Stratigraphy of Paleozoic Rocks in the Carlin-Pinon Range Area, Nevada

Total Page:16

File Type:pdf, Size:1020Kb

Stratigraphy of Paleozoic Rocks in the Carlin-Pinon Range Area, Nevada ' I' .._- .... ~ : Stratigraphy of Paleozoic Rocks in the Carlin-Pinon Range Area, Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 867-A Prepared in cooperation with Nevada Bureau of Mines and Geology f:.:. ~, ' n" : . ' ,'_ Stratigraphy of Paleozoic Rocks in the Carlin-Pinon Range Area, Nevada By J. FRED SMITH, JR., and KEITH B. KETNER GEOLOGY OOF THE CARLIN-PINON RANGE AREA, NEVADA GEOLOGICAL SURVEY PROFESSIONAL PAPER 867-A Prepared in cooperation with Nevada Bureau of Mines and Geology UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Smith, Joe Fred, 1911- Stratigraphy of Paleozoic rocks in the Carlin-Pinon Range area, Nevada. (Geology of the Carlin-Pinon Range area, Nevada) (Geological Survey Professional Paper 867-A) Bibliography: p. Includes index. 1. Geology, Stratigraphic-Paleozoic. 2. Geology-Nevada-Carlin region. I. Ketner, Keith Brindley, 1921- joint author. II. Nevada. Bureau of Mines. III. Title. IV. Series. V. Series: United States Geological Survey Professional Paper 867-A. QE654.S53 551. 7'2'0979316 74-31422 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02628-7 CONTENTS Page Page Abstract . A1 Rock formations-Continued Introduction . 3 Devonian System-Continued The Carlin-Pinon Range area . 3 Transitional assemblage . A32 Fieldwork and acknowledgment.:;....................... 5 Roberts Mountains Formation . 32 Previous work . 5 Limestone and chert unit . 34 Rock formations ...................................... ·. 5 Late Late Devonian-early Early Mississippian uncon- Ordovician System . 5 formity . 34 Carbonate (eastern) assemblage . 5 Mississippian System . 35 Pogonip Group (part) . 5 Webb Formation . 35 Eureka Quartzite............................. 6 Argillite unit of Lee Canyon....................... 38 Hanson Creek Formation . 6 Mississippian and Pennsylvanian Systems . 40 S'iliceous (western) assemblage . 9 Chainman Shale and Diamond Peak Formation . 40 Valmy Formation . 9 Chainman Shale . 40 Vinini Formation . 9 Diamond Peak Formation . 44 Transitional assemblage . 12 Composite measured section of the Diamond Peak For- Ordovician rocks of Marys Mountain . 12 mation and the Chainman Shale . 46 Silurian System . 14 Age and correlation of Diamond Peak Formation and Carbonate (eastern) assemblage . 14 Chainman Shale . 46 Lone Mountain Dolomite . 14 Pennsylvanian System . 51 Siliceous (western) assemblage . 17 Moleen Formation . 52 Silurian rocks of Marys Mountain . 17 Tomera Formation . 56 Devonian System . 18 Tomera and Moleen Formations undivided . 57 Carbonate (eastern) assemblage . 18 Middle Pennsylvanian unconformity . 57 Nevada Formation . 18 Pennsylvanian and Permian Systems . 58 Beacon Peak Dolomite Member . 21 Strathearn Formation . 59 Oxyoke Canyon Sandstone Member........ 22 Upper Pennsylvanian and Permian rocks Upper dolomite member . 24 undivided . 63 Devils Gate Limestone . 25 Depositional history . 74 Siliceous (western) assemblage . 27 References cited . 81 Woodruff Formation . 27 Index . 85 ILLUSTRATIONS Page PLATE 1. Generalized geologic map of Paleozoic rocks .................................................................. In pocket 2. Columnar sections of Upper Pennsylvanian and Permian rocks, Carlin-Pinon Range area ......................... In pocket FIGURE 1. Index map . A4 2. Map showing localities where Hanson Creek Formation and equivalent carbonate-assemblage roc,ks are exposed in the region 8 3. Photograph showing chert and some shale in the Vinini Formation . 10 4. Columnar section of Ordovician rocks on east side of Marys Mountain . 13 5. Correlation diagram of Devonian strata . 19 6. Map showing principal localities where Nevada Formation and probable equivalent carbonate-assemblage rocks are exposed 20 7. Photographs of part of the clawlike or jawlike rami of Angustidontus . 31 8. Map showing localities where transitional-assemblage Roberts Mountains Formation and equivalent carbonate-assemblage rocks are exposed in the region . 33 9. Map showing approximate thicknesses of the Webb Formation and the formations on which it lies . 36 10. Photograph showing Chainman Shale and argillite of Lee Canyon . 39 11. Map showing areas of prominent exposures of pebbly mudstone and of limestone pebbles and cobbles in the Chainman Shale and Diamond Peak Formation . 42 12. Photographs of pebbly mudstone in Chainman Shale . 43 13. Photograph showing angular unconformity between Diamond Peak Formation and overlying Strathearn Formation . 58 14. Sketch map showing outcrops and general lithologic types of Upper Pennsylvanian and Permian rocks . 60 15. Sketch map showing outcrops and ages of basal beds of Upper Pennsylvanian and Permian rocks . 62 16. Sketch section illustrating westward onlap of Upper Pennsylvanian and Permian rocks . 70 17. Map showing approximate position of east-to-west change from mostly dolomite to limestone for several Paleozoic formations 76 III IV CONTENTS TABLES Page TABLE 1. Graptolite collections from the Vinini Formation along the north side of Willow Creek . All 2. Graptolites from the Vinini Formation . 12 3. Graptolites from the Ordovician rocks on Marys Mountain . 15 . 4. Chemical analyses of nodules from the Woodruff Formation . 28 5. Conodonts collected from the Woodruff Formation and from the transitional limestone and chert unit . 28 6. Analyses of carbonate, calcium, and magnesium and Ca/Mg molal ratios of 11 rock samples from the Woodruff Formation 30 7. Conodonts from the Webb Formation ........................................................................ ."... 37 8. Semiquantitative spectrographic analyses of solid bitumen by the laser-fired method . 44 9. Fossils of Early Mississippian age (Kinderhookian Series) from the Chainman Shale and the undivided Chainman Shale and Diamond Peak Formation . 49 10. Fossils of late Early (Osagean Series) and possibly early Late (early Meramecian Series) Mississippian age . 50 11. Diaphragmus phillipsi assemblage of late Late Mississippian age . 51 12. Fossils of Early Pennsylvanian age from the upper part of the Diamond Peak Formation . 51 13. Fossils of Pennsylvania~ age from the Moleen and Tomera Formations . 53 14. Names applied to Upper Pennsylvanian and Permian rocks in the area of Carlin Canyon . 59 15. Analyses of calcium and magnesium and Ca/Mg molal ratios of some Upper Pennsylvanian and Permian rocks . 65 16. Late Pennsylvanian Foraminifera from lower part of Stratheam Formation and equivalent beds . 71 17. Pennsylvanian(?)-Permian Foraminifera from middle part of Strathearn Formation and equivalent beds . 72 18. Early Permian Foraminifera from the upper part of the Strathearn Formation and equivalent beds . 72 19. Early Permian Foraminifera from undivided beds above the Stratheam Formation . 73 MEASURED STRATIGRAPHIC SECTIONS Page SECTION Sl. Lone Mountain Dolomite northeast of Bunker Hill in W 1/2 sec. 3, T. 30 N., R. 53 E .............................. A16 S2. Lone Mountain Dolomite on.
Recommended publications
  • Late Carboniferous Bryozoans from La Hermida, Spain
    Late Carboniferous bryozoans from La Hermida, Spain Andrej Ernst and Elke Minwegen Acta Palaeontologica Polonica 51 (3), 2006: 569-588 Fifteen bryozoan species belonging to thirteen genera have been identified from an outcrop of the Picos de Europa Formation (Moscovian, Upper Carboniferous) at La Hermida in northern Spain. Three species and one genus are new Coscinium hermidensis sp. nov., Cystodictya pustulosa sp. nov., and Cystocladia hispanica gen. et sp. nov. Rhabdomesid bryozoans are the most diverse order with seven species, followed by cystoporids (four species), fenestellids (three species) and trepostomids (one species). Bryozoans with erect branched or reticulate colonies dominate in the studied assemblage; only two species possess encrusting colonies. Together with associated crinoids, the bryozoan assemblage indicates a subtidal environment below the zone of vigorous water movement. The La Hermida bryozoan fauna confirms the Upper Carboniferous age of the Picos de Europa Formation and allows various biogeographical interpretations. All previously known species of the genus Coscinium were reported from the Lower Permian of Russia. Clausotrypa monticola is known from the Lower Permian of Russia and Arctic as well as from the Upper Carboniferous of Carnic Alps (Austria). Rhabdomeson cf. propatulissimum and Penniretepora pseudotrilineata are known from the same level of Italian Carnic Alps. Streblotrypa (Streblascopora ) nikiforovae and Rhombocladia punctata are known from the Upper Carboniferous (Moscovian) of Ukraine. Fistulipora petaloida is known from Kasimovian Stage of Russian Plate. Several other species show connections with North America. Key words: Bryozoa, Cystoporida, Fenestellida, Carboniferous, Picos de Europa Formation, Spain. Andrej Ernst [email protected], Institut für Geowissenschaften, Christian-Albrechts-Universität zu Kiel, Ludewig-Meyn-Str.
    [Show full text]
  • Paleozoic Biostratigraphy and Paleontology Along the Mogollon Rim, Arizona
    PALEOZOIC BIOSTRATIGRAPHY AND PALEONTOLOGY ALONG THE MOGOLLON RIM, ARIZONA This one-day field trip permits examination of Devonian, Pennsyl­ vanian, and Permian stratigraphy and biostratigraphy. Pennsylvanian and Permian fossil localities will also be visited. The field trip guide consists of three separate articles. These involve, in order, paleontology, stratigraphy, and a road log. The road log from Payson to Pine, on pages 34-36 of the New Mexico Geological Society Thirteenth Field Conference Guidebook (1962), might also prove useful. PALEONTOLOGY OF THE NACO FORMATION IN THE KOHL RANCH AREA, ARIZONA by Stanley S. Beus NorthernArizona University and Douglas C. Brew University of Minnesota This trip will traver-se part of the Basin and Range Province north­ east of Tempe and end up in the transition zone between the Basin and Range and Colorado Plateau provinces below the Mogollon Rim. The total distance is about 230 miles. We will examine outcrops of Devonian through Permian age, and collect Devonian, Pennsylvanian and Permian fossils. The major col­ lecting site will be in the Naco Formation near Kohl Ranch, discussed below. Possible localities are indicated in figure 1. GENERAL STRATIGRAPHY lenses. The lower unbedded portion is generally interpreted to represent a regolith formed in situ via solution of the The Naco formation of central Arizona is a predom­ Redwall Limestone, whereas the upper portion consists inantly marine sequence of interbedded limestones and predominantly of insoluble residues reworked by marine or terrigenous sedimentary rocks of Pennsylvanian age. The perhaps both nonmarine and marine agencies (Huddle and formation is separated from the underlying Mississippian Dobrovolny, 1945, 1952; Brew, 1970; McKee and Redwall Limestone by a conspicuous regional disconfor­ Gutschick, 1969).
    [Show full text]
  • LZ Streets County Boundary Printed 4/23/2018 ®
    H R A I L R FR526 D A R G R HORSE SAD I DLE M SO E A A AP 9 STO RIN M N NE G 8 R TAIL RAN P I CH R E O O HORN L BUFFALO C C E O C TW K W A V O T O F N E B H R R C R W E RAWA S DIAMOND PEAK LZ AR E 2 A L E S A D 0 A V S 2 M O K L E A WALNO C R O B F B E O C M R N # K R * N E L I D W R A A E C G L K O D N T A A O D BIG HOLE A E S C N R R E A R R P H N E I E F D R B 8 E R Y R 9 V O P R L F SOAPSTONE PRAIRIE NA NORTH LOT LZ P O F S T R E C C A Y D U U H IX D Y W T M K A C D B L K W E S N F # N * M N T F E A S U L O Y Y IT A O L T M S B N O E Y Y V E M C O B R S D N R K O W A R I I A E N E O A R L R N E H I C IG L C L R W R AN I G 4 W E T D S E C S P F A B 3 R R N 7 A I E U T 8 NG I P F P N S G E R A Q O R F S L R L T H C T I S Y P R V 6 I E F C 4 0 I S N 5 A 2 O N E C D A D S R R C L G R 3 F N R G D 1 W T E N 2 U R N S 0 AIL L E I E O C R RED MOUNTAIN OPEN SPACE LZ K 3 RE K K O A O EK R L E M C Z R M N TIM P L N E BER # S E *N O C G T W H I O K R L N N Y E E N L O K H E C I C N C R L A Y C O I I C L H A O V T L P CR80C & FR87C LZ T E VIRGINIA DALE LZ I N A R G C N R RA ED O N J E E A A L P A R I S SH W E L 2 B R C F Y E R A T *# *# P F 8 1 S H C R C A D 8 O E 1 T A 7 E T A HOHNHOLZ LAKES LZ K R AT R E SOAPSTONE PRAIRIE NA SOUTH LOT LZ R V R N I C O R M M P E T R F F E I T 200 B U E W FR L E P # B S L E # * Y * R E K IN E T S C T I H L O 5 C N G K 4 E LS CREEK R I C DEVI D O F A 5 C N S D N E E W R EATON RESERVOIR LZ A I T F I N P U R E BE R A P E R K Q A D 5 R L 9 P *# N O V N K E I A T S T D L I M U D I CR80C MM 22 LZ L D M H E R E Y *# E C B V U R S L CR80C & CR89 LZ T L T DE D E M R S # W PA N E * A R T U L K HOMESTEAD LZ JOY A R N C 0 O J K CANYON O 4 E W A P HA F W 5 R R # L IV ROUND BUTTE LZ * X E R I ATE D F D M R CR92 W IV # B E * CH E E N L F A AN D R R H E R C 5 T J 2 O 3 R P R 1 .
    [Show full text]
  • Middle Permian Brachiopods from Setamai, the Type Locality of The
    Sci. Rep., Niigata Univ., Ser. E(Geology), No. 16, 1-33, 2001 Middle Permian brachiopods from Setamai,the type locality of the Kanokura Formation,southern Kitakami Mountains, northeast Japan Jun-ichi TAZAWA* and Yosuke IBARAKI** Abstract A Middle Permian (Kubergandian-Murgabian) brachiopod fauna is described from the type section of the lower Kanokura Formation in the Setamai area, southern Kitakami Moun tains, northeast Japan. This fauna contains the following nine species: Transennatia gratiosa, Tyloplecta cf. yangzeensis, Waagenoconcha sp., Linoproductus cora, Cancrinella sp., Leptodus nobilis, Derbyia grandis, Derbyia nipponica and Spiriferella keilhavii. The Setamai fauna is characterized by the mixuture of both the Boreal and Tethyan elements. Key words: Boreal-Tethyan mixed fauna, brachiopods. Middle Permian, Setamai, southern Kitakami Mountains. Introduction The Permian brachiopod specimens described in this paper were collected by the authors and late Prof. M. Minato of Hokkaido University from nine localities in the Kanokurasawa and Kacchizawa valleys in the Setamai area, the type locahty of the lower part of the Kanokura Formation, southern Kitakami Mountains, northeast Japan (Figs. 1,2). The Middle Permian Kanokura Formation was named by Onuki (1937) as the Kanokura Stage, but Onuki (1956)later changed the name to 'formation' with the outcrops along the Kanokurasawa valley as its type section. The stratigraphy of the Kanokura Formation in the Setamai area was described and discussed in detail by Minato et al.(1954,1978,1979), Onuki (1956, 1969), Murata (1964), Saito (1966, 1968) and Choi (1973, 1976). In palaeontology, many species of fusulinaceans (Choi, 1973), corals (Minato, 1955; Minato and Kato, 1965), brachiopods (Hayasaka, 1953; Hayasaka and Minato, 1956; Minato and Nakamura, 1956; * Department of Geology, Faculty of Science, Niigata University, Niigata 950-2181, Japan ** Graduate School of Science and Technology, Niigata University, Niigata 950-2181, Japan (Manuscript received 24 November, 2(XX); accepted 21 December, 2000) J.
    [Show full text]
  • Carboniferous Formations and Faunas of Central Montana
    Carboniferous Formations and Faunas of Central Montana GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 Carboniferous Formations and Faunas of Central Montana By W. H. EASTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 A study of the stratigraphic and ecologic associa­ tions and significance offossils from the Big Snowy group of Mississippian and Pennsylvanian rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows : Eastern, William Heyden, 1916- Carboniferous formations and faunas of central Montana. Washington, U.S. Govt. Print. Off., 1961. iv, 126 p. illus., diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 348) Part of illustrative matter folded in pocket. Bibliography: p. 101-108. 1. Paleontology Montana. 2. Paleontology Carboniferous. 3. Geology, Stratigraphic Carboniferous. I. Title. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, B.C. CONTENTS Page Page Abstract-__________________________________________ 1 Faunal analysis Continued Introduction _______________________________________ 1 Faunal relations ______________________________ 22 Purposes of the study_ __________________________ 1 Long-ranging elements...__________________ 22 Organization of present work___ __________________ 3 Elements of Mississippian affinity.._________ 22 Acknowledgments--.-------.- ___________________
    [Show full text]
  • Conodont Biostratigraphy and Paleoecology of The
    CONODONT BIOSTRATIGRAPHY AND PALEOECOLOGY OF THE LOWER DEVONIAN HELDERBERG GROUP OF VIRGINIA by Elizabeth G. Cook Thesis submitted to the Graduate Faculty of the Virginia Polytechnic Institute and State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Geological Sciences APPROVED: Dr. C. G. Tillman, Chairman -------------~-""'\-----7----- --------------------~-~------- Dr. W. D.)Lowry Dr. J. F. Read May, 1981 Blacksburg, Virginia ACKNOWLEDGEMENTS I thank Dr. Tillman for proposing the problem and for continued help and encouragement during the research and writing of the thesis. Dr. J. F. Read and W. D. Lowry offered constructive criticism of the ' ' manuscript. Thanks are also due to William Seaton for assistance with some of the sampling and to Gordon Love for assistance with the photography. I also acknowledge financial support from the Department of Geological Sciences at Virginia Polytechnic Institute and State University. E. G. C. ii TABLE OF CONTENTS Page ACKNOWLEDGEMENTS ii LIST OF FIGURES vi LIST OF TABLES vii INTRODUCTION • 1 LOCATION OF SECTIONS 3 METHODS 5 STRUCTURAL SETTING • 7 STRATIGRAPHY • 8 Introduction • 8 Previous Work 8 Description of Formations in the Study Area 10 Keyser Formation • • 10 New Creek Limestone 12 Healing Springs Sandstone 12 Corriganville Limestone 13 Licking Creek Formation 13 Regional Correlation 14 DEPOSITIONAL ENVIRONMENTS 17 Introduction • • 17 Keyser Formation 17 Laminated limestone lithofacies 17 Nodular limestone lithofacies 20 Cross-stratified sand lithofacies 22 iii Page Shale lithofacies 23 Deeper water facies 23 Swmnary of Keyser facies in the study area • 24 New Creek Limestone 24 Healing Springs Sandstone 25 Corriganville Limestone 26 Licking Creek Formation 26 Cherry Run Member 26 Little Cove Member .
    [Show full text]
  • Paleozoic Rocks Antelope Valley Eureka and Nye Counties Nevada
    :It k 'I! ' Paleozoic Rocks Antelope Valley Eureka and Nye Counties Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 423 Paleozoic Rocks of Antelope Valley Eureka and Nye Counties Nevada By CHARLES W. MERRIAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 423 P,rinciples of stratigraphy applied in descriptive study of the Central Great Basin Paleozoic column UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 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 25, D.C. CONTENTS Page Page Silurian system ____________________________________ _ Abstract------------------------------------------- 1 36 Introduction. _____________________________________ _ 2 General features-------------------------------- 36 Geologic setting ______________ ------ ___ --------- 2 Roberts Mountains formation ___________________ _ 37 History of investigation ________________________ _ 5 Lone Mountain dolomite ______ ---_-------------- 39 Purpose and scope _____________ -- ______ ------ --- 6 Devonian system ______________ ---- __ - _- ___ - _------- 41 Acknowledgments ______________________________ _ 6 General features _____________ - ___________ -_----- 41 Geologic structure as related to stratigraphy __________ _ 6 Western Helderberg age limestones of the Monitor Paleontologic studies ______ ..:. _______ ~ ________________ _ 9 · Range ______ - _.- ___ --------------------------- 42 The Paleozoic column at Antelope Valley
    [Show full text]
  • 1 Xerox University Microfilmst Ann Arbor, Michigan 48106
    I 76-9946 ti I CARNES, John Beynon, 1943- CONODONT BIOSTRATIGRAPHY IN THE LOWER I MIDDLE ORDOVICIAN OF THE WESTERN I APPALACHIAN THRUST-BELTS IN NORTHEASTERN TENNESSEE. The Ohio State University, Ph.D., I 1975 I Geology 1 Xerox University Microfilmst Ann Arbor, Michigan 48106 THIS DISSERTATION HAS BEEN MICROFILMED EXACTLY AS RECEIVED. CONODONT BIOSTRATIGRAPHY IN THE LOWER MIDDLE ORDOVICIAN OF THE WESTERN APPALACHIAN THRUST-BELTS IN NORTHEASTERN TENNESSEE DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By John B. Carnes, B.A., B.S The Ohio State University 1975 Reading Committee: Approved by Professor S. M. Bergstr8m, Chairman Professor W. C. Sweet Professor Gunter Faure 7 Q / Adviser irtment or and Mineralogy ACKNOWLEDGMENTS Dr. Stig Mo Bergstrom suggested and supervised this project. Dr. Bergstrflm has been an enthusiastic adviser and a stimulating educator; his interest, his guidance, and the tremendous amount of time he devoted to this project are greatly appreciated. Dr. Walter C. Sweet read the manuscript and offered many helpful suggestions. Dr. Sweet has spent many hours, to the writer's profit, discussing conodont biostratigraphy and taxonomy and sharing his insights. Thanks are also due to Dr. Gunter Faure, who read the manuscript; to Dr. Aurele LaRocque who kindly allowed the writer to use his office space, his drafting equipment, and his personal library; and to Dr. Barry J. Cooper and Dr. Robert B. Votaw, who, while graduate students at The Ohio State University, freely discussed their ideas with the writer. I am deeply indebted to several good friends who provided valuable assistance in the final assembly of this report.
    [Show full text]
  • Six Charts Showing Biostratigraphic Zones, and Correlations Based on Conodonts from the Devonian and Mississippian Rocks of the Upper Mississippi Valley
    14. GS: C.2 ^s- STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION SIX CHARTS SHOWING BIOSTRATIGRAPHIC ZONES, AND CORRELATIONS BASED ON CONODONTS FROM THE DEVONIAN AND MISSISSIPPIAN ROCKS OF THE UPPER MISSISSIPPI VALLEY Charles Collinson Alan J. Scott Carl B. Rexroad ILLINOIS GEOLOGICAL SURVEY LIBRARY AUG 2 1962 ILLINOIS STATE GEOLOGICAL SURVEY URBANA 1962 CIRCULAR 328 I I co •H co • CO <— X c = c P o <* CO o CO •H C CD c +» c c • CD CO ft o e c u •i-CU CD p o TJ o o co CO TJ <D CQ x CO CO CO u X CQ a p Q CO *» P Mh coc T> CD *H O TJ O 3 O o co —* o_ > O p X <-> cd cn <d ^ JS o o co e CO f-l c c/i X ex] I— CD co = co r CO : co *H U to •H CD r I .h CO TJ x X CO fc TJ r-< X -P -p 10 co C => CO o O tJ CD X5 o X c c •> CO P <D = CO CO <H X> a> s CO co c %l •H CO CD co TJ P X! h c CD Q PI CD Cn CD X UJ • H 9 P CD CD CD p <D x c •—I X Q) p •H H X cn co p £ o •> CO o x p •>o C H O CO "P CO CO X > l Ct <-c . a> CD CO X •H D. CO O CO CM (-i co in Q.
    [Show full text]
  • Distribution of the Middle Ordovician Copenhagen Formation and Its Trilobites in Nevada
    Distribution of the Middle Ordovician Copenhagen Formation and its Trilobites in Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 749 Distribution of the Middle Ordovician Copenhagen Formation and its Trilobites in Nevada By REUBEN JAMES ROSS, JR., and FREDERICK C. SHAW GEOLOGICAL SURVEY PROFESSIONAL PAPER 749 Descriptions of Middle Ordovician trilobites belonging to 21 genera contribute to correlations between similar strata in Nevada) California) and 0 klahoma UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. lVIOR TON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 78-190301 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 70 cents (paper cover) Stock Number 2401-2109 CONTENTS Page Page Abstract ______________________________ -------------------------------------------------- 1 Descriptions of trilobites __________________________________________________ _ 14 Introduction ________________________________________________________________________ _ 1 Genus T1·iarth1·us Green, 1832 .... ------------------------------ 14 Previous investigations _____________________________________________ _ 1 Genus Carrickia Tripp, 1965 ____________________________________ _ 14 Acknowledgments-------------------------------------------------------· 1 Genus Hypodicranotus Whittington, 1952 _____________ _ 15 Geographic occurrences of the Copenhagen Genus Robergia Wiman, 1905·----------------------------------
    [Show full text]
  • GEOLOGICAL SURVEY RESEARCH 1972 Chapter B
    GEOLOGICAL SURVEY RESEARCH 1972 Chapter B GEOLOGICAL SURVEY PROFESSIONAL PAPER 800-8 Scientific notes and summaries of investigations in geology, hydrology, and related fields UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director For sale by the Superintendent of Documents, U.S. Qovernment Printing Office, Washington, D.C., 20402 - Price $2.26 CONTENTS GEOLOGIC STUDIES Marine geology Page Structural features of the continental margin, northeastern Gulf of Mexico, by R. G. Martin, Jr. Marine geology of Yakutat Bay, Alaska, by F. F. Wright . Paleontology and stratigraphy Leiosphaeridio (Acritarcha) in the Mesozoic oil shales of northern Alaska, by R. F. Boneham and I. L. Tailleur . Quartzsand-bearing zone and Early Silurian age of upper part of the Hanson Creek Formation in Eureka County, Nev., by T. E. MullensandF.G.Poole ................................................................................... Trend-surface analysis of the thickness of the High Bridge Group (Middle Ordovician) of central Kentucky and its bearing on the nature of the post-Knox unconformity, by D. E. Wolcott, E. R. Cressman, and J. J. Connor . Glacial geology The Ingraham esker, Chazy, N.Y ., by C. S. Denny . Economic geology High-purity veins of soda-niter, NaN03, and associated saline minerals in the Chilean nitrate deposits, by G. E. Ericksen and M. E. Mrose ................................................................................................. Thorium distribution in a ganite stock near Bull Canyon, Lemhi County, Idaho, by M. H. Staatz, C. M. Bunker, and C. A. Bush . White clay deposits of Centre, Blair, Huntingdon, and Bedford Counties, Pa., by J. W. Hosterman . Reconnaissance geology and mineral potential of Thomas, Keg, and Desert calderas, central Juab County, Utah, by D.
    [Show full text]
  • Catalog of Type Specimens of Invertebrate Fossils: Cono- Donta
    % {I V 0> % rF h y Catalog of Type Specimens Compiled Frederick J. Collier of Invertebrate Fossils: Conodonta SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY NUMBER 9 SERIAL PUBLICATIONS OF THE SMITHSONIAN INSTITUTION The emphasis upon publications as a means of diffusing knowledge was expressed by the first Secretary of the Smithsonian Institution. In his formal plan for the Insti­ tution, Joseph Henry articulated a program that included the following statement: "It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge." This keynote of basic research has been adhered to over the years in the issuance of thousands of titles in serial publications under the Smithsonian imprint, com­ mencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Annals of Flight Smithsonian Contributions to Anthropology Smithsonian Contributions to Astrophysics Smithsonian Contributions to Botany Smithsonian Contributions to the Earth Sciences Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology Smithsonian Studies in History and Technology In these series, the Institution publishes original articles and monographs dealing with the research and collections of its several museums and offices and of profes­ sional colleagues at other institutions of learning. These papers report newly acquired facts, synoptic interpretations of data, or original theory in specialized fields. These publications are distributed by mailing lists to libraries, laboratories, and other in­ terested institutions and specialists throughout the world. Individual copies may be obtained from the Smithsonian Institution Press as long as stocks are available.
    [Show full text]