ~2.5 generally restricted, studies for more than km thick Cretaceous section is assigned to the of broad, transgressive-regressive (T-R) cycles of 150 years. (ascending order) Dakota Formation (locally deposition in the Western Interior Seaway, and includes the Oak Canyon [?] and Paguate also in terms of Laramide orogenic -
1 Supplementary Materials and Methods 1 S1 Expanded
1 Supplementary Materials and Methods 2 S1 Expanded Geologic and Paleogeographic Information 3 The carbonate nodules from Montañez et al., (2007) utilized in this study were collected from well-developed and 4 drained paleosols from: 1) the Eastern Shelf of the Midland Basin (N.C. Texas), 2) Paradox Basin (S.E. Utah), 3) Pedregosa 5 Basin (S.C. New Mexico), 4) Anadarko Basin (S.C. Oklahoma), and 5) the Grand Canyon Embayment (N.C. Arizona) (Fig. 6 1a; Richey et al., (2020)). The plant cuticle fossils come from localities in: 1) N.C. Texas (Lower Pease River [LPR], Lake 7 Kemp Dam [LKD], Parkey’s Oil Patch [POP], and Mitchell Creek [MC]; all representing localities that also provided 8 carbonate nodules or plant organic matter [POM] for Montañez et al., (2007), 2) N.C. New Mexico (Kinney Brick Quarry 9 [KB]), 3) S.E. Kansas (Hamilton Quarry [HQ]), 4) S.E. Illinois (Lake Sara Limestone [LSL]), and 5) S.W. Indiana (sub- 10 Minshall [SM]) (Fig. 1a, S2–4; Richey et al., (2020)). These localities span a wide portion of the western equatorial portion 11 of Euramerica during the latest Pennsylvanian through middle Permian (Fig. 1b). 12 13 S2 Biostratigraphic Correlations and Age Model 14 N.C. Texas stratigraphy and the position of pedogenic carbonate samples from Montañez et al., (2007) and cuticle were 15 inferred from N.C. Texas conodont biostratigraphy and its relation to Permian global conodont biostratigraphy (Tabor and 16 Montañez, 2004; Wardlaw, 2005; Henderson, 2018). The specific correlations used are (C. Henderson, personal 17 communication, August 2019): (1) The Stockwether Limestone Member of the Pueblo Formation contains Idiognathodus 18 isolatus, indicating that the Carboniferous-Permian boundary (298.9 Ma) and base of the Asselian resides in the Stockwether 19 Limestone (Wardlaw, 2005). -
Geologic Map of the Moriarty North 7.5-Minute Quadrangle, Santa Fe and Torrance Counties, New Mexico
Geologic Map of the Moriarty North 7.5-Minute Quadrangle, Santa Fe and Torrance Counties, New Mexico By Bruce Allen New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, NM 87801 June, 2016 New Mexico Bureau of Geology and Mineral Resources Open-file Digital Geologic Map OF-GM 258 Scale 1:24,000 This work was supported by the U.S. Geological Survey, National Cooperative Geologic Mapping Program (STATEMAP) under USGS Cooperative Agreement G15AC00243 and the New Mexico Bureau of Geology and Mineral Resources. New Mexico Bureau of Geology and Mineral Resources 801 Leroy Place, Socorro, New Mexico, 87801-4796 The views and conclusions contained in this document are those of the author and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government or the State of New Mexico. Description of Map Units to Accompany Geologic Map of the Moriarty North 7.5-Minute Quadrangle Bruce D. Allen* June 2016 *New Mexico Bureau of Geology and Mineral Resources, New Mexico Tech, Socorro, NM 87801 Description of Map Units to Accompany Geologic Map of the Moriarty North 7.5-Minute Quadrangle Bruce D. Allen, June 2016 General The Moriarty North 7.5-minute quadrangle (Fig. 1) is located about 50 km east of the Albuquerque metropolitan area in Santa Fe and Torrance counties, New Mexico. The quadrangle is in the ~5000 km2 Estancia topographic basin; the town of Moriarty and Interstate Highway 40 are located along its southern edge. Figure 1. Index map showing location of Moriarty North 7.5' quadrangle, generalized geology, and physiographic features. -
Rhenium-Osmium Geochronology and Geochemistry of the Permian Brushy
APPLICATIONS OF THE RHENIUM-OSMIUM ISOTOPIC SYSTEM, AND PLATINUM AND IRIDIUM ABUNDANCES IN ORGANIC-RICH MUD ROCKS: A GEOCHRONOLOGY, GEOCHEMISTRY, AND REDOX STUDY ------------------------------------------------------------- A Dissertation Presented to the Faculty of the Department of Earth and Atmospheric Sciences University of Houston ________________________________________ In Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy _________________________________________ By Shawn Curtis Wright August 2015 APPLICATIONS OF THE RHENIUM-OSMIUM ISOTOPIC SYSTEM, AND PLATINUM AND IRIDIUM ABUNDANCES IN ORGANIC-RICH MUD ROCKS: A GEOCHRONOLOGY, GEOCHEMISTRY, AND REDOX STUDY _______________________________________ Shawn Curtis Wright APPROVED: _______________________________________ Dr. Alan Brandon, Chairman _______________________________________ Dr. Henry Chafetz _______________________________________ Dr. William Dupré _______________________________________ Dr. Amy Kelly _______________________________________ Dr. Eugene Domack _______________________________________ Dean, College of Natural Sciences and Mathematics ii “Every major achievement is almost always preceded by years of toil, hard work, failure, stress, tests of character, determination, and sleepless nights... All of which help form the network of roots that can then support real accomplishments.” - Prakash Iyer iii APPLICATIONS OF THE RHENIUM-OSMIUM ISOTOPIC SYSTEM, AND PLATINUM AND IRIDIUM ABUNDANCES IN ORGANIC-RICH MUD ROCKS: A GEOCHRONOLOGY, GEOCHEMISTRY, -
Pennsylvanian Stratigraphy in the Northern Oscura Mountains, Socorro County, New Mexico Spencer G
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/60 Pennsylvanian stratigraphy in the northern Oscura Mountains, Socorro County, New Mexico Spencer G. Lucas and Karl Krainer, 2009, pp. 153-166 in: Geology of the Chupadera Mesa, Lueth, Virgil; Lucas, Spencer G.; Chamberlin, Richard M.; [eds.], New Mexico Geological Society 60th Annual Fall Field Conference Guidebook, 438 p. This is one of many related papers that were included in the 2009 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. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Paleontology of the Bears Ears National Monument
Paleontology of Bears Ears National Monument (Utah, USA): history of exploration, study, and designation 1,2 3 4 5 Jessica Uglesich , Robert J. Gay *, M. Allison Stegner , Adam K. Huttenlocker , Randall B. Irmis6 1 Friends of Cedar Mesa, Bluff, Utah 84512 U.S.A. 2 University of Texas at San Antonio, Department of Geosciences, San Antonio, Texas 78249 U.S.A. 3 Colorado Canyons Association, Grand Junction, Colorado 81501 U.S.A. 4 Department of Integrative Biology, University of Wisconsin-Madison, Madison, Wisconsin, 53706 U.S.A. 5 University of Southern California, Los Angeles, California 90007 U.S.A. 6 Natural History Museum of Utah and Department of Geology & Geophysics, University of Utah, 301 Wakara Way, Salt Lake City, Utah 84108-1214 U.S.A. *Corresponding author: [email protected] or [email protected] Submitted September 2018 PeerJ Preprints | https://doi.org/10.7287/peerj.preprints.3442v2 | CC BY 4.0 Open Access | rec: 23 Sep 2018, publ: 23 Sep 2018 ABSTRACT Bears Ears National Monument (BENM) is a new, landscape-scale national monument jointly administered by the Bureau of Land Management and the Forest Service in southeastern Utah as part of the National Conservation Lands system. As initially designated in 2016, BENM encompassed 1.3 million acres of land with exceptionally fossiliferous rock units. Subsequently, in December 2017, presidential action reduced BENM to two smaller management units (Indian Creek and Shash Jáá). Although the paleontological resources of BENM are extensive and abundant, they have historically been under-studied. Here, we summarize prior paleontological work within the original BENM boundaries in order to provide a complete picture of the paleontological resources, and synthesize the data which were used to support paleontological resource protection. -
Back Matter (PDF)
Index Page numbers in italics refer to Figures. Page numbers in bold refer to Tables. Abadeh Section (Iran) 74, 81, 83, 112 Annweiler Formation 397 Abadehceras 198 Anomalonema reumauxi–Peudestheria simoni assemblage Abichites 199 zone 370, 372–373 Abo Formation 73, 408, 409, 412, 425 Antarctica, palynostratigraphy 337 Abrahamskraal Formation 64, 78, 80, 418, 428 Anthracolithic System 25 radiometric dating 86 Anuites 193 Abrek Formation 295 Apache Dam Formation 409 acritarchs 322–323 Aquaw Creek (Colorado), magnetic polarity data 66 Admiral Formation 410 Arabia, palynostratigraphy 333, 333 Adrianites 194 Arabia Plate, fusuline biostratigraphy 255 A. elegans 195 Araksian Stage 40 Afghanistan Arasella 199 fusuline biostratigraphy 255, 260–261 Araxoceras spp. 196, 198 Agathiceras 187, 189 A. latissimum 198 Aidaralash CreekGSSP (Kazakstan)3, 28,29, 32, 53,67, 88,187,321,325 A. ventrosulcatum 198 Akiyoshi Terrane, fusuline biostratigraphy 270–271, 271 Archer City Formation 410, 411 Akmilleria 189 archosaurs 51 Aktastinian Substage 2, 33, 189 Argentina ammonoid assemblages 185 magnetic polarity data 64, 69, 72 Aktasty River Section 33 palynostratigraphy 330, 331, 331 Aktastynian Stage, ammonoid assemblages 185 tetrapods 387 Aktubinskia 189 Aricoceras 192 Aktyubinsk section 33 Aristoceras 187 Al Khlata Formation 336 Aristoceratoides 194 Alaska Region, fusuline biostratigraphy 255 Arizona, tetrapods 412–413 Albaillella cavitata interval zone 154, 157 Arnhardtia 39 Albaillella excelsa interval zone 155 Arrayo de Alamillo Formation 395, 409 Albaillella levis interval zone 155 Arroya del Agua Formation 408, 409, 425 Albaillella sinuata abindance zone 148–149 Arroya Formation 410 Albaillella triangularis interval zone 155, 157 Arroyo Vale Formation 411 Albaillella xiaodongensis assemblage zone 148 Artinskia spp. -
Geologic Resources Inventory Map Document for Glen Canyon National Recreation Area
U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Directorate Geologic Resources Division Glen Canyon National Recreation Area GRI Ancillary Map Information Document Produced to accompany the Geologic Resources Inventory (GRI) Digital Geologic Data for Glen Canyon National Recreation Area glca_geology.pdf Version: 9/29/2011 I Glen Canyon National Recreation Area Geologic Resources Inventory Map Document for Glen Canyon National Recreation Area Table of Contents Geolog.i.c. .R...e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .M...a..p.. .D..o..c..u..m...e..n..t....................................................................... 1 About th..e.. .N...P..S.. .G...e..o..l.o..g..i.c. .R...e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .P...r.o..g..r.a..m........................................................... 2 Map Un.i.t. .L..i.s..t.......................................................................................................................... 4 Map Un.i.t. .D..e..s..c..r.i.p..t.i.o..n..s............................................................................................................. 8 Man ma..d..e.. .d..e..p..o..s..i.t.s....................................................................................................................................................... 8 Qfd - .A...r.t.i.f.i.c..ia..l. .f.i.l.l .a..n..d.. .d..i.s..t.u..r.b..e..d.. .a..r..e..a..s.. .(.H..o..l.o..c..e..n..e..).............................................................................................. 8 Qfdm .-.. .C..o..n..c..r.e..t.e.. .f..il.l. .in.. .G...l.e..n.. .C..a..n..y..o..n.. .D..a..m... .(.H...o..lo..c..e..n..e..).......................................................................................... 8 Alluvial. .d..e..p..o..s..i.t.s........................................................................................................................................................... -
This Article Appeared in a Journal Published by Elsevier
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Palaeogeography, Palaeoclimatology, Palaeoecology 342–343 (2012) 17–26 Contents lists available at SciVerse ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Increased continental weathering flux during orbital-scale sea-level highstands: Evidence from Nd and O isotope trends in Middle Pennsylvanian cyclic carbonates Bethany P. Theiling a,b,⁎, Maya Elrick a, Yemane Asmerom a a University of New Mexico, United States b Purdue University, United States article info abstract Article history: Despite the common occurrence of orbital-scale (104–105 yr) sedimentary cycles in a wide range of Protero- Received 16 September 2011 zoic through Neogene marine and non-marine depositional systems, understanding the effects and phase re- Received in revised form 16 April -
Developing a 3-D Subsidence Model for the Late Paleozoic Taos Trough in Northern New Mexico
Developing a 3-D subsidence model for the late Paleozoic Taos trough in northern New Mexico By Nur Uddin Md Khaled Chowdhury, MS A Dissertation In Geology Submitted to the Graduate Faculty of Texas Tech University in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY Approved Dustin E. Sweet Chair of Committee George B. Asquith James E. Barrick Seiichi Nagihara Mark Sheridan Dean of the Graduate School December, 2019 Copyright 2019, Nur Uddin Md Khaled Chowdhury Texas Tech University, Nur Uddin Md Khaled Chowdhury, December 2019 ACKNOWLEDGEMENTS Numerous individuals have been instrumental in the completion of this dissertation. First, and foremost, I would like to sincerely thank my adviser, Dr. Dustin E. Sweet, for his guidance, unwavering support, and ultimately, for making this endeavor thoroughly exciting and enjoyable. I also sincerely thank my committee members Dr. George B. Asquith, Dr. James E. Barrick, and Dr. Seiichi Nagihara. I would like to thank Annabelle Lopez and New Mexico Bureau of Geology & Mineral Resources for providing me access to cores and cuttings repository and providing me available resources including well log data, well reports and strip logs relevant to this study. I am thankful to Neuralog Inc. for providing me free access to Neuralog software. Funding for this research was generously supported by John Emery Adams Memorial Scholarship and Concho Resources Inc. Scholarship from West Texas Geological Society (WTGS), student research grants from Geological Society of America (GSA), and grants-in-aid from the southwest section of American Association of Petroleum Geologists (AAPG). I am indebted to the department of Geosciences at Texas Tech University.