DOCSLIB.ORG

Paleozoic Stratigraphy and Stucture of the Dry Creek Area, Elko And

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Paleozoic Stratigraphy and Stucture of the Dry Creek Area, Elko And AN ABSTRACT OF THE THESIS OF Robert Vincent Visconti for the degree of Master of Science in Geology presented on December 9, 1982 Title: PALEOZOIC STRATIGRAPHY AND STRUCTURE OF THE DRY CREEK AREA, ELKO AND EUREKA COUNTIES, NEVADA. Abstract approved: Redacted for Privacy C) Dr. J.Gljohnson The purpose of this investigation was to test two hypotheses. The first hypothesis interprets allochthonous rocks in the southern Pinyon Range to lie on the Devonian Nevada Group. The second hypothesis interprets allochthonous rocks to lie on the Mississippian Dale Canyon Formation. Evidence presented here supports the second hypothesis. During Late Silurian to Middle Devonian time, deposition in the southern Pinyon Range occurred in a miogeoclinal shallow shelf environment characterized by the Lone Mountain Dolomite and Nevada Group. Deposition of the Pilot Shale in an incipient basin developed within the shelf, beginning no later,than marginifera-Lower velifer Zone time, marked the onset of the Antler orogeny. A westward- dipping subduction zone formed to the west, developing an accretionary wedge which later became the Roberts Mountains allochthon. Incipient subduction of continental crust resulted in obduction of the allochthon onto the continential crust. The Antler foreland basin formed east of the advancing allochthon where deposition of the Dale Canyon Formation unconformably on the Pilot Shale formed a submarine fan complex consisting of siliciclastic sediments shed from the rising allochthon. The Roberts Mountains allochthon in the southern Pinyon Range consists of the Devonian Woodruff Formation forming the base, the Ordovician Vinini Formation thrust over the Woodruff, with slices of the Devonian Roberts Mountains Formation occurring in between at places. The allochthon was emplaced in the southern Pinyon Range, over the Dale Canyon Formation during or after late isosticha-Upper crenulata Zone time. Paleozoic Stratigraphy and Structure of the Dry Creek Area, Elko and Eureka Counties, Nevada by Robert Vincent Visconti A THESIS submitted to Oregon State University in partial fulfillment of the requirements for the degree of Master of Science Completed December 9, 1982 Commencement June 1983 APPROVED: Redacted for Privacy Professor in charge of major Redacted for Privacy Chairman of Department of7blogy Redacted for Privacy Dean of Grad e School d Date thesis is presented December 9, 1982 Typed by Heidi W. Pearson for Robert Vincent Visconti ACKNOWLEDGEMENTS I am grateful to many people for their help in this project. The guidance and encouragement given by Dr. J.G. Johnson was deeply appreciated. I thank Dr. E. Julius Dasch and Dr. Harold Demarest for their critical review of the manuscript. Claudia Regier prepared the conodont samples, which were identified by Dr. Gilbert Klapper of the University of Iowa. A coral was identified by Dr. William Oliver of the U.S. Geological Survey. Graptolites were identified by Dr. W.B.N. Berry of the University of California at Berkeley. Dr. Keith B. Ketner of the U.S. Geological Survey provided an interesting field trip and discussion. Dr. Donald Carlisle and Dr. C.A. Nelson of the University of California at Los Angeles provided a copy of their unpublished map of the Mineral Hill quadrangle and unpublished fossil data. I thank John Whitaker for many helpful discussions and car pooling into town during the field season. I thank my parents for their support and patience. A National Science Foundation grant to Dr. J.G. Johnson provided much of the financial support. TABLE OF CONTENTS Page INTRODUCTION 1 Purpose 1 Location and Accessibility 1 Previous Work 2 Methods and Terminology 5 GEOLOGIC SETTING 7 VININI FORMATION (ALLOCHTHONOUS) 9 ROBERTS MOUNTAINS FORMATION (ALLOCHTHONOUS) 12 WOODRUFF FORMATION (ALLOCHTHONOUS) 13 General Statement 13 Age 13 Lithology 14 Laminated quartz-silty dolomite and bioturbated dolomitic siltstone 14 Chert 14 Partially dolomitized biomicrite 16 Siliceous mudstone 16 Depositional Environment and Regional Significance 16 LONE MOUNTAIN DOLOMITE (AUTOCHTHONOUS) 19 NEVADA GROUP (AUTOCHTHONOUS) 20 Beacon Peak Dolomite 20 Oxyoke Canyon Sandstone 21 Telegraph Canyon Formation 21 Lithology 22 Silicification 23 PILOT SHALE (AUTOCHTHONOUS) 25 General Statement 25 Thickness and Contact Relations 25 Age 26 Lithology 26 Page Lower member 26 Upper member 28 Silicified shale 28 Depositional Environment 32 Regional Significance 32 DALE CANYON FORMATION (AUTOCHTHONOUS) 34 General Statement 34 Age 35 Contact Relations and Thickness 35 Facies Interpretation 36 Basin slope facies 36 Inner fan facies 38 Lithology 38 Chert-arenite 33 Pebbly chert-wacke 41 Fine grained rocks 41 Coarse-grained debris flow deposits 46 Regional Significance 46 INTRUSIVE ROCKS 48 LANDSLIDE DEPOSITS 49 STRUCTURE 50 GEOLOGIC HISTORY 53 SUMMARY 55 REFERENCES CITED 58 APPENDIX 62 LIST OF FIGURES Figure Page 1. Index map of the Pinyon Range. 3 2. Summary Paleozoic stratigraphic section of the mapped area. 4 3. Photomicrograph of bedded chert (Ordovician). 11 4. Photomicrograph of laminated quartz-silty dolomite 15 (Devonian). 5. Photomicrograph of partially dolomitized biomicrite 17 (Devonian). 6. Photomicrograph of jasperoid in the Telegraph Canyon 24 Formation. 7. Photomicrograph of laminated quartz-silty dolomite 27 (Devonian). 8. Photomicrograph of laminated carbonaceous shaly 29 dolomite (Devonian). 9. Silicified Pilot Shale. 30 10. Photomicrograph of silicified shale (Devonian). 31 11. Channel filled with coarse sandstone, basin slope facies 37 of the Dale Canyon Formation. 12. Amalgamated massive sandstone beds (Mississippian). 39 13. Unconformable contact between the Pilot Shale and 40 Dale Canyon Formation. 14. Photomicrograph of chert-arenite (Mississippian). 42 15. Photomicrograph of pebbly chert-wacke (Mississippian). 43 16. Photomicrograph of carbonaceous spicular biomicrite 44 (Mississippian). 17. Photomicrograph of coarse-grained debris flow 45 conglomerate (Mississippian). Figure Page 18. Comparative geologic cross sections along Dry Creek 56 LIST OF PLATES Plate Page I. Geologic map of the Dry Creek Area, Elko and pocket Eureka Counties, Nevada. 2. Geologic cross sections. pocket PALEOZOIC STRATIGRAPHY AND STRUCTURE OF THE DRY CREEK AREA, ELKO AND EUREKA COUNTIES, NEVADA INTRODUCTION Purpose The Paleozoic rocks in the vicinity of Dry Creek, Sulphur Spring and Pinyon Ranges, are in several elongate fault blocks across and subparallel to the toe of the Roberts Mountains thrust. Published and unpublished geologic maps (Smith and Ketner, 1978; Carlisle and Nelson, ms) interpret allochthonous rocks to lie below the Chainman Shale or Chainman-Diamond Peak Formation, undivided. However, Johnson and Pendergast (1981) interpret the same maps to show the allochthon over- lying the Chainman Shale. Remapping of the critical area was done to test the two hypotheses. The Dry Creek area also includes the "Dry Creek fault", recently proposed (Thorman and Ketner, 1979) as an important left-lateral strike- slip fault zone. Johnson (oral commun., 1981) suggests that there is no strike-slip fault zone and that it also is a misinterpretation. These two hypotheses are also tested. Location and Accessibility The area mapped is located approximately 33 miles south of the town 2 of Carlin, lying along the boundary of Elko and Eureka Counties, Nevada. It includes the southwestern edge of the Pinyon Range and the northern tip of the Sulphur Spring Range (Fig. 1). The area mapped occupies roughly 13 square miles (34 square kilometers). Access may be gained from the west on three unimproved dirt roads leading east from Union Summit Road. Previous Work Carlisle and Nelson (ms) mapped the southern one third of the thesis area as part of an unpublishedgeologic map of the MineralHill quadrangle. They mapped the allochthonous units as Ordovician Vinini Group (western facies), Devonian Bruffey Formation (transitionalfacies), and an.unnamed Devonian shale, all thrust over the autochthonous Silurian-Devonian Lone Mountain Dolomite, Devonian Nevada Group, and Devils Gate Limestone. The Mississippian Diamond Peak Formation-Chainman Shale undivided was mapped as overlapping the autochthonous and allochthonous units. Carlisle and Nelson (1955) did not assign an age to the Roberts Mountains thrust. Carlisle and others (1957) described Devonian stratigraphy of the Pinyon and Sulphur Spring Ranges with emphasis on the autochthonous carbonate units. Reconnaissance mapping of Elko County (Granger and others, 1958) included approximately the eastern three fourths of the thesis area. Smith and Ketner (1975, 1977) describe the Paleozoic stratigraphy and interpret the tectonic history of the Pinyon Range. The northern two thirds of the study area was mapped by Smith and Ketner (1978) as part of a U.S. Geological Survey map of the Pinyon Range. Smith and Ketner's mapping shows the same basic stratigraphic sequence as 3 CARLIN 1166 0 40°30' Map Area NEVADA DRY CREEK AREA 0 5 10 15 miles 1 Figure I. Index map of the Pinyon andSulphur Spring Ranges, showing the location of theDry-Creek Area. 4 AGE ROCK UNIT THICKNESS Ordovician Vinini Formation 1500 ft. A A A Roberts Mts. Fm 200 A A A Devonian Woodruff Formation 1200 A A Mississippian Dale Canyon Formation 1000 Pilot Shale . 200 Telegraph Canyon 2065 Formation Devonian Oxyoke Canyon Ss. 400 Beacon Peak Dolomite 675 Lone Mt. Dolomite 1400 Silurian Figure 2. Summary Paleozoic stratigraphic section of themapped area. 5 mapped by Carlisle and Nelson. The allochthonous units were mapped as Ordovician
Load more

Recommended publications
  • Quaternary Fault and Fold Database of the United States
    Jump to Navigation Quaternary Fault and Fold Database of the United States As of January 12, 2017, the USGS maintains a limited number of metadata fields that characterize the Quaternary faults and folds of the United States. For the most up-to-date information, please refer to the interactive fault map. Diamond Valley fault (Class A) No. 1161 Last Review Date: 2000-06-06 citation for this record: Anderson, R.E., compiler, 2000, Fault number 1161, Diamond Valley fault, in Quaternary fault and fold database of the United States: U.S. Geological Survey website, https://earthquakes.usgs.gov/hazards/qfaults, accessed 12/14/2020 02:17 PM. Synopsis The Diamond Valley fault is along the precipitous east-facing bedrock escarpment of the Sulphur Spring Range adjacent to Diamond Valley near the southeastern corner of the Winnemucca 1:250,000 map. It includes a subparallel 6-km-long fault along the east margin of Union Mountain in Elko County. The Sulphur Spring Range is an east-tilted structural block similar to many ranges in the region. The range is also a north-trending horst, and the Diamond Valley fault is the east-bounding structure of the horst. The precipitous, convex-eastward bedrock escarpment along the fault is little incised by transverse drainages, and generally lacks the faceted spurs and wineglass valleys that tend to characterize the geomorphology of major active range blocks. The fault probably juxtaposes Quaternary alluvium against bedrock, but fault scarps and (or) lineaments on Quaternary surficial deposits or erosion surfaces are apparently lacking. Name Modified from dePolo (1998 #2845), who applied the name comments Diamond Valley fault zone to a single-trace north-striking fault mapped by Dohrenwend and Moring (1991 #282) at the base of the precipitous east-facing bedrock escarpment of the Sulphur Spring Range adjacent to Diamond Valley.
    [Show full text]
  • Size Distribution of the Late Devonian Ammonoid Prolobites: Indication for Possible Mass Spawning Events
    Swiss J Geosci (2010) 103:475–494 DOI 10.1007/s00015-010-0036-y Size distribution of the Late Devonian ammonoid Prolobites: indication for possible mass spawning events Sonny Alexander Walton • Dieter Korn • Christian Klug Received: 17 December 2009 / Accepted: 18 October 2010 / Published online: 15 December 2010 Ó Swiss Geological Society 2010 Abstract Worldwide, the ammonoid genus Prolobites is Abbreviations only known from a few localities, and from these fossil SMF Senckenberg Museum, Frankfurt a. M., Germany beds almost all of the specimens are adults as shown by the MB.C. Cephalopod collection of the Museum fu¨r presence of a terminal growth stage. This is in marked Naturkunde Berlin (the collections of Franz contrast to the co-occurring ammonoid genera such as Ademmer, Werner Bottke, and Harald Simon Sporadoceras, Prionoceras, and Platyclymenia. Size dis- are incorporated here) tribution of specimens of Prolobites from three studied localities show that, unlike in the co-occurring ammonoid species, most of the material belongs to adult individuals. The morphometric analysis of Prolobites delphinus Introduction (SANDBERGER &SANDBERGER 1851) demonstrates the intra- specific variability including variants with elliptical coiling The mid-Fammenian (Late Devonian) ammonoid genus and that dimorphism is not detectable. The Prolobites Prolobites is only known from a few localities worldwide, material shows close resemblance to spawning populations mainly in the Rhenish Mountains and the South Urals. of Recent coleoids such as the squid Todarodes filippovae Where it does occur, the majority of the specimens show a ADAM 1975. Possible mass spawning events are discussed terminal growth stage suggesting that these are adults.
    [Show full text]
  • Paleozoic Geology of the Dobbin Summit-Clear Creek Area, Monitor
    AN ABSTRACT OF THE THESIS OF DIANE CAROL WISE for the degree of MASTER OF SCIENCE in Geology presented on August 13, 1976 Title: PALEOZOIC GEOLOGY OF THE DOBBIN SUMMIT- CLEAR CREEK AREA, MONITOR RANGE, NYiE COUNTY, NEVADA Abstract approved: Redacted for Privacy son Paleozoic limestones, dolomites, quartz arenites, and other clastic rocks were mapped in the vicinity of Dobbin Summit and Clear Creek in the central Monitor Range. Sedimentary rock units present in this area represent the shallow-shelf eastern assemblage and basin and also the basin-slope facies of the traditional limestone- clastic assemblage. The four oldest, Ordovician, units were deposited in shallow shelf environments. The Lower Ordovician Goodwin Formation is composed of about 1200 feet of calcareous shales and thin-bedded limestones. The overlying Antelope Valley Limestone is about 500 feet thick and consists of wackestones, packstones, and rare algal grainstones.The Copenhagen Formation (135 feet thick) is the highest regressive deposit of sandstone, siltstone, and limestone below the transgressive Eureka Quartzite.The Eureka is a quartz arenite 181 feet thick, with an intercalated shallow marine dolomite member. The transition from shallow to deep water conditions can be seen in the change from algal boundstones to laminated lime mud- stones in the Hanson Creek Formation (190 feet thick).The super- jacent Roberts Mountains Formation (285 feet thick) is composed of lime mudstones and allodapic beds deposited in basinal, deep water conditions.During earliest Devonian
    [Show full text]
  • Detrital Zircon U-Pb Geochronology and Hf Isotope Geochemistry of the Roberts Mountains Allochthon: New Insights Into the Early GEOSPHERE; V
    Research Paper GEOSPHERE Detrital zircon U-Pb geochronology and Hf isotope geochemistry of the Roberts Mountains allochthon: New insights into the early GEOSPHERE; v. 12, no. 3 Paleozoic tectonics of western North America doi:10.1130/GES01252.1 Gwen M. Linde1, James H. Trexler, Jr.1, Patricia H. Cashman1, George Gehrels2, and William R. Dickinson2,* 12 figures; 2 tables; 2 supplemental tables 1Department of Geological Sciences and Engineering, University of Nevada, Reno, Nevada 89557-0172, USA 2Department of Geosciences, University of Arizona, Tucson, Arizona 85721-0077, USA CORRESPONDENCE: gwenlinde@ yahoo .com CITATION: Linde, G.M., Trexler, J.H., Jr., Cashman, ABSTRACT et al., 1958; Burchfiel and Davis, 1972; Madrid, 1987). Various workers have P.H., Gehrels, G., and Dickinson, W.R., 2016, Detrital zircon U-Pb geochronology and Hf isotope suggested wildly disparate sources for the RMA strata. Some workers (e.g., geochemistry of the Roberts Mountains allochthon: Detrital zircon U-Pb geochronology and Hf isotope geochemistry provide Roberts et al., 1958; Burchfiel and Davis, 1972; Poole et al., 1992) suggested New insights into the early Paleozoic tectonics of new insights into the provenance, sedimentary transport, and tectonic evo- that the RMA strata originated in western Laurentia (Fig. 1) and deposited in western North America: Geosphere, v. 12, no. 3, p. 1016–1031, doi:10.1130/GES01252.1. lution of the Roberts Mountains allochthon strata of north-central Nevada. an ocean basin to the west. Speed and Sleep (1982) hypothesized that the RMA Using laser-ablation inductively coupled plasma mass spectrometry, a total of strata are the accretionary prism of a far-traveled arc.
    [Show full text]
  • F I N a L Mineral Assessment Report
    BLM F I N A L MINERAL ASSESSMENT REPORT Battle Mountain District Office - Nevada J A N U A R Y 2 0 1 2 This page intentionally left blank Bureau of Land Management Mineral Assessment Report SUMMARY The Bureau of Land Management (BLM) Battle Mountain District Office (BMDO) is in the process of revising the district’s Resource Management Plan (RMP). As part of the RMP revision process, the BLM is required to prepare a Mineral Assessment Report providing information regarding mineral occurrences and potential within the BMDO Planning Area (planning area). This report provides an intermediate level of detail for mineral assessment as prescribed in BLM Manual 3060 (BLM 1994). Information presented in this report will be summarized and incorporated into an Environmental Impact Statement (EIS) for the proposed RMP and into the final RMP. The geologic history of central and southern Nevada and the planning area is very complex and includes two major cycles of sedimentation (western and eastern facies sources), episodic thrust faulting, mountain building, and associated intrusive and igneous activity. More recent geologic history includes a period of crustal extension that was accompanied by bimodal (rhyolite-basalt) volcanism, large volume caldera volcanism, and basin and range block-faulting resulting in high-levels of shallow crustal heat flow. The regional and local geologic setting has been instrumental in the location of and potential for numerous economic metallic mineral deposits in the planning area, as well as development of economic geothermal resources. MINING AND MINERAL ACTIVITY IN NEVADA Mineral exploration, particularly for gold, is an ongoing enterprise in Nevada by both operators of existing mines and by other exploration companies.
    [Show full text]
  • Mineral Potential Report
    FRTC Modernization EIS Supporting Study Mineral Potential Report This Page Intentionally Left Blank REPORT Mineral Potential Report for the Fallon Range Training Complex Modernization for ManTech International Corporation Submitted to: ManTech International Corporation 420 Stevens Avenue, Suite 300 Solana Beach, California 92075 Submitted by: Golder Associates Inc. +1 520 888-8818 18108941 November 2018 November 2018 18108941 Executive Summary This Mineral Potential Report (MPR) has been prepared to support an Environmental Impact Statement (EIS) for the land withdrawal extension and expansion at the Naval Air Station (NAS) Fallon Range Training Complex (FRTC), in Churchill, Lyon, Mineral, Nye, and Pershing Counties, Nevada. This MPR is intended to be used as a planning tool that provides land managers with mineral resource information to develop management plans. The FRTC is part of the US Department of Navy (DON). The FRTC currently encompasses an area of 223,562 acres (ac). Figure ES.1 presents the areas involved. The FRTC consists of federal land that has been withdrawn from public use and reserved for military training and operations through the Military Lands Withdrawal Act of 1999, Public Law 106-65 (MLWA). The current withdrawal will expire in November 2021, unless Congress enacts legislation providing an extension. Withdrawal of additional lands to support DON activities in ranges B-16, B-17, B-20, and the DVTA may impact public and private lands including mining and geothermal leases, as well as access to mineral exploration and production infrastructure such as roads, pipelines, and temporary and fixed facilities. As part of the EIS process, the DON proposed three action alternatives for the land withdrawal extension and expansion for the FRTC.
    [Show full text]
  • STRATIGRAPHY and STRUCTURE of the SOUTHERN SULPHUR SPRING RANGE, EUREKA COUNTY, NEVADA Redacted for Privacy Abstract Approved: U G
    AN ABSTRACT OF THE THESES OF Joseph T. Lipka IC for the degree ofMaster of Sciencein Geology presented on April 17, 1987 Title:STRATIGRAPHY AND STRUCTURE OF THE SOUTHERN SULPHUR SPRING RANGE, EUREKA COUNTY, NEVADA Redacted for Privacy Abstract approved: U G. Johnson Early Paleozoic limestones and dolomites of the shallow shelf transitional facies belt were mapped in the southern Sulphur Spring Range, Eureka County, Nevada.The four youngest units in the map area are in fault contact with the Lower Devonian rocks and wereprobably transported westward, along a low-angle normal fault. The minoirlal dolomites of the Hanson Creek Formation, dated as latest Ordovician in the map area, were deposited in a low-energy lagoon.Overlying the Hanson Creek Formation, with a gradational contact, is the lower member ofthe Lone Mountain Dolomite, a probable reef complex.The exposed thickness of the lower Lone Mountain Dolomite is estimated to be 250 feet.The Lower Devonian Old Whalen Member of the Lone Mountain Dolomite is composed of well-bedded, alternating brown and gray dolomites.The repetition of rock types in the Old Whalen Member indicates recurring shallow marine environments on a broad carbonate platform.The Old Whalen is estimated to be 1400 feet thick.Directly overlying the Old Whalen Member, is the Kobeh Member of the Mc Colley Canyon Formation.Rocks of the Mc Colley Canyon Formation were deposited on a shallow shelf under normal marine conditions.The mid-Lower Devonian Kobeh Member is sparsely to abundantly fosciliferous and varies from a peloidal wackestone to a peloidal sandy wackestone to a sandy peloidal packstone.The thickness is 276 feet.Overlying the Kobeh Member are the abundantly fossiliferous beds of the lower part of the Bartine.
    [Show full text]
  • Ordovician News 2005
    ORDOVICIAN NEWS SUBCOMMISSION ON ORDOVICIAN STRATIGRAPHY INTERNATIONAL COMMISSION ON STRATIGRAPHY Nº 22 2005 ORDOVICIAN NEWS Nº 22 INTERNATIONAL UNION OF GEOLOGIAL SCIENCES President: ZHANG HONGREN (China) Vice-President: S. HALDORSEN (Norway) Secretary General: P. T. BOBROWSKI (Canada) Treasurer: A. BRAMBATI (Italy) Past-President: E.F.J. DE MULDER (The Netherlands) INTERNATIONAL COMMISSION ON STRATIGRAPHY Chairman: F. GRADSTEIN (Norway) Vice-Chairman: S. C. FINNEY (USA) Secretary General: J. OGG (USA) Past-Chairman: J. REMANE (Switzerland) INTERNATIONAL SUBCOMMISSION ON ORDOVICIAN STRATIGRAPHY Chairman: CHEN XU (China) Vice-Chairman: J. C. GUTIÉRREZ MARCO (Spain) Secretary: G. L. ALBANESI (Argentina) F. G. ACEÑOLAZA (Argentina) A. V. DRONOV (Russia) O. FATKA (Czech Republic) S. C. FINNEY (USA) R. A. FORTEY (UK) D. A. HARPER (Denmark) W. D. HUFF (USA) LI JUN (China) C. E. MITCHELL (USA) R. S. NICOLL (Australia) G. S. NOWLAN (Canada) A. W. OWEN (UK) F. PARIS (France) I. PERCIVAL (Australia) L. E. POPOV (Russia) M. R. SALTZMAN (USA) Copyright © IUGS 2005 i ORDOVICIAN NEWS Nº 22 CONTENTS Page NOTE FOR CONTRIBUTORS iii EDITOR'S NOTE iii CHAIRMAN´S AND SECRETARY´S ADDRESSES iii CHAIRMAN´S REPORT 1 SOS ANNUAL REPORT FOR 2001 1 INTERNATIONAL SYMPOSIA AND CONFERENCES 4 PROJECTS 7 SCIENTIFIC REPORTS 7 HONORARY NOTES 8 MISCELLANEA 9 CURRENT RESEARCH 9 RECENT ORDOVICIAN PUBLICATIONS 25 NAMES AND ADDRESS CHANGES 40 URL: http://www.ordovician.cn, http://seis.natsci.csulb.edu/ISOS Cover: The Wangjiawan GSSP for the base of the Hirnantian Stage, China. ii ORDOVICIAN NEWS Nº 22 NOTE FOR CONTRIBUTORS The continued health and survival of Ordovician News depends on YOU to send in items of Ordovician interest such as lists and reviews of recent publications, brief summaries of current research, notices of relevant local, national and international meetings, etc.
    [Show full text]
  • Back Matter (PDF)
    Index Page numbers in italic denote Figures. Page numbers in bold denote Tables. Acadian Orogeny 224 Ancyrodelloides delta biozone 15 Acanthopyge Limestone 126, 128 Ancyrodelloides transitans biozone 15, 17,19 Acastella 52, 68, 69, 70 Ancyrodelloides trigonicus biozone 15, 17,19 Acastoides 52, 54 Ancyrospora 31, 32,37 Acinosporites lindlarensis 27, 30, 32, 35, 147 Anetoceras 82 Acrimeroceras 302, 313 ?Aneurospora 33 acritarchs Aneurospora minuta 148 Appalachian Basin 143, 145, 146, 147, 148–149 Angochitina 32, 36, 141, 142, 146, 147 extinction 395 annulata Events 1, 2, 291–344 Falkand Islands 29, 30, 31, 32, 33, 34, 36, 37 comparison of conodonts 327–331 late Devonian–Mississippian 443 effects on fauna 292–293 Prague Basin 137 global recognition 294–299, 343 see also Umbellasphaeridium saharicum limestone beds 3, 246, 291–292, 301, 308, 309, Acrospirifer 46, 51, 52, 73, 82 311, 321 Acrospirifer eckfeldensis 58, 59, 81, 82 conodonts 329, 331 Acrospirifer primaevus 58, 63, 72, 74–77, 81, 82 Tafilalt fauna 59, 63, 72, 74, 76, 103 ammonoid succession 302–305, 310–311 Actinodesma 52 comparison of facies 319, 321, 323, 325, 327 Actinosporites 135 conodont zonation 299–302, 310–311, 320 Acuticryphops 253, 254, 255, 256, 257, 264 Anoplia theorassensis 86 Acutimitoceras 369, 392 anoxia 2, 3–4, 171, 191–192, 191 Acutimitoceras (Stockumites) 357, 359, 366, 367, 368, Hangenberg Crisis 391, 392, 394, 401–402, 369, 372, 413 414–417, 456 agnathans 65, 71, 72, 273–286 and carbon cycle 410–413 Ahbach Formation 172 Kellwasser Events 237–239, 243, 245, 252
    [Show full text]
  • The Stratigraphic Section in the Vicinity of Eureka, Nevada
    The Stratigraphic Section in the Vicinity of Eureka, Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 276 The Stratigraphic Section in the Vicinity of Eureka, Nevada By T. B. NOLAN, C. W. MERRIAM, and J. S. WILLIAMS GEOLOGICAL SURVEY PROFESSIONAL PAPER 276 Revision of the pre- Tertiary stratigraphy of east-central Nevada UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1956 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.00 (paper cover) CONTENTS Page Page Abstract_ _____________________ 1 Silurian system.___________________________ 36 Introduction. _--___-______--___- 2 Roberts Mountains formation.__________ 36 Acknowledgments- --.-_---___-_-. 3 Lone Mountain dolomite__________... 37 Structural setting._______________ 3 Devonian system.__________-_-_-__--_____. 40 Economic significance. _-__._. 5 Nevada formation_________--______--. 40 Cambrian system.________________ 5 Beacon Peak dolomite member. 42 Prospect Mountain quartzite.. 6 Oxyoke Canyon sandstone member... 43 Pioche shale_______--_-_-_.__. 7 Sentinel Mountain dolomite member. 43 Eldorado dolomite___________ 9 Woodpecker limestone member. 44 Geddes limestone.___________ 11 Bay State dolomite member.--...--. 45 Secret Canyon shale._________ 12 Devils Gate limestone._________________ 48 Lower shale member. .... 13 Meister member.__________________ 49 Hayes Canyon member.____________ 49 Clarks Spring member.._ 14 Devonian and Mississippian systems. ________ 52 Hamburg dolomite.___-_.____ 16 Pilot shale________-__-_-___--__---_-_. 52 Dunderberg shale.___________ 18 Carboniferous systems_.____-__-______-__- 54 Windfall formation.__________ 19 Mississippian system._________--,___-_- 54 Catlin member._________ 20 Joana limestone,___________________ 54 Bullwhacker member.
    [Show full text]
  • Acta Geologica Polonica, Vol
    Acta Geologica Polonica, Vol. 50 (2000), No. 1, pp. 21-27 Mantle expansion upon the conch in the Late Devonian ammonoid Erfoudites DIETER KORN Institut und Museum für Geologie und Paläontologie der Eberhard-Karls-Universität Tübingen, Sigwartstraße 10, D-72076 Tübingen, Germany. E-mail: [email protected] ABSTRACT: KORN, D. 2000. Mantle expansion upon the conch in the Late Devonian ammonoid Erfoudites. Acta Geologica Polonica, 50 (1), 21-27. Warszawa. Specimens of the Late Devonian ammonoid species Erfoudites rugosus sp. nov. from the Rhenish Massif of Germany show an additional wrinkled structure that covers the body chamber ornament. The pattern closely resembles the dorsal wrinkle layer known from many ammonoids; the course of the wrinkles is radial, par- tially following the growth line course. This wrinkle structure is interpreted as resulting from a secretion of the mantle, which expanded ventrally or dorsally over the conch. Key words: Ammonoids, Erfoudites rugosus sp. nov., Germany, Devonian. INTRODUCTION mens from the Hunsrück Shale (STÜRMER 1969, ZEISS 1969). However, interpretations of the materi- After many decades of using Recent Nautilus as al may be equivocal. The lack of information on a living example for hypotheses on ammonoid soft Palaeozoic ammonoids is particularly due to the fact body morphology and mode of life of ammonoids, that the recrystallisation of the shell wall only rarely many palaeontologists now prefer living squids as permits the investigation of ultrastructural features. better models. This is based on the view that Hence identification of different shell wall elements ammonoids may be more closely related to squids is usually prevented.
    [Show full text]
  • Sepkoski, J.J. 1992. Compendium of Fossil Marine Animal Families
    MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. Department of the Geophysical Sciences University of Chicago Chicago, Illinois 60637 Milwaukee Public Museum Contributions in Biology and Geology Rodney Watkins, Editor (Reviewer for this paper was P.M. Sheehan) This publication is priced at $25.00 and may be obtained by writing to the Museum Gift Shop, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Orders must also include $3.00 for shipping and handling ($4.00 for foreign destinations) and must be accompanied by money order or check drawn on U.S. bank. Money orders or checks should be made payable to the Milwaukee Public Museum. Wisconsin residents please add 5% sales tax. In addition, a diskette in ASCII format (DOS) containing the data in this publication is priced at $25.00. Diskettes should be ordered from the Geology Section, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Specify 3Y. inch or 5Y. inch diskette size when ordering. Checks or money orders for diskettes should be made payable to "GeologySection, Milwaukee Public Museum," and fees for shipping and handling included as stated above. Profits support the research effort of the GeologySection. ISBN 0-89326-168-8 ©1992Milwaukee Public Museum Sponsored by Milwaukee County Contents Abstract ....... 1 Introduction.. ... 2 Stratigraphic codes. 8 The Compendium 14 Actinopoda.
    [Show full text]