DOCSLIB.ORG

Geologic Resources Inventory Map Document for Chattahoochee River National Recreation Area

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Geologic Resources Inventory Map Document for Chattahoochee River National Recreation Area U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Directorate Geologic Resources Division Chattahoochee River National Recreation Area GRI Ancillary Map Information Document Produced to accompany the Geologic Resources Inventory (GRI) Digital Geologic Data for Chattahoochee River National Recreation Area chat_geology.pdf Version: 1/16/2013 I Chattahoochee River National Recreation Area Geologic Resources Inventory Map Document for Chattahoochee River National Recreation Area Table of Contents Geologi.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 GRI Dig.i.t.a..l. .M...a..p..s. .a..n..d.. .S..o..u..r..c.e.. .M...a..p.. .C..i.t.a..t.i.o..n..s............................................................................ 4 GRI Digital Geologic Map of the Southern portion of Chattah.o..o..c..h..e..e.. .N..R..A................................................................................................................. 5 CHTS M..a..p.. .U...n..it. .L..i.s..t....................................................................................................................................................... 5 CHTS M..a..p.. .U...n..it. .D...e..s..c..r.i.p..t.io..n..s.......................................................................................................................................... 6 JTRd .-. .D..i.a..b..a..s..e.. .(.L..a..t.e.. .T..r..ia..s..s..i.c.. .t.o.. .E..a..r.l.y.. .J..u..r.a..s..s..i.c..)................................................................................................ 6 PPNM.m..b.. .-.. .M..y..l.o..n..i.t.iz..e..d.. .B...e..n.. .H..i.ll. .G...r.a..n..i.t.e.. .(.C..a..r..b..o..n..if..e..r.o..u..s..?.. .t.o.. .P..e..r.m...i.a..n..?..)................................................................ 6 PSm -. .M...y..lo..n..i.t.i.z..e..d.. .g..r.a..n..i.t.o..id.. .(..S..i.lu..r..ia..n..?.. .t.o.. .P..e..r..m..i.a..n..?..)............................................................................................. 6 POb -. .B..u..t.t.o..n.. .s..c..h..i.s..t. .(.U..p..p..e..r.. .O..r..d..o..v..ic..i.a..n..?.. .t.o.. .P..e..r.m...i.a..n..?..)........................................................................................ 7 POms. .-. .B...u..t.t.o..n.. .s..c..h..is..t. .a..n..d.. .s..h..e..a..r..e..d.. .a..m..p..h..i.b..o..l.it.e.. .(..U..p..p..e..r. .O...r.d..o..v..i.c..i.a..n..?.. .t.o.. .P..e..r.m...ia..n..?..).............................................. 7 POs -. .G..a..r..n..e..t. .H..i.ll. .t.y..p..e.. .a..l.t.e..r.e..d.. .r.o..c..k..s.. .(.U...p..p..e..r. .O...r.d..o..v..i.c..ia..n..?.. .t.o.. .P..e..r..m..i.a..n..?..)............................................................... 7 PYl - L..o..n..g.. .I.s..l.a..n..d.. .C..r.e..e..k.. .G...n..e..is..s.. .(..M..i.d..d..l.e.. .P..r.o..t.e..r.o..z..o..i.c..?.. .t.o.. .P..e..r.m...i.a..n..?..).................................................................... 7 PNMb. .-. .B..e..n.. .H...il.l. .G..r..a..n..it.e.. .(..P..e..n..n..s..y..lv..a..n..i.a..n.. .a..n..d.. .M...is..s..i.s..s..i.p..p..ia..n..)................................................................................ 8 Dl - Li.t.h..o..n..ia.. .G...n..e..i.s..s..,. .u..n..d..iv..d..e..d.. .(..D..e..v..o..n..i.a..n..).......................................................................................................... 8 PZgn .-. .U...n..n..a..m..e..d.. .g..r..a..n..it.i.c.. .g..n..e..i.s..s.. .(.P..a..l.e..o..z..o..ic..)....................................................................................................... 9 OCbh. .-. .I.n..f.o..r.m...a..l. .s..c..h..is..t. .o..f.. .H..u..l.e..t.t. .f.a..c..i.e..s.. .(.C..a..m...b..r.i.a..n.. .t.o.. .L..o..w...e..r.. .O..r..d..o..v..ic..i.a..n..?..)......................................................... 9 OZu -. .A...lt.e..r..e..d.. .m..e..t.a..-..u..lt.r..a..m..a..f..ic.. .r..o..c..k. .(..L..a..t.e.. .P..r.o..t.e..r.o..z..o..i.c..?.. .t.o.. .M...id..d..l.e.. .O...r.d..o..v..i.c..ia..n..?..).................................................. 9 OZus. .-. .S..e..r..p..e..n..t.in..i.t.e.. .(.L..a..t.e.. .P..r..o..t.e..r.o..z..o..i.c..?.. .t.o.. .M..i.d..d..l.e.. .O..r..d..o..v..ic..i.a..n..?..).......................................................................... 9 OZs -. .S..t.o..n..e..w....a..ll. .G...n..e..is..s.. .(..L..a..t.e.. .P..r.o..t.e..r.o..z..o..i.c..?.. .t.o.. .M...id..d..l.e.. .O...r.d..o..v..i.c..ia..n..?..)................................................................... 9 OZs.p.. .-. .S..t.o..n..e..w....a..ll. .G...n..e..is..s..,. .P..o..w....e..r.s.. .F..e..r.r..y.. .M..e..m...b..e..r. .(..L..a..t.e.. .P..r.o..t.e..r.o..z..o..i.c..?.. .t.o.. .M...id..d..l.e.. .O...r.d..o..v..i.c..ia..n..?..)......................... 10 OZc.m.. .-.. .C..l.a..ir..m..o..n..t. .F..o..r..m..a..t.i.o..n.. .(.L..a..t.e.. .P..r..o..t.e..r.o..z..o..i.c..?.. .t.o.. .M..i.d..d..l.e.. .O..r..d..o..v..ic..i.a..n..?..)........................................................... 10 OZc.r. .-. .C...r.i.d..e..r. .G...n..e..is..s.. .(..L..a..t.e.. .P..r.o..t.e..r.o..z..o..i.c..?.. .t.o.. .M...id..d..l.e.. .O...r.d..o..v..i.c..ia..n..?..)...................................................................... 10 OZr .-. .R...o..p..e..s.. .C..r.e..e..k.. .M...e..t.a..b..a..s..a..lt. .(..L..a..t.e.. .P..r.o..t.e..r.o..z..o..i.c..?.. .t.o.. .M...id..d..l.e.. .O...r.d..o..v..i.c..ia..n..?..)....................................................... 11 OZw.. .-. .W....a..h..o..o.. .C..r.e..e..k.. .F..o..r.m...a..t.i.o..n.. .(.L..a..t.e.. .P..r.o..t.e..r..o..z..o..ic..?.. .t.o.. .M...i.d..d..le.. .O...r.d..o..v..i.c..i.a..n..?..)..................................................... 11 OZm. .-.. .In..f..o..r.m...a..l .m...i.x..e..d.. .u..n..it. .(..L..a..t.e.. .P..r.o..t.e..r.o..z..o..i.c..?.. .t.o.. .M...id..d..l.e.. .O...r.d..o..v..i.c..ia..n..?..)............................................................... 11 OZm.g..s.. .-.. .G..a..r..n..e..t.-.r.i.c..h.. .s..c..h..i.s..t. .(.L..a..t.e.. .P..r.o..t.e..r..o..z..o..ic..?.. .t.o.. .M...i.d..d..le.. .O...r.d..o..v..i.c..i.a..n..?..)........................................................... 12 OZm.m... .-. .S...p..e..s..s..a..r.t.i.n..e.. .q..u..a..r.t.z..i.t.e.. .(.L..a..t.e.. .P..r.o..t.e..r..o..z..o..ic..?.. .t.o.. .M...i.d..d..le.. .O...r.d..o..v..i.c..i.a..n..?..)....................................................... 12 OZc.l .-.. .C..l.a..r.k..s..t.o..n.. .F..o..r.m...a..t.io..n.. .(..L..a..t.e.. .P..r.o..t.e..r.o..z..o..i.c..?.. .t.o.. .M...id..d..l.e.. .O...r.d..o..v..i.c..ia..n..?..)............................................................. 12 OZa. .-. .A...m..p..h..i.b..o..l.it.e.. .(..L..a..t.e.. .P..r.o..t.e..r.o..z..o..i.c..?.. .t.o.. .M...id..d..l.e.. .O...r.d..o..v..i.c..ia..n..?..)........................................................................... 12 Caq .-. .T..h..i.n.. .(.<..2..m... .t.h..i.c..k.).. .m..a..p..p..a..b..l.e.. .u..n..i.t.s.. .o..f. .m...u..s..c..o..v..it.e.. .q..u..a..r..t.z..it.e.. .(..C..a..m...b..r.i.a..n..?..)..................................................... 13 Ccf -.. .C..r.a..w....f.i.s..h.. .C..r.e..e..k.. .F..o..r.m...a..t.i.o..n.. .(.C..a..m...b..r.i.a..n.. .a..n..d.. .C..a..m...b..r.i.a..n..?..)............................................................................ 13 Ccq .-. .C...le..a..n.. .q..u..a..r..t.z..it.e.. .u..n..i.t.s.. .(.C...a..m..b..r..ia..n.. .a..n..d.. .C...a..m..b..r..ia..n..?..)..................................................................................... 13 Ccp .-. .C...h..a..t.t.a..h..o..o..c..h..e..e.. .P..a..li.s..a..d..e..s.. .Q...u..a..r.t.z..i.t.e.. .(.C..a..m...b..r.i.a..n..?..).................................................................................... 13 Cas .-. .A...l.u..m..i.n..o..u..s.. .s..c..h..i.s..t. .u..n..it. .(..C..a..m...b..r.i.a..n..?..).......................................................................................................... 13 Geolo.g..i.c.. .In..v..e..s..t.i.g..a..t.i.o..n..s.. .S..e..r.i.e..s.. .M...a..p.. .I-..2..6..0..2................................................................................................................. 13 Map .I.-.2..6..0..2.. .C...o..r.r.e..l.a..t.i.o..n.. .o..f. .U..n..i.t.s.
Load more

Recommended publications
  • ECTE0017.Pdf
    Universidad de Investigación de Tecnología Experimental Yachay ESCUELA DE CIENCIAS DE LA TIERRA ENERGÍA Y AMBIENTE Characterization of the Silante Fm. Along the Salinas-Lita Transect in Northern Ecuador Trabajo de integración curricular presentado como requisito para la obtención del título de Geólogo Autor: Luis Bryan Sarmiento López Tutor: PhD. Rafael Almeida Urcuquí, September 2020 ii iii AUTORÍA Yo, LUIS BRYAN SARMIENTO LÓPEZ, con cédula de identidad 1724886385, declaro que las ideas, juicios, valoraciones, interpretaciones, consultas bibliográficas, definiciones y conceptualizaciones expuestas en el presente trabajo; así cómo, los procedimientos y herramientas utilizadas en la investigación, son de absoluta responsabilidad de el/la autora (a) del trabajo de integración curricular. Así mismo, me acojo a los reglamentos internos de la Universidad de Investigación de Tecnología Experimental Yachay. Urcuquí, noviembre 2020. ___________________________ Luis Bryan Sarmiento López CI:1724886385 iv AUTORIZACIÓN DE PUBLICACIÓN Yo, LUIS BRYAN SARMIENTO LÓPEZ, con cédula de identidad 1724886385, cedo a la Universidad de Tecnología Experimental Yachay, los derechos de publicación de la presente obra, sin que deba haber un reconocimiento económico por este concepto. Declaro además que el texto del presente trabajo de titulación no podrá ser cedido a ninguna empresa editorial para su publicación u otros fines, sin contar previamente con la autorización escrita de la Universidad. Asimismo, autorizo a la Universidad que realice la digitalización y publicación de este trabajo de integración curricular en el repositorio virtual, de conformidad a lo dispuesto en el Art. 144 de la Ley Orgánica de Educación Superior Urcuquí, noviembre 2020. ___________________________ Luis Bryan Sarmiento López CI: 1724886385 v DEDICATORY I want to dedicate this work to my parents Lucia López and Luis Abelardo Sarmiento because this achievement is theirs, and to my grandfather Eladio López for being the voice of wisdom that helps me make my way to my goals.
    [Show full text]
  • A New Giant Basal Titanosaur Sauropod in the Upper Cretaceous (Coniacian) of the Neuquen Basin, Argentina
    Cretaceous Research 100 (2019) 61e81 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes A new giant basal titanosaur sauropod in the Upper Cretaceous (Coniacian) of the Neuquen Basin, Argentina * Leonardo S. Filippi a, , Leonardo Salgado b, c, Alberto C. Garrido d, e a Museo Municipal Argentino Urquiza, Jujuy y Chaco s/n, 8319 Rincon de los Sauces, Neuquen, Argentina b CONICET, Argentina c Instituto de Investigacion en Paleobiología y Geología, Universidad Nacional de Río Negro-Conicet, Av. Gral. J. A. Roca 1242, 8332 General Roca, Río Negro, Argentina d Museo Provincial de Ciencias Naturales “Profesor Dr. Juan A. Olsacher”, Direccion Provincial de Minería, Etcheluz y Ejercito Argentino, 8340 Zapala, Neuquen, Argentina e Departamento Geología y Petroleo, Facultad de Ingeniería, Universidad Nacional del Comahue, Buenos Aires 1400, Neuquen 8300, provincia del Neuquen, Argentina article info abstract Article history: A new basal sauropod titanosaur, Kaijutitan maui gen. et sp. nov., is described. The holotype of this Received 21 November 2018 species, which comes from the Sierra Barrosa Formation (upper Coniacian, Upper Cretaceous), consists of Received in revised form cranial, axial, and appendicular elements presenting an unique combination of plesiomorphic and 3 February 2019 apomorphic characters. The most notable characteristic observed in Kaijutitan is the presence of anterior Accepted in revised form 9 March 2019 cervical vertebrae with bifid neural spines, a condition that would have evolved several times among Available online 28 March 2019 sauropods. The phylogenetic analysis places Kaijutitan as a basal titanosaur, the sister taxon of Epachthosaurus þ Eutitanosauria. The new species supports the coexistence, in the Late Cretaceous Keywords: Sauropoda (Turonian-Santonian), of basal titanosaurs and eutitanosaurian sauropods, at least in Patagonia.
    [Show full text]
  • Article (Published Version)
    Article Carboniferous Orogenic Gold Deposits at Pataz, Eastern Andean Cordillera, Peru: Geological and Structural Framework, Paragenesis, Alteration, and 40Ar/39Ar Geochronology HAEBERLIN, Yves, et al. Abstract The Pataz province forms the central part of a ≥160-km-long orogenic gold belt extending along the Eastern Andean Cordillera in northern Peru and has produced a total of 6 million ounces (Moz) gold from vein-type deposits during the last 100 yr. The deposits present several recurrent and typical field characteristics, including (1) at a regional scale, location of the mineralization in low-order structures within a 1- to 5-km-wide structural corridor east of a major north-northwest–striking lineament and in spatial association with the northnorthwest– striking margins of the 330 to 327 Ma Pataz batholith; (2) at the mine scale, strong lithological controls of the vein geometries and styles, the lodes occurring as fairly continuous ≤5-km-long quartz veins inside or along the margins of the batholith or as branching and bedding-concordant narrow ore shoots within adjacent folded Ordovician turbidite sequences; (3) consistent orientations of veins, in particular within the batholith, where more than 80 percent of the quartz veins are emplaced in north- to northwest-striking, eastdipping, brittle-ductile deformation [...] Reference HAEBERLIN, Yves, et al. Carboniferous Orogenic Gold Deposits at Pataz, Eastern Andean Cordillera, Peru: Geological and Structural Framework, Paragenesis, Alteration, and 40Ar/39Ar Geochronology. Economic Geology, 2004, vol. 99, no. 1, p. 73-112 DOI : 10.2113/gsecongeo.99.1.73 Available at: http://archive-ouverte.unige.ch/unige:21636 Disclaimer: layout of this document may differ from the published version.
    [Show full text]
  • Controls on Middle to Late Ordovician Synorogenic Deposition in the Southeastern Corner of Laurentia
    University of Kentucky UKnowledge University of Kentucky Doctoral Dissertations Graduate School 2003 CONTROLS ON MIDDLE TO LATE ORDOVICIAN SYNOROGENIC DEPOSITION IN THE SOUTHEASTERN CORNER OF LAURENTIA German Bayona University of Kentucky, [email protected] Right click to open a feedback form in a new tab to let us know how this document benefits ou.y Recommended Citation Bayona, German, "CONTROLS ON MIDDLE TO LATE ORDOVICIAN SYNOROGENIC DEPOSITION IN THE SOUTHEASTERN CORNER OF LAURENTIA" (2003). University of Kentucky Doctoral Dissertations. 364. https://uknowledge.uky.edu/gradschool_diss/364 This Dissertation is brought to you for free and open access by the Graduate School at UKnowledge. It has been accepted for inclusion in University of Kentucky Doctoral Dissertations by an authorized administrator of UKnowledge. For more information, please contact [email protected]. ABSTRACT OF DISSERTATION Germán Bayona The Graduate School University of Kentucky 2003 CONTROLS ON MIDDLE TO LATE ORDOVICIAN SYNOROGENIC DEPOSITION IN THE SOUTHEASTERN CORNER OF LAURENTIA _____________________________________ ABSTRACT OF DISSERTATION _____________________________________ A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the College of Arts and Sciences at the University of Kentucky By Germán Bayona Lexington, Kentucky Director: Dr. William A. Thomas, Professor of Geological Sciences Lexington, Kentucky 2003 Copyright © Germán Bayona 2003 ABSTRACT OF DISSERTATION CONTROLS ON MIDDLE TO LATE ORDOVICIAN SYNOROGENIC DEPOSITION IN THE SOUTHEASTERN CORNER OF LAURENTIA Middle and Upper Ordovician strata in the southernmost Appalachians document initial collision along the southeastern margin of Laurentia during the Blountian orogeny, an early phase of the Taconic orogeny. Coeval drowning and exposure of different parts of the former platform and variations in stratal architecture have been attributed to tectonic and depositional loading along the collisional margin.
    [Show full text]
  • Geologic Map of the Great Smoky Mountains National Park Region, Tennessee and North Carolina
    Prepared in cooperation with the National Park Service Geologic Map of the Great Smoky Mountains National Park Region, Tennessee and North Carolina By Scott Southworth, Art Schultz, John N. Aleinikoff, and Arthur J. Merschat Pamphlet to accompany Scientific Investigations Map 2997 Supersedes USGS Open-File Reports 03–381, 2004–1410, and 2005–1225 2012 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 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 To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Southworth, Scott, Schultz, Art, Aleinikoff, J.N., and Merschat, A.J., 2012, Geologic map of the Great Smoky Moun- tains National Park region, Tennessee and North Carolina: U.S. Geological Survey Scientific Investigations Map 2997, one sheet, scale 1:100,000, and 54-p. pamphlet. (Supersedes USGS Open-File Reports 03–381, 2004–1410, and 2005–1225.) ISBN 978-1-4113-2403-9 Cover: Looking northeast toward Mount Le Conte, Tenn., from Clingmans Dome, Tenn.-N.C.
    [Show full text]
  • TRACE: Tennessee Research and Creative Exchange
    University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Masters Theses Graduate School 8-2003 Structural and Stratigraphic Investigations at the Southwest End of the Tellico-Sevier Syncline, Southeast Tennessee Milan A. Heath II University of Tennessee - Knoxville Follow this and additional works at: https://trace.tennessee.edu/utk_gradthes Part of the Geology Commons Recommended Citation Heath, Milan A. II, "Structural and Stratigraphic Investigations at the Southwest End of the Tellico-Sevier Syncline, Southeast Tennessee. " Master's Thesis, University of Tennessee, 2003. https://trace.tennessee.edu/utk_gradthes/1973 This Thesis is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Masters Theses by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a thesis written by Milan A. Heath II entitled "Structural and Stratigraphic Investigations at the Southwest End of the Tellico-Sevier Syncline, Southeast Tennessee." I have examined the final electronic copy of this thesis for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Master of Science, with a major in Geology. Robert D. Hatcher, Jr, Major Professor We have read this thesis and recommend its acceptance: William M. Dunne, Steven G. Driese Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) To the Graduate Council: I am submitting herewith a thesis written by Milan A.
    [Show full text]
  • Flora and Vegetation of the Huascarán National Park, Ancash, Peru: With
    Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1988 Flora and vegetation of the Huascarán National Park, Ancash, Peru: with preliminary taxonomic studies for a manual of the flora David Nelson Smith Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Botany Commons Recommended Citation Smith, David Nelson, "Flora and vegetation of the Huascarán National Park, Ancash, Peru: with preliminary taxonomic studies for a manual of the flora " (1988). Retrospective Theses and Dissertations. 8891. https://lib.dr.iastate.edu/rtd/8891 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. INFORMATION TO USERS The most advanced technology has been used to photo­ graph and reproduce this manuscript from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion.
    [Show full text]
  • Heidelbergensis
    GAEA heidelbergensis The 23rd Latin American Colloquium on Earth Sciences Christina Ifrim, Francisco José Cueto Berciano and Wolfgang Stinnesbeck 19 23rd LAK, 2014, Heidelberg Organizing Team 3 Organizing Team Organizers Organizing Team Dominic Lange Christina Ifrim Sami Al Najem Manuela Lexen Wolfgang Stinnesbeck Gregor Austermann Christian Lorson Seija Beckmann Martin Maier Organizing Desk Suzana Bengtson Annika Meuter Peter Bengtson Manuela Böhm Georg Miernik Francisco José Cueto Berciano Sven Brysch Filip Neuwirth Karin Dietzschold Marcelo Carvalho Daniela Oestreich Kristina Eck Carolina Doranti Tiritan Judith Pardo Ulrich A. Glasmacher Werner Fielitz Lisa Pees Margot Isenbeck-Schröter Nico Goppold Ricardo Pereyra Carla Gutiérrez Basso Daniel Pfeiff Jan Hartmann Sabrina Pfister Dominik Hennhöfer Thomas Reutner Fabio Hering Silvia Rheinberger Anne Hildenbrand Stefan Rheinberger Michael Hornacsek Simon Ritter Hartmut Jäger Lennart Rohrer Maximilian Janson Gerhard Schmidt Graciela Kahn Christian Scholz Jens Kaub Dominik Soyk Bernd Kober Christian Stippich Sebastian Kollenz Manfred Vogt Johanna Kontny Klaus Will Eduardo A.M. Koutsoukos Patricio Zambrano Lobos Michael Kraeft Patrick Zell Cite as: Ifrim, C., Bengtson, P., Cueto Berciano, F.J., Stinnesbeck, W. (Eds.) 2014: 23rd International Colloquium on Latin American Earth Sciences, Abstracts and Programme. GAEA heidelbergensis 19, 176 pp. Cover picture: Landscape with 4 levels of geology. Photo: Wolfgang Stinnesbeck 4 Supported by 23rd LAK, 2014, Heidelberg Kindly supported by Bundesministerium
    [Show full text]
  • Heidelbergensis
    GAEA heidelbergensis The 23rd Latin American Colloquium on Earth Sciences Christina Ifrim, Francisco José Cueto Berciano and Wolfgang Stinnesbeck 19 23rd LAK, 2014, Heidelberg Organizing Team 3 Organizing Team Organizers Organizing Team Dominic Lange Christina Ifrim Sami Al Najem Manuela Lexen Wolfgang Stinnesbeck Gregor Austermann Christian Lorson Seija Beckmann Martin Maier Organizing Desk Suzana Bengtson Annika Meuter Peter Bengtson Manuela Böhm Georg Miernik Francisco José Cueto Berciano Sven Brysch Filip Neuwirth Karin Dietzschold Marcelo Carvalho Daniela Oestreich Kristina Eck Carolina Doranti Tiritan Judith Pardo Ulrich A. Glasmacher Werner Fielitz Lisa Pees Margot Isenbeck-Schröter Nico Goppold Ricardo Pereyra Carla Gutiérrez Basso Daniel Pfeiff Jan Hartmann Sabrina Pfister Dominik Hennhöfer Thomas Reutner Fabio Hering Silvia Rheinberger Anne Hildenbrand Stefan Rheinberger Michael Hornacsek Simon Ritter Hartmut Jäger Lennart Rohrer Maximilian Janson Gerhard Schmidt Graciela Kahn Christian Scholz Jens Kaub Dominik Soyk Bernd Kober Christian Stippich Sebastian Kollenz Manfred Vogt Johanna Kontny Klaus Will Eduardo A.M. Koutsoukos Patricio Zambrano Lobos Michael Kraeft Patrick Zell Cite as: Ifrim, C., Bengtson, P., Cueto Berciano, F.J., Stinnesbeck, W. (Eds.) 2014: 23rd International Colloquium on Latin American Earth Sciences, Abstracts and Programme. GAEA heidelbergensis 19, 176 pp. Cover picture: Landscape with 4 levels of geology. Photo: Wolfgang Stinnesbeck 4 Supported by 23rd LAK, 2014, Heidelberg Kindly supported by Bundesministerium
    [Show full text]
  • Nouveau Modèle Tectono-Climatique Des Andes Centrales Du Nord (5-9°S)
    THESE` En vue de l’obtention du DOCTORAT DE L’UNIVERSITE´ DE TOULOUSE Délivré par: Université de Toulouse III Paul Sabatier (UT3 Paul Sabatier) présentée et soutenue publiquement par Alice Prudhomme le 17 avril 2019 Titre: Nouveau modèle tectono-climatique des Andes Centrales du Nord (5-9°S) Directeurs de thèse: Patrice Baby et Alexandra Robert Ecole´ doctorale: Sciences de l’univers, de l’environnement et de l’espace (SDU2E) Discipline ou spécialité: Sciences de la Terre et des Planètes Solides JURY: Sébastien Carretier, DR, GET, Toulouse Président du jury Jean-Paul Callot, Pr., UPPA, Pau Rapporteur Isabelle Moretti, Chercheuse associée, ISTeP, Paris Rapporteure Xavier Robert, CR, ISTerre, Grenoble Examinateur Patrice Baby, DR, GET, Toulouse Directeur de thèse Alexandra Robert, MCF, GET, Toulouse Directrice de thèse Stéphane Brusset, MCF, GET, Toulouse Invité 2 Remerciements et digressions Je profite de cette page blanche pour écrire quelques lignes sur les raisons et rencontres qui m’ont amenée à faire une thèse sur une des plus belles chaînes de montagnes, mais aussi pour remercier ceux qui m’ont accompagnée dans l’aboutissement de cette thèse. Ca commence certainement par une petite collection de fossiles et de minéraux durant mon enfance, comme sûrement beaucoup de géologues, à part pour certains inconditionnels de Jurassic Park ! On hérite un jour d’une petite boîte de ces pierres, précieuses à nos yeux, et puis vient l’envie de dénicher ces trésors du passé dans des amas de poussières et de cailloux. On y comprend rien à ces pierres, elles sont juste belles, brillantes ou colorées, et parfois captent la vie ! C’est plus tard au lycée qu’on saisie enfin que ces pierres sont le fruit d’un événement particulier, et même de plusieurs, et qu’on peut finalement remonter dans le temps, retracer les changements d’environnement d’une pierre, et finalement comprendre comment fonctionne le système Terre.
    [Show full text]
  • Detailed Geologic Mapping of the Parksville 7.5-Minute Quadrangle
    University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Masters Theses Graduate School 12-2018 DETAILED GEOLOGIC MAPPING OF THE PARKSVILLE 7.5-MINUTE QUADRANGLE AND THE KINEMATICS OF EMPLACEMENT OF LARGE HORSES ALONG THE GREAT SMOKY FAULT, SOUTHEASTERN TENNESSEE Trenton Joel Walker University of Tennessee Follow this and additional works at: https://trace.tennessee.edu/utk_gradthes Recommended Citation Walker, Trenton Joel, "DETAILED GEOLOGIC MAPPING OF THE PARKSVILLE 7.5-MINUTE QUADRANGLE AND THE KINEMATICS OF EMPLACEMENT OF LARGE HORSES ALONG THE GREAT SMOKY FAULT, SOUTHEASTERN TENNESSEE. " Master's Thesis, University of Tennessee, 2018. https://trace.tennessee.edu/utk_gradthes/5375 This Thesis is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Masters Theses by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a thesis written by Trenton Joel Walker entitled "DETAILED GEOLOGIC MAPPING OF THE PARKSVILLE 7.5-MINUTE QUADRANGLE AND THE KINEMATICS OF EMPLACEMENT OF LARGE HORSES ALONG THE GREAT SMOKY FAULT, SOUTHEASTERN TENNESSEE." I have examined the final electronic copy of this thesis for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Master of Science, with a major in Geology. Robert D. Hatcher Jr., Major Professor
    [Show full text]
  • Geology of the Western Great Smoky Mountains Tennessee
    Geology of the Western Great Smoky Mountains Tennessee GEOLOGICAL SURVEY PROFESSIONAL PAPER 349-D Geology of the Great Smoky Mountains Tennessee and North Carolina GEOLOGICAL SURVEY PROFESSIONAL PAPER 349 This volume was published in separate chapters, A D Geology of the Western Great Smoky Mountains Tennessee By ROBERT B. NEUMAN and WILLIS H. NELSON GEOLOGY OF THE GREAT SMOKY MOUNTAINS, TENNESSEE AND NORTH CAROLINA GEOLOGICAL SURVEY PROFESSIONAL PAPER 349-D Interpretation of geologic history from late Precambrian on, based on mapping in and around the western part of the Great Smoky Mountains National Park UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1965 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract______-------_---_-_______________ Dl Devonian System.______________________-----------_ D40 Introduction ________________________________ 2 Upper Devonian Series._________________________ 40 Location.._ ___-___-___--_--_____________ 2 Chattanooga Shale__________________________ 40 Geography._____________________________ 3 Mississippian System-___________-__-___---_---__--_- 41 Physiography _______________________ 3 Lower Mississippian Series_______________________ 41 Human geography ___________________ 3 Grainger Formation.._______________________ 41 Fieldwork_ __ __________________________ 4 Upper Mississippian Series_______________________
    [Show full text]