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Stratigraphic Framework And
U.S. DEPARTMENT OF THE INTERIOR SCIENTIFIC INVESTIGATIONS MAP 2916 U.S. GEOLOGICAL SURVEY (SHEET 2 OF 2) Explanatory pamphlet accompanies map 82° 80° 78° 82° 80° 78° Table 1.—Wells used to construct cross section F–F '. Refer to figure 2 for well locations. Also shown are perforated intervals, initial production flow per day, and reservoir names. Lake Ontario [Reservoirs: C, “Clinton” sandstone; M, Medina sandstone; T, Tuscarora Sandstone. Oil and gas production terms: AF, after hydrofracturing; BO, barrels of oil; BW, barrels of water; MCFG, thousand cubic feet of gas; N, natural (no stimulation of reservoir); OH, open hole (no casing with perforations); P&A, plugged and abandoned; TA, temporarily abandoned; TO, trace of oil; TW, trace of water. Well that connects section F–F ' with section A–A' shown as 81, A–A' (54); number in parentheses refers to well 54 on section A–A' . A' Lake Ontario —, no data] A' Map American Township Date of Perforated or open hole Initial production flow Orleans Company Lease County/State Reservoirs no. Petroleum (7.5–min quadrangle) log run interval (depth in ft) of natural gas, oil, Niagara Institute no. and water (per day) Ontario Erie 1 34–089–22051 Southern Triangle Oil Co. No. 1 Swetnam Comm. Licking/Ohio Burlington 11–27–63 — P&A, 11–29–63; 1,200 MCFG, — N (from “Clinton” in nearby well No. 1 Houck, 6–30–1905) Lake Erie 2 34–089–22300 Lake Shore Pipeline Co. No. 1 Shipley Licking Burlington 12–13–65 — P&A, 12–12–65; 1,200 MCFG, — B N (from “Clinton” in nearby well No. -
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EVALUATION OF POTENTIAL STACKED SHALE-GAS RESERVOIRS ACROSS NORTHERN AND NORTH-CENTRAL WEST VIRGINIA ABSTRACT Jessica Pierson Moore1, Susan E. Pool1, Philip A. Dinterman1, J. Eric Lewis1, Ray Boswell2 Three shale-gas units underlying northern and north-central West Virginia create opportunity for one horizontal well pad to produce from multiple zones. The Upper Ordovician Utica/Point Pleasant, Middle Devonian Marcellus, and Upper Devonian Burket/Geneseo 1 West Virginia Geological & Economic Survey, 2 U.S. DOE National Energy Technology Laboratory construction of fairway maps for each play. Current drilling activity focuses on the Marcellus, with more than 1,000 horizontal completions reported through mid-2015. Across northern West Virginia, the Marcellus is 40 to 60 ft. thick with a depth range between 5,000 and 8,000 ft. Total Organic Carbon (TOC) REGIONAL GEOLOGY is generally 10% or greater. Quartz content is relatively high (~60%) and clay content is low (~30%). Reservoir pressure estimates STRUCTURAL CROSS-SECTION FROM HARRISON CO., OHIO TO HARDY CO., WEST VIRGINIA range from 0.3 to 0.7 psi/ft and generally increase to the north. Volumetric assessment of the Marcellus in this area yields preliminary NW SE 81° 80° 79° 78° 1 2 3 4 5 original gas-in-place estimates of 9 to 24 Bcf/mi2. OH WV WV WV WV Pennsylvania Figure 2.—Location of seismic sections, wells, and major basement Harrison Co. Marshall Co. Marion Co. Preston Co. Hardy Co. 34-067-20103 47-051-00539 47-049-00244 47-077-00119 47-031-00021 UTICA SHALE PLAY GR 41 miles GR 36 miles GR 27 miles GR 32 miles GR Westmoreland The Burket /Geneseo interval is approximately 15 to 40 ft thick across the fairway. -
Proterozoic Paleozoic Cambrian Ordovician Silurian Devonian
Approximate location of Burley No. 1 well Seismic Stratigraphic Extensional and Thrust Age West Formation or Group Name East Lithology Packages Orogenic Events Sheets Perm. Lower Upper Post-Pottsville rocks, undivided Pottsville Group and Middle post-Pottsville rocks Alleghanian orogeny Penn. Lower Pottsville Group Upper Greenbrier Limestone and Mauch Chunk Group Greenbrier Limestone Miss. Lower Berea Sandstone, Sunbury Shale, and Price Formation Venango Group Venango Group (Formation) Hampshire Formation and Riceville Formation Chagrin Shale Bradford Group Bradford Group Huron Mbr. of Greenland Gap Group the Ohio Shale Upper Salina sheet Acadian orogeny Java Formation Angola Shale Member Devonian West Falls Elk Group Formation Rhinestreet Shale Member Brallier Formation Elk Group Sonyea Formation Genesee Formation Harrell Shale Middle Tully Limestone, Hamilton Group, Marcellus Shale, and Onondaga Limestone Hamilton Group Lower Oriskany Sandstone and Helderberg Group Upper Salina Group (includes salt beds) Salina Group, Tonoloway Limestone, and Wills Creek Formation and Wills Creek Formation Salina Group Paleozoic Lockport Dolomite and Keefer Sandstone McKenzie Limestone and Keefer Sandstone Silurian Rose Hill Formation Lower Reedsville- Tuscarora Sandstone Taconic orogeny Martinsburg Juniata Formation Juniata Formation sheet Oswego Sandstone Upper Reedsville Shale (Utica Shale at base) Reedsville Shale Trenton Limestone Trenton Limestone Black River Limestone Middle Ordovician Knox unconformity Beekmantown Group Beekmantown Group ? Passive continental Lower Rome- margin modified Waynesboro Upper sandstone member of the Copper Ridge Dolomite of the Knox Group by Rome trough sheet Upper extension Copper Ridge Dolomite of the Knox Group Knox Group and Middle pre-Knox rocks Conasauga Group and Rome Formation Cambrian Lower Autochthonous Grenvillian basement Grenvillian Grenvillian basement basement Proterozoic Figure 3.--Correlation chart of Paleozoic and Proterozoic rocks in the study area and associated thrust sheets. -
In Weight Percent
Bass Islands Dolomite Keyser Limestone (lower) and Salina Group Keyser Limestone (lower) and Salina Group Big Mountain Shale through Tonoloway Limestone Bass Islands Dolomite Bass Islands Dolomite Bass Islands Dolomite Bass Islands Dolomite Bass Islands Dolomite and Camillus Shale Bass Islands Dolomite and Camillus Shale Bass Islands Dolomite and Camillus Shale Bass Islands Dolomite and Camillus Shale Bass Islands Dolomite through Salina Group Bass Islands Dolomite and Salina Group Bass Islands Dolomite and Salina Group Bass Islands Dolomite and Salina Group Bass Islands Dolomite through Tonoloway Limestone Bass Islands Dolomite through Tonoloway Limestone Bass Islands Dolomite and Camillus Shale Keyser Formation Keyser Formation and Camillus Shale Keyser Limestone (lower) through Wills Creek Formation Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Camillus Shale Syracuse Formation Syracuse Formation Syracuse Formation Syracuse Formation Syracuse Formation Syracuse Formation Syracuse Formation Syracuse Formation Syracuse Formation Syracuse Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation Vernon Formation -
Xsec A-A Sht1of2 Layout FINAL V
U.S. DEPARTMENT OF THE INTERIOR SCIENTIFIC INVESTIGATIONS MAP 3425 U.S. GEOLOGICAL SURVEY (SHEET 1 OF 2) Explanatory pamphlet accompanies map A Ontario Allegheny Lowlands Plateau province province SEVERNE WATKINS-BEAVER LODI POINT FIRTREE DAMS ALPINE VAN ETTEN ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE GLENORA SYNCLINE UNNAMED COHOCTON CORBETT POINT ENFIELD CAYUTA SYNCLINE SYNCLINE SYNCLINE SYNCLINE SYNCLINE Bend in section Bend in section Bend in section New York W SE Oatka Genesee NW SE Canisteo NW SW Pennsylvania Black Creek River Canaseraga River Tuscarora Creek Creek Creek FEET MILES 0 10 20 30 40 50 60 70 80 90 3,000 1 2 3 4 5 6 William Duchscherer, Jr. E.F. Blair and Associates NYS Natural Gas Company E.F. Blair and Associates Bowdoin Storage Service Inc. NYS Natural Gas Company No. 1 J. Klotzbach No. 1 L. Tyler No. 1 Albert McClurg No. 1 Arthur N. Kennedy No. 1 Hubbard No. 1 Robert Olin API No. 31-037-05117 API No. 31-037-04593 API No. 31-051-04552 API No. 31-051-04630 API No. 31-101-21496 API No. 31-101-03924 Genesee Co., New York Genesee Co., New York Livingston Co., New York Livingston Co., New York Steuben Co., New York Steuben Co., New York Perrysburg Formation Dunkirk Dunkirk Shale Shale 2,000 Member Wiscoy Sandstone Member Java Perrysburg West River Shale, Nunda Wiscoy Sandstone Member Formation Formation Genundewa Sandstone Member unnamed Pipe Creek 0 Pipe Creek shale member Limestone, Penn Member Shale Member Shale Member Perrysburg Yan Shale, and rmation Formation 0 Dun West River Shale, Java Fo kirk -
Unraveling the Central Appalachian Fold-Thrust Belt, Pennsylvania: the Power of Sequentially Restored Balanced Cross Sections for a Blind Fold-Thrust Belt
Unraveling the central Appalachian fold-thrust belt, Pennsylvania: The power of sequentially restored balanced cross sections for a blind fold-thrust belt Peter B. Sak1, Nadine McQuarrie2,*, Benjamin P. Oliver2,*, Natasha Lavdovsky2, and Margaret S. Jackson1,* 1Department of Earth Sciences, Dickinson College, Carlisle, Pennsylvania 17013, USA 2Department of Geosciences, Princeton University, Princeton, New Jersey 08540, USA ABSTRACT Anticlinorium, the northernmost structure of example of a blind thrust system. At its north- the fold-thrust belt that cuts upsection from ernmost end, the fold-thrust belt sweeps east- We present a kinematic model for the the Cambrian Waynesboro Formation to the ward, creating the broad arc of the Pennsylvania sequential development of the Appalachian Silurian Salina décollement. Because the fault salient (Fig. 1). Although previous research in fold-thrust belt (eastern U.S.) across a clas- that cores the Nittany Anticlinorium can only the central Appalachians has made considerable sic transect through the Pennsylvania salient. facilitate 10 km of shortening on the plateau, progress toward quantifying how shortening New map and strain data are used to create an early history of Appalachian Plateau LPS is distributed among microscopic (e.g., Smart a balanced geologic cross section from the in Silurian and younger rocks is required to et al., 1997; Thorbjornsen and Dunne, 1997), southern edge of the Valley and Ridge Prov- balance the section. We propose that the addi- mesoscopic (e.g., Smart et al., 1997; Hogan -
A New Lower Devonian Arthrodire (Placodermi) from the NW Siberian Platform
Estonian Journal of Earth Sciences, 2013, 62, 3, 131–138 doi: 10.3176/earth.2013.11 A new Lower Devonian arthrodire (Placodermi) from the NW Siberian Platform Elga Mark-Kurik Institute of Geology at Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia; [email protected] Received 24 August 2012, accepted 5 November 2012 Abstract. A new genus and species of arthrodires, Eukaia elongata (Actinolepidoidei, Placodermi), is described from the Lower Devonian, ?Pragian of the Turukhansk region, NW Siberian Platform. A single specimen of the fish, a skull roof, comes probably from the lower part of the Razvedochnyj Formation. The occurrence of an actinolepidoid arthrodire in the Early Devonian of this area of Siberia is unexpected. Eukaia shows some distant relationship with the genus Actinolepis, but several features indicate similarity to representatives of other arthrodires. Key words: actinolepidoid arthrodire, placoderm, Lower Devonian, ?Pragian, NW Siberian Platform. INTRODUCTION (Fig. 1). The first two units are Lochkovian in age, the lower part of the Razvedochnyj Fm belongs to the Pragian The northwestern part of the Siberian Platform in the and the upper part of the Razvedochnyj Fm plus the lower Russian Arctic is well known for rich and amphiaspidid- part of the Mantura Fm to the Emsian (Matukhin 1995). dominated Early Devonian fish faunas. One of the The Zub Fm (up to 150 m thick) consists of carbonaceous- important areas where these faunas have been discovered argillaceous and sulphate rocks. Invertebrates and fossil is the near-Yenisej zone of the Tunguska syneclise fishes, e.g. a cyathaspidid Steinaspis, are comparatively (Krylova et al. -
Morphology and Histology of Acanthodian Fin Spines from the Late Silurian Ramsasa E Locality, Skane, Sweden Anna Jerve, Oskar Bremer, Sophie Sanchez, Per E
Morphology and histology of acanthodian fin spines from the late Silurian Ramsasa E locality, Skane, Sweden Anna Jerve, Oskar Bremer, Sophie Sanchez, Per E. Ahlberg To cite this version: Anna Jerve, Oskar Bremer, Sophie Sanchez, Per E. Ahlberg. Morphology and histology of acanthodian fin spines from the late Silurian Ramsasa E locality, Skane, Sweden. Palaeontologia Electronica, Coquina Press, 2017, 20 (3), pp.20.3.56A-1-20.3.56A-19. 10.26879/749. hal-02976007 HAL Id: hal-02976007 https://hal.archives-ouvertes.fr/hal-02976007 Submitted on 23 Oct 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Palaeontologia Electronica palaeo-electronica.org Morphology and histology of acanthodian fin spines from the late Silurian Ramsåsa E locality, Skåne, Sweden Anna Jerve, Oskar Bremer, Sophie Sanchez, and Per E. Ahlberg ABSTRACT Comparisons of acanthodians to extant gnathostomes are often hampered by the paucity of mineralized structures in their endoskeleton, which limits the potential pres- ervation of phylogenetically informative traits. Fin spines, mineralized dermal struc- tures that sit anterior to fins, are found on both stem- and crown-group gnathostomes, and represent an additional potential source of comparative data for studying acantho- dian relationships with the other groups of early gnathostomes. -
Ptyctodontid Fishes (Vertebrata, Placodermi) from the Late Devonian Gogo Formation, Western Australia, with a Revision of the European Genus Ctenurella 0Rvig, 1960
Ptyctodontid fishes (Vertebrata, Placodermi) from the Late Devonian Gogo Formation, Western Australia, with a revision of the European genus Ctenurella 0rvig, 1960 John A. LONG Department of Earth and Planetary Sciences, The Western Australian Museum, Francis Street, Perth, Western Australia, 6000 (Australia) Long J. A. 1997. — Ptyctodontid fishes (Vertebrata, Placodermi) from the Late Devonian Gogo Formation, Western Australia, with a revision of the European genus Ctenurella 0rvlg, 1960. Geodiversitas 19 (3) : 515-555. ABSTRACT A new, almost complete specimen of the ptyctodontid placoderm Campbellodus decipiens Miles et Young, 1977 enables description of the skull toof, trunk shield, visceral skeleton, pelvic girdle, dermal scale cover, and parts of the vertebtal column. A new reconstruction of the head shield of Ctenurella gladbachensis 0rvig, 1960 from Bergisch-Gladbach permits this taxon to be genetically defined from the Gogo species pteviously referred to that genus. The Gogo form is here referred to Austroptyctodus n.g. A new spe KEYWORDS cimen of Austroptyctodus gardineri Miles et Young, 1977, together with new Ptyctodontida, observations of Chelyophorus verneuili Agassiz, 1844 and Ctenurella gladba Devonian, chensis 0rvig, 1960, shows new information fot the endocranium, the hyoid Placodermi, Gogo, arch and visceral skeleton, identifying the previously identified "metaptery- Australia, goid" elements as paired nasal bones. The large visceral skeleton bone poste Austroptyctodus n.g., rior to the jaw joint in ptyctodontids is here identified as an elongated Ctenurella, Chelyophorus. interhyal. RESUME Une nouvelle description du toit crânien, de la cuirasse thoracique, du sque lette viscéral, de la ceinture pelvienne, de l'écaillure et de quelques éléments de la colonne vertébtale est proposée à partit d'un nouveau spécimen sub complet du ptyctodonte Campbellodus decipiens Miles et Young, 1977. -
Figure 2 (Pdf)
South North West East West East West East West East Eastern Kentucky Central West Virginia Eastern and Central Ohio Western and Central Pennsylvania Western and Central New York Age Stratigraphy from: Repetski and others (2008) Stratigraphy from: Ryder and others (2008, 2009) Stratigraphy from: Ryder and others (2008, 2009, 2010) Stratigraphy from: Berg and others (1983); Ryder and others (2010) Stratigraphy from: Repetski and others (2008) Era System Series (Ma) Valley Valley Rome Trough Rome Trough Rome Trough and Ridge Bedford Shale and Ridge Cleveland Member Venango Group Catskill Formation 359.2 Upper Devonian strata, undivided Ohio Shale Ohio Three Lick Bed Chagrin Shale equivalent rocks Chagrin Shale Bradford Group Foreknobs Formation Perrysburg Formation Shale Dunkirk Shale Member Huron Member of Ohio Shale Huron Member Elk Group Scherr Formation Upper Dunkirk Shale Java Formation Angola Shale Member Olentangy Shale (upper) Java Formation Java Formation Angola Shale Member West Falls West Falls Brallier Formation West Falls Angola Shale Member Formation Rhinestreet Shale Member Rhinestreet Shale Member of the Formation Rhinestreet Shale Member Formation Rhinestreet Shale Member Upper Devonian strata, undivided West Falls Formation 385.3 Sonyea and Genesee Formations, undivided Sonyea and Genesee Formations, undivided Sonyea and Genesee Formations, undivided Tully Limestone Tully Limestone Tully Limestone Mahantango Formation Mahantango Formation Moscow, Ludlowville, and Skaneateles Shales, undivided Hamilton Olentangy Shale (lower) -
A New Genus of Ptyctodont (Placodermi) from the Late Devonian of Baltic Area
Palaeontologia Electronica palaeo-electronica.org A new genus of ptyctodont (Placodermi) from the Late Devonian of Baltic area Kate Trinajstic, John A. Long, Alexander O. Ivanov, and Elga Mark-Kurik ABSTRACT The ptyctodont fish first referred to as Chelyophorus pskovensis Obruchev, 1947 from the Early Frasnian (Late Devonian) of Velikaya River, Pskov Region, Russia, is redescribed following the collection of additional materials from the contemporaneous Meeksi Mill outcrop, Estonia; Piskovichi and Snetnaya Gora outcrops, Russia and is here referred to Meeksiella gen. nov. With the exception of an articulated skull roof, the fossils occur as three dimensionally preserved isolated plates, and this has allowed accurate reconstruction of the dermal skeleton. A phylogenetic analysis resolves Meeksiella pskovensis gen. et sp. nov. within a previously recovered cluster of taxa which includes Ctenurella from Europe and Austroptyctodus from Western Australia, demonstrating global distribution of this clade during the Late Devonian. Kate Trinajstic. School of Molecular and Life Sciences, Curtin University, Bently, Western Australia 6845, Australia. [email protected] John Long. College of Science and Engineering, Flinders University, Sturt Rd, Bedford Park South Australia 5042, Australia; Research School of Earth Sciences, The Australian National University, Canberra, 0200, Australia. [email protected] Alexander O. Ivanov. Institute of Earth Sciences, St. Petersburg State University, St. Petersburg, 199178, Russia; Kazan Federal University, Kazan, Russia. [email protected] Elga Mark-Kurik. Department of Geology, Tallinn University of Technology, Tallinn, 19086 Estonia (posthumous) Keywords: new genus; Placoderm; Ptyctodont; phylogeny; Frasnian; Estonia; Pskov Region Submission: 16 May 2018. Acceptance: 18 March 2019. http://zoobank.org/A0E8E9EA-5A21-4F1F-9E5D-BAD240B4981F Trinajstic, Kate, Long, John A., Ivanov, Alexander O., and Mark-Kurik, Elga. -
Geologic Resources Inventory Ancillary Map Information Document
U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Directorate Geologic Resources Division Allegheny Portage Railroad National Historic Site and Johnstown Flood National Memorial GRI Ancillary Map Information Document Produced to accompany the Geologic Resources Inventory (GRI) Digital Geologic-GIS Data for Allegheny Portage Railroad National Historic Site and Johnstown Flood National Memorial alpo_jofl_geology.pdf Version: 5/11/2020 I Allegheny Portage Railroad National Historic Site and Johnstown Flood National Memorial Geologic Resources Inventory Map Document for Allegheny Portage Railroad National Historic Site and Johnstown Flood National Memorial Table of Contents Geologic Resourc..e..s.. .I.n..v..e..n..t.o...r.y.. .M...a..p.. .D...o..c..u..m...e...n..t............................................................................ 1 About the NPS Ge..o..l.o..g..i.c... .R..e..s..o..u...r.c..e..s.. .I.n..v..e..n...t.o..r.y.. .P...r.o..g...r.a..m............................................................... 3 GRI Digital Maps a..n...d.. .S..o..u...r.c..e.. .M...a..p.. .C...i.t.a..t.i.o...n..s.................................................................................. 5 Index Map .................................................................................................................................................................... 6 Digital Bedrock Geologic-GIS Map of Allegheny Portage Railroad National Historic Site, John..s..t..o..w...n.. .F..l.o..o...d.. .N...a..t.i.o..n..a..l. .M...e..m...o...r.i.a..l. .a..n..d... .V..i.c..i.n..i.t.y.................................................. 7 Map Unit Lis.t................................................................................................................................................................... 7 Map Unit De.s..c..r.i.p..t.io..n..s...................................................................................................................................................... 8 PNcc - Cas.s..e..l.m...a..n.