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Cambrian Ordovician
Open File Report LXXVI the shale is also variously colored. Glauconite is generally abundant in the formation. The Eau Claire A Summary of the Stratigraphy of the increases in thickness southward in the Southern Peninsula of Michigan where it becomes much more Southern Peninsula of Michigan * dolomitic. by: The Dresbach sandstone is a fine to medium grained E. J. Baltrusaites, C. K. Clark, G. V. Cohee, R. P. Grant sandstone with well rounded and angular quartz grains. W. A. Kelly, K. K. Landes, G. D. Lindberg and R. B. Thin beds of argillaceous dolomite may occur locally in Newcombe of the Michigan Geological Society * the sandstone. It is about 100 feet thick in the Southern Peninsula of Michigan but is absent in Northern Indiana. The Franconia sandstone is a fine to medium grained Cambrian glauconitic and dolomitic sandstone. It is from 10 to 20 Cambrian rocks in the Southern Peninsula of Michigan feet thick where present in the Southern Peninsula. consist of sandstone, dolomite, and some shale. These * See last page rocks, Lake Superior sandstone, which are of Upper Cambrian age overlie pre-Cambrian rocks and are The Trempealeau is predominantly a buff to light brown divided into the Jacobsville sandstone overlain by the dolomite with a minor amount of sandy, glauconitic Munising. The Munising sandstone at the north is dolomite and dolomitic shale in the basal part. Zones of divided southward into the following formations in sandy dolomite are in the Trempealeau in addition to the ascending order: Mount Simon, Eau Claire, Dresbach basal part. A small amount of chert may be found in and Franconia sandstones overlain by the Trampealeau various places in the formation. -
Stratigraphic Succession in Lower Peninsula of Michigan
STRATIGRAPHIC DOMINANT LITHOLOGY ERA PERIOD EPOCHNORTHSTAGES AMERICANBasin Margin Basin Center MEMBER FORMATIONGROUP SUCCESSION IN LOWER Quaternary Pleistocene Glacial Drift PENINSULA Cenozoic Pleistocene OF MICHIGAN Mesozoic Jurassic ?Kimmeridgian? Ionia Sandstone Late Michigan Dept. of Environmental Quality Conemaugh Grand River Formation Geological Survey Division Late Harold Fitch, State Geologist Pennsylvanian and Saginaw Formation ?Pottsville? Michigan Basin Geological Society Early GEOL IN OG S IC A A B L N Parma Sandstone S A O G C I I H E C T I Y Bayport Limestone M Meramecian Grand Rapids Group 1936 Late Michigan Formation Stratigraphic Nomenclature Project Committee: Mississippian Dr. Paul A. Catacosinos, Co-chairman Mark S. Wollensak, Co-chairman Osagian Marshall Sandstone Principal Authors: Dr. Paul A. Catacosinos Early Kinderhookian Coldwater Shale Dr. William Harrison III Robert Reynolds Sunbury Shale Dr. Dave B.Westjohn Mark S. Wollensak Berea Sandstone Chautauquan Bedford Shale 2000 Late Antrim Shale Senecan Traverse Formation Traverse Limestone Traverse Group Erian Devonian Bell Shale Dundee Limestone Middle Lucas Formation Detroit River Group Amherstburg Form. Ulsterian Sylvania Sandstone Bois Blanc Formation Garden Island Formation Early Bass Islands Dolomite Sand Salina G Unit Paleozoic Glacial Clay or Silt Late Cayugan Salina F Unit Till/Gravel Salina E Unit Salina D Unit Limestone Salina C Shale Salina Group Salina B Unit Sandy Limestone Salina A-2 Carbonate Silurian Salina A-2 Evaporite Shaley Limestone Ruff Formation -
Columnals (PDF)
2248 22482 2 4 V. INDEX OF COLUMNALS 8 Remarks: In this section the stratigraphic range given under the genus is the compiled range of all named species based solely on columnals assigned to the genus. It should be noted that this range may and often differs considerably from the range given under the same genus in Section I, because that range is based on species identified on cups or crowns. All other abbreviations and format follow that of Section I. Generic names followed by the type species are based on columnals. Genera, not followed by the type species, are based on cups and crowns as given in Section I. There are a number of unlisted columnal taxa from the literature that are indexed as genera recognized on cups and crowns. Bassler and Moodey (1943) did not index columnal taxa that were not new names or identified genera with the species unnamed. I have included some of the omissions of Bassler and Moodey, but have not made a search of the extensive literature specifically for the omitted citations because of time constraints. Many of these unlisted taxa are illustrated in the early state surveys of the eastern and central United States. Many of the columnal species assigned to genera based on cups or crowns are incorrect assignments. An uncertain, but significant, number of the columnal genera are synonyms of other columnal genera as they are based on different parts of the stem of a single taxon. Also a number of the columnal genera are synonyms of genera based on cups and crowns as they come from more distal parts of the stem not currently known to be associated with the cup or crown. -
Tremichnus in Crinoid Pluricolumnals from the Silurian of Western Estonia (Baltica)
Carnets Geol. 15 (17) Tremichnus in crinoid pluricolumnals from the Silurian of western Estonia (Baltica) Olev VINN 1 Mark A. WILSON 2 William I. AUSICH 3 Ursula TOOM 4 Abstract: Rare pits attributed to Tremichnus have been found in crinoids from the Silurian of Estonia. The Rhuddanian Tremichnus is the earliest symbiont in crinoid columnals of Baltica. These pits presu- mably were domiciles of unknown organisms. Tremichnus had a negative effect on the host crinoid as demonstrated by swollen columnals. Tremichnus in the Silurian of Estonia is less common than similar traces in the Silurian of nearby Gotland. The most important aspect of this study is the rarity of this interaction in these samples in contrast to most other samples of comparable age elsewhere. These structures have a very patchy distribution. Key Words: Trace fossils; Tremichnus; symbiosis; crinoids; Silurian; Estonia. Citation: VINN O., WILSON M.A., AUSICH W.I. & TOOM U. (2015).- Tremichnus in crinoid pluricolumnals from the Silurian of western Estonia (Baltica).- Carnets Geol., Madrid, vol. 15, nº 17, p. 239-243. Résumé : Tremichnus dans des segments de tiges de crinoïdes du Silurien d'Estonie occiden- tale (bouclier balte).- Quelques petites cavités attribuées à Tremichnus ont été trouvées dans des crinoïdes provenant du Silurien d'Estonie. Ce Tremichnus rhuddanien est le symbiote le plus ancien ob- servé dans des segments de tiges de crinoïdes du bouclier balte. Ces cavités correspondent vraisem- blablement à des habitats d'organismes inconnus. Tremichnus a eu un impact négatif sur le crinoïde hôte comme en attestent les renflements des tiges. Tremichnus est moins fréquent dans le Silurien d'Estonie que des traces semblables dans le Silurien du Gotland voisin. -
Deep Oil Possibilities of the Illinois Basin
s Ccc 36? STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION DEEP OIL POSSIBILITIES OF THE ILLINOIS BASIN Alfred H. Bell Elwood Atherton T. C. Buschbach David H. Swann ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief URBANA CIRCULAR 368 1964 . DEEP OIL POSSIBILITIES OF THE ILLINOIS BASIN Alfred H. Bell, Elwood Atherton, T. C. Buschbach, and David H. Swann ABSTRACT The Middle Ordovician and younger rocks of the Illinois Basin, which have yielded 3 billion barrels of oil, are underlain by a larger volume of virtually untested Lower Ordovician and Cambrian rocks. Within the region that has supplied 99 percent of the oil, where the top of the Middle Ordovician (Trenton) is more than 1,000 feet be- low sea level, less than 8 inches of hole have been drilled per cubic mile of the older rocks. Even this drilling has been near the edges; and in the central area, which has yielded five- sixths of the oil, only one inch of test hole has been drilled per cubic mile of Lower Ordovician and Cambrian. Yet drilling depths are not excessive, ranging from 6,000 to 14,000 feet to the Precambrian. More production may be found in the Middle Ordovician Galena Limestone (Trenton), thus extending the present productive regions. In addition, new production may be found in narrow, dolomitized fracture zones in the tight limestone facies on the north flank of the basin . The underlying Platteville Limestone is finer grained and offers fewer possibilities. The Joachim Dolomite oil- shows occur in tight sandstone bodies that should have commercial porosity in some re- gions. -
X Hydrogeologic Framework and Geochemistry of Ground Water
U.S. DEPARTMENT OF THE INTERIOR PREPARED IN COOPERATION WITH THE WATER-RESOURCES INVESTIGATIONS REPORT 02-4123 U.S. GEOLOGICAL SURVEY U.S. DEPARTMENT OF THE NAVY, SOUTHERN DIVISION, SHEET 1 of 3 NAVAL FACILITIES ENGINEERING COMMAND Taylor. C.J., and Hostettler, F.D., 2002, Hydrogeologic Framework and Geochemistry of Ground Water and Petroleum in the Silurian-Devonian Carbonate Aquifer, South-Central Louisville, Kentucky science USGSfor a changing world INTRODUCTION (A) (B) (C) (D) Previously published investigations concerning the ground-water resources HOLE DIAMETER, ACOUSTIC HOLE DIAMETER. ACOUSTIC HOLE DIAMETER. ACOUSTIC HOLE DIAMETER, ACOUSTIC of the city of Louisville and Jefferson County, Kentucky, have mostly focused on IN INCHES LITHOLOGY TELEVIEWER IN INCHES LITHOLOGY TELEVIEWER IN INCHES LITHOLOGY TELEVIEWER IN INCHES LITHOLOGY TELEVIEWER the highly productive Ohio River alluvial aquifer (Rorabaugh, 1956; Walker, 1957; Bell. 1966: Unthank and others, 1995). In contrast, relatively little attention has been given to the Ordovician and Silurian-Devonian carbonate aquifers that 10h X 10.4 underlie much of the Louisville and Jefferson County area (fig. I) because of their limited potential for water-supply development (Palmquist and Hall, 1960). LLJ LU O O However, detailed information about the ground-water quality and hydrogeology of £ the carbonate aquifer is needed by State and Federal environmental regulators and o: a: ^ ID private consultants for planning and conducting local environmental t,ite 5% CO C/3 t. * assessments and ground-water remediation. The Silurian-Devonian carbonate Q Q aquifer is of particular interest because it underlies much of the urbanized and 40;: 72%- industrialized areas of the city of Louisville, exhibits moderately well-developed NF karst, and is potentially vulnerable to human-induced contamination. -
Geologic Cross Section C–C' Through the Appalachian Basin from Erie
Geologic Cross Section C–C’ Through the Appalachian Basin From Erie County, North-Central Ohio, to the Valley and Ridge Province, Bedford County, South-Central Pennsylvania By Robert T. Ryder, Michael H. Trippi, Christopher S. Swezey, Robert D. Crangle, Jr., Rebecca S. Hope, Elisabeth L. Rowan, and Erika E. Lentz Scientific Investigations Map 3172 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: Ryder, R.T., Trippi, M.H., Swezey, C.S. Crangle, R.D., Jr., Hope, R.S., Rowan, E.L., and Lentz, E.E., 2012, Geologic cross section C–C’ through the Appalachian basin from Erie County, north-central Ohio, to the Valley and Ridge province, Bedford County, south-central Pennsylvania: U.S. Geological Survey Scientific Investigations Map 3172, 2 sheets, 70-p. -
Stratigraphic Framework of Cambrian and Ordovician Rocks in The
Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Medina County, Ohio, through Southwestern and South-Central Pennsylvania to Hampshire County, West Virginia U.S. GEOLOGICAL SURVEY BULLETIN 1839-K Chapter K Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Medina County, Ohio, through Southwestern and South-Central Pennsylvania to Hampshire County, West Virginia By ROBERT T. RYDER, ANITA G. HARRIS, and JOHN E. REPETSKI Stratigraphic framework of the Cambrian and Ordovician sequence in part of the central Appalachian basin and the structure of underlying block-faulted basement rocks U.S. GEOLOGICAL SURVEY BULLETIN 1839 EVOLUTION OF SEDIMENTARY BASINS-APPALACHIAN BASIN U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, Jr., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government UNITED STATES GOVERNMENT PRINTING OFFICE: 1992 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging in Publication Data Ryder, Robert T. Stratigraphic framework of Cambrian and Ordovician rocks in the central Appalachian Basin from Medina County, Ohio, through southwestern and south-central Pennsylvania to Hampshire County, West Virginia / by Robert T. Ryder, Anita C. Harris, and John E. Repetski. p. cm. (Evolution of sedimentary basins Appalachian Basin ; ch. K) (U.S. Geological Survey bulletin ; 1839-K) Includes bibliographical references. Supt. of Docs, no.: I 19.3:1839-K 1. Geology, Stratigraphic Cambrian. -
Le Silurien Du Synclinorium De Moncorvo (Ne Du Portugal): Biostratigraphie Et Importance Paléogéographique
LE SILURIEN DU SYNCLINORIUM DE MONCORVO (NE DU PORTUGAL): BIOSTRATIGRAPHIE ET IMPORTANCE PALÉOGÉOGRAPHIQUE GRACIELA NOEMI SARMIENTO, JOSÉ MANDEL PIÇARRA, JOSÉ ALMEIDA REBELO, MICHEL ROBARDET, JUAN CARLOS GUTIÉRREZ-MARCO, PETR STORCH & ISABEL RABANO SARMIENTO G.N., PIÇARRA, REBELO J.A., ROBARDET M., GUTIÉRREZ-MARCO J.C., STORCH P. & RABANO I. 1999. Le Silurien du synclinorium de Moncorvo (NE du Portugal): biostratigraphie et importance paléogéogra- phique. [The Silurian of the Moncorvo synclinorium (NE Portugal): biostratigraphy and paleogeographical impor- tance]. GEOBIOS, 32, 5: 749-767. Villeurbanne, le 31.10.1999. RÉSUMÉ - Dans la succession silurienne du synclinorium de Moncorvo (NW de la Zone Centre Ibérique, Portugal), des lentilles calcaires ont livré, dans deux localités distinctes, les premiers conodontes siluriens du Portugal. Dans la première localité, Kockelella cf. uariabilis, K. cf. absidata, Ozarkodina confluens, Oz. excauata et Pseudooneotod us beckmanni indiquent le Ludlow s.l. (ou peut-être le Wenlock supérieur ou terminal). Dans la seconde, Oulod us ele- gans, O. cf. cristagalli et Ozarkodina ex gr. remscheidensis indiquent le Pridoli, ce que confirme la présence, dans le même gisement, de scyphocrinoïdes du genre Scyphocrinites, et en particulier les lobolithes à cirrhes. Dans les schistes noirs à nodules sous-jacents aux calcaires, des graptolites montrent l'existence de niveaux du Llandovery moyen et supérieur (Aéronien et Télychien) et du Wenlock. La succession silurienne de Moncorvo apparaît ainsi comme une séquence condensée, analogue, en particulier, à celles qui existent dans la Zone d'Ossa Morena, en Sardaigne et dans certaines régions d'Afrique du Nord. Ces successions sont bien différentes de celles qui caracté- risent les régions centrales et méridionales de la Zone Centre Ibérique où, dans leur partie supérieure, les dépôts siluriens, de faible profondeur, sont beaucoup plus épais et plus riches en matériel terrigène grossier. -
Geology for Environmental Planning . in Marion County
GEOLOGY FOR ENVIRONMENTAL PLANNING . GEOLOGY--:~ .\RY IN MARION COUNTY, INDIANA SURVEY Special Report 19 c . 3 State of)pdiana Department of N'.atural Resources GEOLOGICAL SURVEY SCIENTIFIC AND TECHNICAL STAFF OF THE GEOLOGICAL SURVEY JOHN B. PATION, State Geologist MAURICE E. BIGGS, Assistant State Geologist MARY BETH FOX, Mineral Statistician COAL AND INDUSTRIAL MINERALS SECTION GEOLOGY SECTION DONALD D. CARR, Geologist and Head ROBERT H. SHAVER, Paleontologist and Head CURTIS H. AULT, Geologist and Associate Head HENRY H. GRAY, Head Stratigrapher PEl-YUAN CHEN, Geologist N. K. BLEUER, Glacial Geologist DONALD L. EGGERT, Geologist EDWIN J. HARTKE, Environmental Geologist GORDON S. FRASER, Geologist JOHN R. HILL, Glacial Geologist DENVER HARPER, Geologist CARL B. REXROAD, Paleontologist WALTER A. HASENMUELLER, Geologist NELSON R. SHAFFER, Geologist GEOPHYSICS SECTION PAUL IRWIN, Geological Assistant MAURICE E. BIGGS, Geophysicist and Head ROBERT F. BLAKELY, Geophysicist JOSEPH F. WHALEY, Geophysicist DRAFTINGANDPHOTOGRAPHYSECTION JOHN R. HELMS, Driller WILLIAM H. MORAN, Chief Draftsman and Head SAMUEL L. RIDDLE, Geophysical Assistant RICHARDT. HILL, Geological Draftsman ROGER L. PURCELL, Senior Geological Draftsman PETROLEUM SECTION GEORGE R. RINGER, Photographer G. L. CARPENTER, Geologist and Head WILBUR E. STALIONS, Artist-Draftsman ANDREW J. HREHA, Geologist BRIAN D. KEITH, Geologist EDUCATIONAL SERVICES SECTION STANLEY J. KELLER, Geologist R. DEE RARICK, Geologist and Head DAN M. SULLIVAN, Geologist JAMES T. CAZEE, Geological Assistant -
IGS 2015B-Maquoketa Group
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106Th Annual Report of the State Geologist
106TH ANNUAL REPORT OF THE STATE GEOLOGIST of INDIANA GEOLOGICAL SURVEY DEPARTMENT OF NATURAL RESOURCES for July 1, 1981 - June 30, 1982 GEOLOGICAL SURVEY ONE HUNDRED AND SIXTH ANNUAL REPORT OF THE STATE GEOLOGIST PERSONNEL Permanent Personnel Administration John B. Patton •.•••• • .•.•••••••••.. State Geo 1og i st Maurice E. Biggs •. Assistant State Geologist Mary E. Fox • • • • • • • • . • . • . • • • • • • . •Mineral Statistician E. Co leen George. • . • . • . • • . • . • . • • • • • Principal Secretary Coal and Industrial Minerals Section Donald D. Carr .•• • •••.•••Geologist and Head Curtis H. Ault ••. .Geologist and Associate Head Donald L. Eggert. • Geologist Gordon S. Fraser •••••• • .•.• Geologist Denver Harper • • · .••• Geologist Nancy R. Hasenmueller .•...• • Geologist Wa 1ter A. Hasenmue 11 er. • • . .••••• Geologist Paul Irwin (Reclamation). • Geologist Nelson R. Shaffer ••• • Geologist Michele Wright (NRC) •. • • Geo log ist Janet Roller ••• · . • • • Secretary (To August 14, 1981) Susan E. Rumple . • • • . • Secretary (From August 12, 1981) Kathryn Shaffer • • . • • . • • Secretary Drafting and Photography Section William H. Moran. ••Chief Draftsman and Head Richard T. Hill •. •••.•.• Senior Geological Draftsman Roger L. Purcell. • Senior Geological Draftsman George R. Ringer ••. • •••••••••.•Photographer Wilbur E. Stalions. • Geological Artist-Draftsman Educational Services Reevan D. Rarick .•••. .•••.•.•. Geologist 1 Geochemistry Section Richard K. Leininger. Geochemist and Head Margaret V. Golde •.••. • .Instrument Analyst