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Detrital Zircon Provenance and Lithofacies Associations Of
geosciences Article Detrital Zircon Provenance and Lithofacies Associations of Montmorillonitic Sands in the Maastrichtian Ripley Formation: Implications for Mississippi Embayment Paleodrainage Patterns and Paleogeography Jennifer N. Gifford 1,*, Elizabeth J. Vitale 1, Brian F. Platt 1 , David H. Malone 2 and Inoka H. Widanagamage 1 1 Department of Geology and Geological Engineering, University of Mississippi, Oxford, MS 38677, USA; [email protected] (E.J.V.); [email protected] (B.F.P.); [email protected] (I.H.W.) 2 Department of Geography, Geology, and the Environment, Illinois State University, Normal, IL 61790, USA; [email protected] * Correspondence: jngiff[email protected]; Tel.: +1-(662)-915-2079 Received: 17 January 2020; Accepted: 15 February 2020; Published: 22 February 2020 Abstract: We provide new detrital zircon evidence to support a Maastrichtian age for the establishment of the present-day Mississippi River drainage system. Fieldwork conducted in Pontotoc County,Mississippi, targeted two sites containing montmorillonitic sand in the Maastrichtian Ripley Formation. U-Pb detrital zircon (DZ) ages from these sands (n = 649) ranged from Mesoarchean (~2870 Ma) to Pennsylvanian (~305 Ma) and contained ~91% Appalachian-derived grains, including Appalachian–Ouachita, Gondwanan Terranes, and Grenville source terranes. Other minor source regions include the Mid-Continent Granite–Rhyolite Province, Yavapai–Mazatzal, Trans-Hudson/Penokean, and Superior. This indicates that sediment sourced from the Appalachian Foreland Basin (with very minor input from a northern or northwestern source) was being routed through the Mississippi Embayment (MSE) in the Maastrichtian. We recognize six lithofacies in the field areas interpreted as barrier island to shelf environments. Statistically significant differences between DZ populations and clay mineralogy from both sites indicate that two distinct fluvial systems emptied into a shared back-barrier setting, which experienced volcanic ash input. -
129 the Use of Joint Patterns for Understanding The
129 THE USE OF JOINT PATTERNS FOR UNDERSTANDING THE ALLEGHANIAN OROGENY IN THE UPPER DEVONIAN APPALACHIAN BASIN, FINGER LAKES DISTRICT, NEW YORK TERRY ENGELDER Department of Geosciences, Pennsylvania State University University Park, Pennsylvania 16802 REGIONAL SIGNIFICANCE Abundantevidence (deformed fo ssils) for layer parallel shortening in western New York indicates the extent to which the Alleghanian Orogeny affected the Appalachian Plateau (Engelder and Engelder, 1977). In addition to low amplitude ( 100 m) long wave length ( 15 km) folds the Upper Devonian sediments of western New York contain many< mesoscopic-scale structures< including joints that can be systematically related to the Alleghanian Orogeny. Based on the nonorthogonality of cleavage and joints, the Alleghanian Orogeny in the Finger Lakes District of New York consists of at least two phases which Geiser and Engelder (1983) correlate with folding and cross-cutting cleavages in the Appalachian Valley and Ridge. To the southeast of the Finger Lakes District the earlier Lackawanna Phase is manifested by formation of the Lackawanna syncline and Green Pond outlier and the development of a northeast-striking disjunctive cleavage within the Appalachian Valley and Ridge mainly fromthe Kingston Arch of the Hudson Valley southwestward beyond Port Jervis, Pennsylvania (Fig. 1). Within the Finger Lakes Distric� New York, a Lackawanna Phase cleavage is absent; and one fm ds instead a cross-fold joint set which is consistent in orientation with a Lackawanna Phase compression. In bedded siltstone-shale sequences (i.e. the Genesee Group) this cross-fold joint set favors development in the siltstones 1# 2#). Main Phase (stops and The is seen as the refolding of the Lackawanna syncline and Green Pond outlier, as well as the development of the major folds in central Pennsylvania. -
Paleozoic 3: Alabama in the Paleozoic
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Paleozoic 3: Alabama in the Paleozoic Instructor: Dr. Douglas W. Haywick Last Time The Paleozoic Part 2 1) Back to Newfoundland 2) Eastern Laurentian Orogenies (Appalachians) 3) Other Laurentian Orogenies (Antler, Ouachita) (web notes 25) Laurentia (Paleozoic North America) Even though this coastline of Laurentia was a passive continental margin, a plate tectonic boundary was rapidly approaching… A B A B Laurentia (Paleozoic North America) The resulting Taconic Orogeny first depressed the seafloor Laurentia (localized transgression) and A Island arc then pushed previously deposited passive continental B margin sediments up into thrust fault mountains. Baltica There was only minimal metamorphism and igneous A intrusions. B Middle Ordovician Laurentia (Paleozoic North America) Laurentia Baltica Middle Ordovician Laurentia (Paleozoic North America) Laurentia Baltica Middle Ordovician Laurentia (Paleozoic North America) The next tectonic event (the Acadian Orogeny) was caused Laurentia by the approach of Baltica A B Baltica A B Baltica Baltica Late Ordovician Laurentia (Paleozoic North America) The Acadian Orogeny was more extensive and more intense (metamorphism and A lots of igneous intrusions) B A B Early Devonian Laurentia (Paleozoic North America) The Acadian Orogeny was more extensive and more intense (metamorphism and lots of igneous intrusions) Early Devonian Laurentia (Paleozoic North America) Lastly, along comes Gondwanna and…. …well you get the idea. A B B A B Mississippian Laurentia (Paleozoic North America) Lastly, along comes Gondwanna and…. …well you get the idea. A B B A B Pennsylvannian Suture zone Laurentia (Paleozoic North America) Lastly, along comes Gondwanna and…. …well you get the idea. -
CIRRICULUM VITAE May 2009 BAIRD, GORDON CARDWELL
CIRRICULUM VITAE May 2009 BAIRD, GORDON CARDWELL BIRTHPLACE AND DATE: Rochester, New York, October 6, 1946 CITIZENSHIP: U.S.A. EDUCATION: B.A. - Earlham College, 1969 M.S. (Geology) - University of Nebraska, 1971 Ph.D. (Geology) - University of Rochester, 1975 AREA OF SPECILIZATION: Paleontology, chronostratigraphy, sedimentology, basin history and basin evolution. POSITIONS: State University of New York at Binghamton: postdoctoral research associate, 1975-1976. Field Museum of Natural History: Assistant Curator of Fossil Invertebrates, Aug. 1976-Dec. 1981. State University College, Fredonia, New York: Assistant Professor of Geology, 1982-1988; promoted to Associate Professor (9/88) and to Full Professor (9/95). GRANTS: NSF GRANT 257-029 (with E.S. Richardson, Jr.) Paleoecology of the Mazon Creek biota. Total grant $50,000 for two years (1/1/79- 1/11/81). Principal investigator. American Chemical Society (Petroleum Research Fund) Summer Fellowship. Part of Grant (PRF 141-71-G2) received by Carlton Brett (University of Rochester). Fellowship total $4,000 for two years (11/82-11/84). NSF grant accepted (with C.E. Brett: principal investigator) Episodic sedimentary events in the Middle Devonian Hamilton Group of Western and Central New York. Total grant $115,000 for two years 8/1/84-7/31/86). NSF grant EAR 88 16856 accepted (with C.E. Brett: principal investigator) 6/88. Small-scale depositional sequences in a Middle Devonian 1 foreland basin. Total grant $99,000 for two years - $7,860 summary salary for Baird. American Chemical Society (Petroleum Research Fund) summer fellowship. Part of grant received by Carlton Brett and David Lehmann (University of Rochester). -
Character of the Alleghanian Orogeny in the Southern Appalachians: Part I
Character of the Alleghanian orogeny in the southern Appalachians: Part I. Alleghanian deformation in the eastern Piedmont of South Carolina DONALD T. SECOR, JR. Department of Geology, University of South Carolina, Columbia, South Carolina 29208 ARTHUR W. SNOKE Department of Geology and Geophysics, University of Wyoming, Laramie, Wyoming 82071 KENNETH W. BRAMLETT Shell Western E and P, Inc., Box 831, Houston, Texas 77001 OLIVER P. COSTELLO Samson Resources, 801 Travis Street, Suite 1630, Houston, Texas 77002 OLLIE P. KIMBRELL Soil & Material Engineers, Inc., 3025 McNaughton Drive, Columbia, South Carolina 29223 ABSTRACT ward, 1957) is a fundamental problem. This report summarizes results of new field work and outlines interpretations concerning late Paleozoic de- The eastern Piedmont Province in South Carolina contains a formation along the Fall Line in west-central South Carolina. This infor- sequence of Cambrian volcanic and sedimentary rocks that was pene- mation is essential to development of a more general analysis of the tratively deformed (Dj) and regionally metamorphosed (Mi) to the Alleghanian orogeny in the southern Appalachians (Secor and others, greenschist facies during the early and/or middle Paleozoic. The east- 1986). era Piedmont was subsequently affected by late Paleozoic (Allegha- nian) polyphase deformation (D2-D4) and regional metamorphism. The OVERVIEW earliest Alleghanian event (D2) is associated with amphibolite facies regional metamorphism and felsic plutonism in a mid-crustal infra- In the southeastern Piedmont, late Paleozoic deformation events af- structure at ca. 295-315 Ma. The gradational interface between infra- fected a region that had previously been strongly deformed in the early structure and overlying suprastructure contained a steep M2 and/or middle Paleozoic. -
Insights Into the Acadian Orogeny, New England Appalachians: a Provenance Study of the Carrabassett and Kittery Formations, Maine
Insights into the Acadian orogeny, New England Appalachians: a provenance study of the Carrabassett and Kittery formations, Maine Michael J. Dorais1*, Robert P. Wintsch2, Wendy R. Nelson3, and Michael Tubrett4 1. Department of Geological Sciences, Brigham Young University, Provo, Utah 84602, USA 2. Department of Geological Sciences, Indiana University, Bloomington, Indiana 47405, USA 3. Department of Geosciences, Penn State University, University Park, Pennsylvania 16802, USA 4. CREAIT Network, MicroAnalysis Facility, Inco Innovation Centre (MAF-IIC), Memorial University, St. John’s, Newfoundland A1B 3X5, Canada * Corresponding author: <[email protected]> Date received: 07 July 2008 ¶ Date accepted: 11 February 2009 ABSTRACT The Central Maine Basin and Merrimack Trough are Silurian basins that formed adjacent to or were accreted to the Laurentian margin during the Acadian orogeny. The Early Devonian Carrabassett Formation of the Central Maine Basin and the Kittery Formation of the Merrimack Trough have major and trace element compositions indica- tive of a passive continental margin provenance, not unlike the older formations of the Central Maine Basin that are thought to have been derived from Laurentian sources. However, both the Carrabassett and Kittery formations have paleocurrent indicators of outboard sources. The Carrabassett Formation is one of the youngest formations of the Central Maine Basin and was deposited just prior to the Acadian orogeny. The Carrabassett and Kittery formations have major and trace element concentrations suggestive of passive margin turbidites derived from intermediate to felsic sources, inconsistent with a juvenile Avalonian provenance. The Carrabassett Formation contains detrital zircon grains that match the ages of peri-Gondwanan Ganderia. Unlike the dominance of positive bulk-rock εNd values that are characteristic of Avalonia, Ganderia has negative εNd values that are a better match for the negative εNd values of the Carrabassett and Kittery formations. -
Early Jointing in Coal and Black Shale: Evidence for an Appalachian-Wide Stress field As a Prelude to the Alleghanian Orogeny
Early jointing in coal and black shale: Evidence for an Appalachian-wide stress field as a prelude to the Alleghanian orogeny Terry Engelder* ⎤ ⎥ Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA Amy Whitaker† ⎦ ABSTRACT means of stratigraphically controlled decolle- Early ENE-striking joints (present coordinates) within both Pennsylvanian coal and ment tectonics (Gates et al., 1988; Wise, Devonian black shale of the Central and Southern Appalachians reflect an approximately 2004). rectilinear stress field with a dimension Ͼ1500 km. This Appalachian-wide stress field (AWSF) dates from the time of joint propagation, when both the coal and shale were FRACTURE EVIDENCE FOR THE buried to the oil window during the 10–15 m.y. period straddling the Pennsylvanian- AWSF Permian boundary. The AWSF was generated during the final assembly of Pangea as a Along the Appalachian Mountains an ENE consequence of plate-boundary tractions arising from late-stage oblique convergence, joint set is the first to propagate in many out- where maximum horizontal stress, SH, of the AWSF was parallel to the direction of closure crops of Devonian through Pennsylvanian between Gondwana and Laurentia. After closure, the AWSF persisted during dextral slip rocks (e.g., Nickelsen and Hough, 1967; Nick- of peri-Gondwanan microcontinents, when SH appears to have crosscut plate-scale trans- elsen, 1979; Kulander and Dean, 1993; Pashin current faults at ϳ30؇. Following Ͼ10 m.y. of dextral slip during tightening of Gondwana and Hinkle, 1997). This early joint set strikes against Laurentia, the AWSF was disrupted by local stress fields associated with thrusting parallel to the orientation of the maximum on master basement decollements to produce the local orocline-shaped Alleghanian map horizontal stress, SH, in a stress field that was pattern seen today. -
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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. -
Paleozoic Evolution of the Appalachians
Paleozoic Evolution of the Appalachians: Tectonic Overview Three major tectonic episodes, all involving lateral accretion of terranes: deformation, terrane migration, accretion, and continental convergence 1. Ordovician Taconic Orogeny (~470-440 Ma) • collision of Laurentian margin with one or more magmatic arcs Shelburne Falls arc (475-470 Ma) and Bronson Hill arc (454-442 Ma) • or, continent-continent collision between Laurentia and proto-Andean region of Gondwana • slope & rise sediments thrust westward over shelf deposits 2. Devonian Acadian Orogeny (~420-360 Ma) • accretion of Avalon terrane southward continuation of Silurian Caledonian Orogeny (NW Europe) collision of Baltica with Laurentia to form Laurussia • deformation of Bronson Hill arc and sedimentary basins seaward of BH arc at least 3 pulses of deformation • oblique accretion of Avalon and other terranes(?) much strike-slip displacement but also subduction (coastal volcanics) • large mountains erosion creates thick clastic wedge (Catskills and Poccono Mtns.); thinned westward toward cratonic interior 3. Pennsylvansylvanian-Permian Alleghenian Orogeny (~325- 275 Ma) • collision with Gondwanaland consolidation of supercontinent Pangea • extensive zone of deformation New England - Georgia & Alabama (Appalachian Mtns.) - Oklahoma, Arkansas (Ouachita Mtns.) - Texas (Marathon Mtns.) • side-effects: deep crustal shear in Mass., formation of Narragansett rift basin basement block faulting in western interior, uplift of ancestral Rockies "TECTONIC CYCLES" • recorded by the creation of foreland basins sedimentation in eastern New York • associated with tectonic uplift and deformation due to the accretion of island arcs to the east in Massachusetts (first the Ordovician Taconic Orogeny followed by the Devonian Acadian Orogeny: Ordovician Taconic Orogeny (generalized succession in eastern NY) Age Environment Lithology Formation late Ordovician deltaic and molasse Queenston Fm. -
(Acadian) Orogenic Events in Scotland John R Mendum British Geological Survey, Edinburgh
Late Caledonian (Scandian) and Proto-Variscan (Acadian) orogenic events in Scotland John R Mendum British Geological Survey, Edinburgh Abstract The later tectonic phases of the Caledonian Orogeny reflect the collision of Baltica and Laurentia. The result was the Scandian event in Silurian times, and the oblique docking of Eastern Avalonia with Scotland, generating deformation and metamorphism in the Southern Uplands. The exhumation of the Caledonide Orogen was then accompanied by sinistral transtensional faulting and emplacement of granitoid plutons. The Iapetus Ocean was finally closed, and subduction activity had migrated south to the Rheic Ocean by early Devonian times. Continental rifting and deposition of the Lower Old Red Sandstone fluvial-lacustrine succession, accompanied by basaltic-andesitic volcanism, occurred across Scotland. Deposition commenced in the late Silurian and continued through to Emsian times, when it was interrupted by the short-lived, northward-directed Acadian event. The resultant deformation and folding, a product of sinistral transpression, were focussed along the major pre-existing faults and shear zones. Evidence for Acadian transpressional movements along the Great Glen Fault (GGF) is found near Rosemarkie, where Moine psammites and semipelites are interleaved with Lewisianoid gneisses in a structural inlier. These lithologies are intruded by pink leucogranite veins that themselves show evidence of two phases of ductile deformation and folding. U-Pb monazite and zircon ages show that the leucogranites were emplaced at c. 399 Ma. Leucogranite intrusion and subsequent deformation are interpreted to have occurred during oblique extrusion of the inlier as an elongate ‘pip’, generated at a northwestward step-over that developed on the GGF during the Acadian Event. -
Marcellus Shale,” Hamilton Group [email protected] 2045 Morse Rd., Bldg
Matthew S. Erenpreiss Ohio Department of Natural Resources, Division of Geological Survey Mapping the Regional Organic Thickness of the “Marcellus Shale,” Hamilton Group [email protected] 2045 Morse Rd., Bldg. C-2, Columbus, OH 43229-6693 ABSTRACT • Regional and statewide isopach maps Shale” in each county and township, where available; this newly compiled data and observing the “Marcellus ASHTABULA REFERENCES WILLIAMS FULTON LUCAS OTTAWA LAKE GEAUGA WOOD Lash, G.G., and Engelder, Terry, 2011, Thickness HENRY TRUMBULL have been developed for the Middle Devonian “Marcellus this approach allowed for an even distribution of control Shale” upper and lower units, net organic thickness SANDUSKY CUYAHOGA DEFIANCE ERIE LORAIN trends and sequence stratigraphy of the Middle PORTAGE HURON SUMMIT Devonian Marcellus Formation, Appalachian Basin— PAULDING SENECA MEDINA Shale” for use in assessing Ohio’s shale gas potential. points and more consistent correlations. This correlation was calculated and contoured. Additional data was also PUTNAM HANCOCK MAHONING Implications for Acadian foreland basin evolution: VAN WERT WYANDOT CRAWFORD RICHLAND ASHLAND WAYNE AAPG Bulletin, v. 95, no. 1, p. 61–103. Existing stratigraphic analyses of Devonian shales in Ohio expansion of the Hamilton Group, “Marcellus Shale,” collected from the state geological surveys of New York, ALLEN STARK COLUMBIANA Ohio Division of Geological Survey, 1988, Analysis of HARDIN MERCER CARROLL stratigraphic and production relationships of Devonian MARION AUGLAIZE HOLMES MORROW TUSCARAWAS shale gas reservoirs in Ohio–Final report October were used as the starting dataset, which was expanded and Onondaga Limestone was based on U.S. Geological Pennsylvania, and West Virginia to create a new regional LOGAN KNOX SHELBY UNION JEFFERSON COSHOCTON HARRISON DELAWARE 1985–November 1988 (prepared for Gas Research DARKE A’ Institute): Ohio Department of Natural Resources, CHAMPAIGN LICKING with additional geophysical logs that span the “Marcellus Survey cross sections published in Bulletin 1909. -
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