Chapter 1: Sequence Stratigraphy of the Glenshaw Formation
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Mine Pool Atlas
West Virginia Geological Survey West Virginia Mine Pool Atlas WEST VIRGINIA West Virginia Mine Pool Atlas Final Project Report for the project period January 1, 2010 through December 31, 2011 Submitted to: West Virginia Department of Environmental Protection 601 57th Street SE Charleston, WV 25304 Submitted by: West Virginia Geological and Economic Survey 1 Mont Chateau Road Morgantown, WV 26508-8079 Principal Investigator Jane S. McColloch, Senior Geologist Co-Investigators Richard D. Binns, Jr., GIS Database Administrator Bascombe M. Blake, Jr., Manager, Coal Programs Michael T. Clifford, GIS Analyst Sarah E. Gooding, Geologist and GIS Cartographer May 2012 Inter-Agency Agreement Number 036 1 ACKNOWLEDGMENTS This study was greatly facilitated by the ongoing work of the Coal Bed Mapping Program (CBMP) staff. In addition, several individuals provided information, technical expertise, and technical support during the course of the project. Notable among these: • William C. Borth, West Virginia Department of Environmental Protection • A. Nick Schaer, West Virginia Department of Environmental Protection • William J. Toomey, West Virginia Bureau for Public Health • Mary C. Behling, West Virginia Geological and Economic Survey • Gayle H. McColloch, West Virginia Geological and Economic Survey • Edward I. Loud, West Virginia Geological and Economic Survey • Betty L. Schleger, West Virginia Geological and Economic Survey • Susan E. Pool, West Virginia Geological and Economic Survey • Samantha J. McCreery, West Virginia Geological and Economic Survey i ABSTRACT The West Virginia Mine Pool Atlas project was a two-year study by the West Virginia Geological and Economic Survey (WVGES) to evaluate abandoned coal mines as potential groundwater sources. This study was funded by the West Virginia Department of Environmental Protection (WVDEP). -
Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution
Graduate Theses, Dissertations, and Problem Reports 2020 Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution Mark D. Swift West Virginia University, [email protected] Follow this and additional works at: https://researchrepository.wvu.edu/etd Part of the Geomorphology Commons Recommended Citation Swift, Mark D., "Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution" (2020). Graduate Theses, Dissertations, and Problem Reports. 7542. https://researchrepository.wvu.edu/etd/7542 This Thesis is protected by copyright and/or related rights. It has been brought to you by the The Research Repository @ WVU with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you must obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in WVU Graduate Theses, Dissertations, and Problem Reports collection by an authorized administrator of The Research Repository @ WVU. For more information, please contact [email protected]. Knickzones in Southwest Pennsylvania Streams Indicate Accelerated Pleistocene Landscape Evolution Mark D. Swift Thesis Submitted to the Eberly College of Arts and Sciences at West Virginia University in partial fulfillment of the requirements for the degree of Master of Arts in Geography Jamison Conley, Ph.D., Co-Chair J. Steven Kite, Ph.D., Co-Chair Nicolas Zegre, Ph.D. Department of Geology and Geography Morgantown, West Virginia 2020 Keywords: landscape evolution, knickzone, southwest Pennsylvania Copyright 2020 Mark D. -
The Contact of the Upper Neoproterozoic with the Lower
Ugidos, J.M., Barba, P., Valladares, M.I., Suarez, M., and Ellam, R.M. (2016) The Ediacaran-Cambrian transition in the Cantabrian Zone 1 (North Spain): sub-Cambrian weathering, K-metasomatism and provenance of detrital series. Journal of the Geological Society, 173(4), pp. 603-615. (doi:10.1144/jgs2016-004) This is the author’s final accepted version. There may be differences between this version and the published version. You are advised to consult the publisher’s version if you wish to cite from it. http://eprints.gla.ac.uk/115950/ Deposited on: 1 February 2016 Enlighten – Research publications by members of the University of Glasgow http://eprints.gla.ac.uk 1 1 The Ediacaran-Cambrian transition in the Cantabrian Zone (North Spain): sub- 2 Cambrian weathering, K-metasomatism and provenance of detrital series 3 4 J.M. Ugidos,a* P. Barba,a M.I. Valladares,a M. Suárez,a R.M. Ellam, b 5 a Departamento de Geología, Facultad de Ciencias, Universidad de Salamanca, 37008 6 Salamanca, Spain b Scottish Universities Environmental Research Centre, East Kilbride G75 OQF, UK 7 8 9 Abstract: The Upper Ediacaran detrital succession in the Cantabrian Zone shows 10 geochemical and mineralogical changes resulting from sub-Cambrian weathering during 11 the Late Ediacaran worldwide sea-level fall. Relative to the unaltered rocks the altered 12 ones show crosscutting rubefaction of varying thickness a remarkable increase in illite, 13 K2O, Rb and Cs indicating K-metasomatism, and also depletion in MgO, CaO, Na2O, 14 Be and Sr, but not in Zr, Nb, Y, Sc. -
A Fan Delta Complex of Dinantian/Namurian Age
The Orustdalen Formation of Braggerhalvaya, Svalbard: A fan delta complex of Dinantian/Namurian age By Ian J. Fairchildl Abstract The Orustdalen Formation of Broggerhalvnya is well exposed on two coastal sections and is 200-250 m thick. It consists dominantly of siliceous conglomerates anid sandstones with subordinate shales and impure coal. One horizoin low in the sequence yielded spores of upper- most Dinantian/lowermost Namurian agc. Three sedimentary facies have been recognised The fluvial channel facies (interbedded conglomerates and cross-stratified sandstones) are interpreted as braided sitream deposits with flow directions to south and west A shale facies, sometimes with dri\fted plant remains, is interpreted as ovrrbank ia origin. Highly quartzose, medium-to-coarse-grained, cross-stratified sandstones make up the reworked facies wheie palaeocurrents are bimodal or indicate movement to the NE The Formation is thought to represent semdiments shed from an early Carboniferuus fault scarp erod,ing a siliceous Lower Palaeozoic source terramin The proximity of a nearby coastline led to the construction of fan deltas where fluvial deposits were reworked by waves and/or tides Early diagenetic events include the local development of pyrite, kaoIinite and calcite cements Reddening probably occurred during Middle Carboniferous times beneath an exposed land surface. Following burial, pressure solution and quartz cementation eliminated porosity at depths greater than 1000 m. Introduction The association of conglomerates with coal is unusual (Heward 1978), but is found in a number of Upper Devonian and Lower Carboniferous sequences in Svalbard (Dineley 1958; Birkenmajer 1964; Worsley and Edwards 1976; Gjelberg 1978; Gjelberg and Steel 1979). A discussion of the Br~ggerhalveya Lower Carboniferous, conglomerates and sandstones with subordinate shales and coals, is thus of interest in contributing to an understanding of this facies association. -
PDF Viewing Archiving 300
Bull. Soc. belge Géologie T. 83 fasc. 4 pp. 235- 253 Bruxelles 1974 THE CHRONOSTRATIGRAPHIC UNITS OF THE UPPER CARBONIFEROUS IN EUROPE R.H. WAGNER * ABSTRACT: The history is traced of the various chronostratigraphic units recognised in the Upper Carboniferous of western Europe, and their stratotypes are discussed. A correlation is given for the chronostratigraphic units in the Middle and Upper Carboniferou& series of Russia, in the light of pre dominantly marine successions in N.W. Spain, and suggestions are made for an integrated scheme of major units. Introduction In western Europe the classification of Carboniferous strata was further taken in The main chronostratigraphic divisions of hand by the Congrès pour !'Avancement des the Carboniferous in Europe were established Etudes de Stratigraphie Carbonifère which by MUNIER CHALMAS & DE LAPPARENT(1893), met in Heerlen in 1927, 1935, 1951 and who distinguished three marine stages charac 1958. The 1927 congress sanctioned the use terised by different faunas, viz. Dinantienl, of Namurian, a stage introduced by PURVES Moscovien2 and Ouralienl, and two stages, in 1883 and which corresponds to the West Westphalien1 and Stéphanien, characterised phalien inférieur of MUNIER CHALMAS & by coal-measures facies. Most of the names DE LAPPARENT. It also introduced the A, had been used before (see footnotes), but B and C divisions for the remaining West the 'Note sur la Nomenclature des Terrains phalian (i.e. the Westphalien supérieur of sédimentaires' provided the first formai MUNIER CHALMAS & DE LAPPARENT). The framework for a subdivision into stages of the 1935 congress expanded the Westphalian Carboniferous System. MuNIER CHALMAS & upwards by recognising the presence of a DE LAPPARENT gave precedence to the marine Westphalian D division, and subdivided the stages, Moscovian and Uralian, and regarded Namurian into A, B and C. -
Historical Development and Problems Within the Pennsylvanian Nomenclature of Ohio.1
Historical Development and Problems Within the Pennsylvanian Nomenclature of Ohio.1 GLENN E. LARSEN, OHIO Department of Natural Resources, Division of Geological Survey, Fountain Sq., Bldg. B, Columbus, OH 43224 ABSTRACT. An analysis of the historical development of the Pennsylvanian stratigraphic nomenclature, as used in Ohio, has helped define and clarify problems inherent in Ohio's stratigraphic nomenclature. Resolution of such problems facilitates further development of a useful stratigraphy and philosophy for mapping. Investigations of Pennsylvanian-age rocks in Ohio began as early as 1819- From 1858 to 1893, investigations by Newberry, I. C. White, and Orton established the stratigraphic framework upon which the present-day nomenclature is based. During the 1950s, the cyclothem concept was used to classify and correlate Pennsylvanian lithologic units. This classification led to a proliferation of stratigraphic terms, as almost every lithologic type was named and designated as a member of a cyclothem. By the early 1960s, cyclothems were considered invalid as a lithostratigraphic classification. Currently, Pennsylvanian nomenclature of Ohio, as used by the Ohio Division of Geological Survey, consists of four groups containing 123 named beds, with no formal formations or members. In accordance with the 1983 North American Stratigraphic code, the Ohio Division of Geological Survey considers all nomenclature below group rank as informal. OHIO J. SCI. 91 (1): 69-76, 1991 INTRODUCTION DISCUSSION Understanding the historical development of Pennsyl- The Early 1800s vanian stratigraphy in Ohio is important to the Ohio The earliest known references to Pennsylvanian-age Division of Geological Survey (OGS). Such an under- rocks in Ohio are found in Atwater's (1819) report on standing of Pennsylvanian stratigraphy helps define Belmont County, and an article by Granger (1821) on plant stratigraphic nomenclatural problems in order to make fossils collected near Zanesville, Muskingum County. -
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. -
The Pre-Pleistocene Phanerozoic Time-Scale- a Review
Downloaded from http://sp.lyellcollection.org/ by guest on September 26, 2021 The pre-Pleistocene Phanerozoic time-scale- a review RICHARD ST JOHN LAMBERT CONTENTS x Introduction IO 2 The Cenozoic era II 3 The Mesozoic era . I4 (A) The Cretaceous period I4 (B) The Jurassic period 16 (c) The Triassic period x8 4 The Palaeozoic era I9 (A) The Permian period I9 (B) The Carboniferous period 20 (c) The Devonian period . 22 (D) The Lower Palaeozoic era 23 5 Conclusions 24 6 References 26 Appendix I : The half-life'of S~Rb 27 Appendix 2: List of critical points 29 (A) Most reliable (pre-Tertiary) determinatxons 29 (B) Most reliable (pre-Tertiary) determinations without duplicate or sup- porting analyses . 3 ~ SUMMARY The data in The Phanerozoic Time-scale (Geo- knowledge of the decay rate of STRb. The cur- logical Society, I964) are reviewed, together rent six per cent range in commonly-used with data relevant to the Phanerozoic time- values of this constant is now of over-riding scale published up to mid-I968. Quaternary importance in causing uncertainty throughout problems are not considered, while the Tertiary the Palaeozoic scale; Rb-Sr determinations is considered to be on a comparatively well- now provide the majority of critical Palaeozoic established basis. The use of glauconite ages to ages. Even without this uncertainty, increases establish any part of the time-scale prior to the in the age of the Westphalian, the base of the Oligocene is not to be recommended, as early Carboniferous (to 36o m.y.) and the base of the glauconites can provide anomalously high Devonian (to ?4o5 m.y.) seem to be indicated apparent ages in addition to the occurrence of by new data (using the 4"7 • xol~ half-life low ages. -
Figure 3A. Major Geologic Formations in West Virginia. Allegheney And
82° 81° 80° 79° 78° EXPLANATION West Virginia county boundaries A West Virginia Geology by map unit Quaternary Modern Reservoirs Qal Alluvium Permian or Pennsylvanian Period LTP d Dunkard Group LTP c Conemaugh Group LTP m Monongahela Group 0 25 50 MILES LTP a Allegheny Formation PENNSYLVANIA LTP pv Pottsville Group 0 25 50 KILOMETERS LTP k Kanawha Formation 40° LTP nr New River Formation LTP p Pocahontas Formation Mississippian Period Mmc Mauch Chunk Group Mbp Bluestone and Princeton Formations Ce Obrr Omc Mh Hinton Formation Obps Dmn Bluefield Formation Dbh Otbr Mbf MARYLAND LTP pv Osp Mg Greenbrier Group Smc Axis of Obs Mmp Maccrady and Pocono, undivided Burning Springs LTP a Mmc St Ce Mmcc Maccrady Formation anticline LTP d Om Dh Cwy Mp Pocono Group Qal Dhs Ch Devonian Period Mp Dohl LTP c Dmu Middle and Upper Devonian, undivided Obps Cw Dhs Hampshire Formation LTP m Dmn OHIO Ct Dch Chemung Group Omc Obs Dch Dbh Dbh Brailler and Harrell, undivided Stw Cwy LTP pv Ca Db Brallier Formation Obrr Cc 39° CPCc Dh Harrell Shale St Dmb Millboro Shale Mmc Dhs Dmt Mahantango Formation Do LTP d Ojo Dm Marcellus Formation Dmn Onondaga Group Om Lower Devonian, undivided LTP k Dhl Dohl Do Oriskany Sandstone Dmt Ot Dhl Helderberg Group LTP m VIRGINIA Qal Obr Silurian Period Dch Smc Om Stw Tonoloway, Wills Creek, and Williamsport Formations LTP c Dmb Sct Lower Silurian, undivided LTP a Smc McKenzie Formation and Clinton Group Dhl Stw Ojo Mbf Db St Tuscarora Sandstone Ordovician Period Ojo Juniata and Oswego Formations Dohl Mg Om Martinsburg Formation LTP nr Otbr Ordovician--Trenton and Black River, undivided 38° Mmcc Ot Trenton Group LTP k WEST VIRGINIA Obr Black River Group Omc Ordovician, middle calcareous units Mp Db Osp St. -
Devonian and Carboniferous Pre-Stephanian Rocks from the Pyrenees
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Repositorio da Universidade da Coruña 1 Published In García-López, S. and Bastida, F. (eds). Palaeozoic conodonts from northern Spain: Eight International Conodont Symposium held in Europe. Instituto Geológico y Minero de España, Serie Cuadernos del Museo Geominero 1, (2002), pp. 367-389. Madrid (438p.). ISBN: 84-74840-446-5. Devonian and Carboniferous pre-Stephanian rocks from the Pyrenees J. SANZ-LÓPEZ Facultad de Ciencias de la Educación. Universidad de A Coruña. Paseo de Ronda 47, 15011 A Coruña (Spain). [email protected] ABSTRACT A stratigraphic description of the Devonian and Carboniferous pre-Variscan rocks of the Pyrenees is presented. The successions are grouped into sedimentary domains that replace the “facies areas” proposed by previous authors for areas with homogeneous stratigraphy. The description of the sedimentary filling is divided into temporal intervals, where the previous stratigraphic correlation, based on lithological criteria, is supplemented by faunal data, especially conodont findings. A simple palaeogeographic model of the sedimentation during the Upper Palaeozoic and data related to southern boundary between the Pyrenean basin and the Cantabro-Ebroian Massif are discussed. Keywords: Devonian, Carboniferous, conodonts, Pyrenees, stratigraphy. RESUMEN Se ha realizado una descripción estratigráfica de las rocas devónicas y carboníferas pre- variscas de los Pirineos. Las sucesiones son agrupadas en dominios sedimentarios que sustituyen a las “áreas de facies” propuestas por los autores previos para zonas con una estratigrafía homogénea. La descripción del relleno sedimentario está dividida en intervalos de tiempo, donde la correlación estratigráfica basada en criterios litológicos está incrementada por los datos faunísticos, sobre todo los hallazgos de conodontos. -
Structural Geology of the Transylvania Fault Zone in Bedford County, Pennsylvania
University of Kentucky UKnowledge University of Kentucky Master's Theses Graduate School 2009 STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA Elizabeth Lauren Dodson 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 Dodson, Elizabeth Lauren, "STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA" (2009). University of Kentucky Master's Theses. 621. https://uknowledge.uky.edu/gradschool_theses/621 This Thesis 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 Master's Theses by an authorized administrator of UKnowledge. For more information, please contact [email protected]. ABSTRACT OF THESIS STRUCTURAL GEOLOGY OF THE TRANSYLVANIA FAULT ZONE IN BEDFORD COUNTY, PENNSYLVANIA Transverse zones cross strike of thrust-belt structures as large-scale alignments of cross-strike structures. The Transylvania fault zone is a set of discontinuous right-lateral transverse faults striking at about 270º across Appalachian thrust-belt structures along 40º N latitude in Pennsylvania. Near Everett, Pennsylvania, the Breezewood fault terminates with the Ashcom thrust fault. The Everett Gap fault terminates westward with the Hartley thrust fault. Farther west, the Bedford fault extends westward to terminate against the Wills Mountain thrust fault. The rocks, deformed during the Alleghanian orogeny, are semi-independently deformed on opposite sides of the transverse fault, indicating fault movement during folding and thrusting. Palinspastic restorations of cross sections on either side of the fault zone are used to compare transverse fault displacement. -
Carboniferous Coal-Bed Gas Total Petroleum System
U.S. Geological Survey Open-File Report 2004-1272 Assessment of Appalachian Basin Oil and Gas Resources: Carboniferous Coal-bed Gas Total Petroleum System Robert C. Milici U.S. Geological Survey 956 National Center Reston, VA 20192 1 Table of Contents Abstract Introduction East Dunkard and West Dunkard Assessment units Introduction: Stratigraphy: Pottsville Formation Allegheny Group Conemaugh Group Monongahela Group Geologic Structure: Coalbed Methane Fields and Pools: Assessment Data: Coal as a source rock for CBM: Gas-In-Place Data Thermal Maturity Generation and Migration Coal as a reservoir for CBM: Porosity and Permeability Coal Bed Distribution Cumulative Coal Thickness Seals: Depth of Burial Water Production Cumulative Production Data: Pocahontas basin and Central Appalachian Shelf Assessment Units Introduction: Stratigraphy: Pocahontas Formation New River Formation Kanawha Formation 2 Lee Formation Norton Formation Gladeville Sandstone Wise Formation Harlan Formation Breathitt Formation Geologic Structure: Coalbed Methane Fields: Coal as a Source Rock for CBM Gas-in-Place Data Thermal Maturity Generation and Migration Coal as a Reservoir for CBM: Porosity and Permeability Coal Bed Distribution Cumulative Coal Thickness Seals: Depth of Burial Water Production Cumulative Production Data: Assessment Results: Appalachian Anthracite and Semi-Anthracite Assessment Unit: Pennsylvania Anthracite Introduction: Stratigraphy: Pottsville Formation Llewellyn Formation Geologic Structure: Coal as a Source Rock for CBM: Gas-In-Place-Data Thermal