5 edition of Perspectives on the Eastern Margin of the Cretaceous Western Interior Basin (Special Paper (Geological Society of America)) found in the catalog.
by Geological Society of America
Written in English
|Contributions||Richard H. Hammond (Editor)|
|The Physical Object|
|Number of Pages||264|
Figure 3. Cretaceous stratigraphy of western Minnesota and adjoining South Dakota (modified from Setterholm, , fig. 8). The Dakota Formation (Fig. 4) and Graneros Shale were deposited within mostly fluvial, deltaic and nearshore environments, as the waters of the Western Interior Seaway first began to rise and encroach eastward across Minnesota in the late Albian to Cenomanian. Cretaceous strata in Arizona, New Mexico, and southern Colorado were deposited in the southern part of the asymmetric Western Interior basin and consist of east- and northeastward-prograding clastic wedges of shoreface sandstones and coastal-plain deposits separated by thick tongues of west- and southwestward-extending marine shale and, on the eastern shelf, by limestone.
THE MANCOS SHALE: IMPLICATIONS FOR LATE CRETACEOUS EVOLUTION OF THE WESTERN INTERIOR FORELAND BASIN OF CENTRAL UTAH, U.S.A. CHRIS M. EDWARDS,* JOHN A. HOWELL,** AND STEPHEN S. FLINT Stratigraphy Group, Department of Earth and Ocean Sciences, University of Liverpool, 4 Brownlow Street, Liverpool L69 3GP, U.K. e-mail: [email protected] The formation overlies the Cedar Mountain Formation, and underlies the Mancos Shale formation, thus occupying the position of sedimentary strata that have historically been called the Dakota term is no longer used for Cretaceous strata that were deposited on the western side of the Cretaceous Seaway.. In most areas, the Naturita Formation is composed of a lower unit of.
The Neuquén Basin is located on the eastern side of the Andes in Argentina (° S) and contains a thick rock succession recording the interplay between tectonics, sea level and volcanic. the eastern equivalent of the Upper Castlegate Sandstone. (Modified from Fouch et al. and Obradovich ) FIG. 2.—The study area is located on the western margin of the Cretaceous Interior Seaway, in what is now northwestern Colorado, indicated with the black rectangle (modified from Roberts and Kirshbaum ; Willis and Gabel ).
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Perspectives on the Eastern Margin of the Cretaceous Western Interior Basin Author(s) George W. Shurr; George W. Shurr Search for other works by this author on: GSW. Google Scholar. Greg A Perspectives on the Eastern Margin of the Cretaceous Western Interior Basin. Author(s): George W.
Shurr, Greg A. Ludvigson, Richard H. Hammond. Dale R. Setterholm, "The Cretaceous rocks of southwestern Minnesota: Reconstructions of a marine to nonmarine transition along the eastern margin of the Western Interior Seaway", Perspectives on the Eastern Margin of the Cretaceous Western Interior Basin, George W.
Shurr, Greg A. Ludvigson, Richard H. Hammond. Robert L. Ravn, Brian J. Witzke, "The mid-Cretaceous boundary in the Western Interior Seaway, central United States: Implications of palynostratigraphy from the type Dakota Formation", Perspectives on the Eastern Margin of the Cretaceous Western Interior Basin, George W.
Shurr, Greg A. Ludvigson, Richard H. Hammond. ISBN: X OCLC Number: Description: iv, pages: illustrations, maps ; 29 cm. Contents: Introductory remarks: perspectives on the eastern margin of the Cretaceous Western Interior Seaway / G.W. Shurr, G.A. Ludvigson and R.H.
Hammond --Cretaceous rocks from southwestern Montana to southwestern Minnesota, northern Rocky Mountains, and Great Plains. Vince Hamilton, "Sequence stratigraphy of Cretaceous Albian and Cenomanian strata in Kansas", Perspectives on the Eastern Margin of the Cretaceous Western Interior Basin, George W.
Shurr, Greg A. Ludvigson, Richard H. Hammond. Brian J. Witzke, Greg A. Ludvigson, "The Dakota Formation in Iowa and the type area", Perspectives on the Eastern Margin of the Cretaceous Western Interior Basin, George W. Shurr, Greg A. Ludvigson, Richard H. Hammond. Book review Full text access Perspectives on the eastern margin of the Cretaceous Western Interior Basin: G.W.
Shurr, G.A. Ludvigson and R.H. Hammond (Editors). Geological Society of America Special PaperGeological Society of America, Boulder, Colo., Paperback, iv + pp., U.S. $ (paperback), ISBN X. The western margin of the Western Interior Basin is composed of an important active explosive volcanic system (i.e., an Andean type magmatic belt).
Paleogeographic reconstruction of a typical segment of the proximal margin of the Western Interior Basin during the Aptian, at a time of sea-level lowstand, based on studies of the Mannville Group (Glauconite Formation) in west-central Alberta.
Modified from Rosenthal (). Download: Download full-size image; Figure Shurr, et al. (Eds.), Perspectives on the Eastern Margin of the Cretaceous Western Interior Basin, Geological Society of America Special Paper (), pp.
Google Scholar Elder and Kirkland, Sedimentary and ecosystem response to Late Cretaceous (Cenomanian - Turonian) paleoenvironmental events along the eastern margin of the Western Interior Seaway, Canada.
by Danielle Dionne A thesis submitted to the Faculty of Graduate and Post Doctoral Affairs in partial fulfillment of the requirements for the degree of Master of Science in. Stratigraphy, depositional environments, and sedimentary tectonics of the western margin, Cretaceous western interior seaway (eds Nations, J.
& Eat. The Late Cretaceous Western Interior Seaway as a model for oxygenation change in epicontinental restricted basins Article (PDF Available) in Earth-Science Reviews. Late Cretaceous palaeogeography of western North America was dominated by three tectonic belts that extended virtually the length of the Cordillera: (1) an Andean-type volcanic–plutonic magmatic arc on the west (i.e., Cordilleran Magmatic Arc), (2) a thin-skinned fold-and-thrust belt on the east (initiated in mid-Cretaceous time), and (3) a hinterland (zone of metamorphism, magmatism, and.
Within the Louann Salt Basin, the KPBD is divisible into eastern and western provinces on the basis of both regional and local trends in structure and thickness (Figures 6 and 7).
An easterly promontory exists on the eastern margin of the western province of the Louann Salt Basin, resulting in an irregular structural boundary between the two. The Western Interior Basin extends north–south over about 35° of latitude, from Texas to the Northwest Territories, a distance of more than 3, km.
the Cretaceous, and this, in turn, provides the basis The Western Interior Basin of North America (Figs. for detailed basin analysis.
1 and 2) is one of the greatest natural laboratories. () Mid-Cretaceous Fluvial Deposits of the Eastern Margin, Western Interior Basin: Nishnabotna Memeber, Dakota Formation; a Field Guide to the Cretaceous of.
In Perspectives on the Eastern Margin of the Cretaceous Western Interior Basin. Edited by G. Shurr, G. Ludvigson, and R. Hammond. Geological Society of America Special Papers, 43– Crossref, Google Scholar. The bulk of Cretaceous sedimentary rocks in the southern interior basin were deposited during the Cenomanian through middle Campanian interval, when peak eustatic sea level, high rates of thrusting in the Sevier orogenic belt, and rapid subsidence of the associated foreland basin provided extensive sediment accommodation along the western margin.
Andrew D. Miall, Initiation of the Western Interior foreland basin, Geology, 37, 4, (), (). Crossref Alexander P. Bump, Three‐dimensional Laramide deformation of the Colorado Plateau: Competing stresses from the Sevier thrust belt and the flat Farallon slab, Tectonics, 23, 1, ().Cretaceous Period, in geologic time, the last of the three periods of the Mesozoic Cretaceous began million years ago and ended 66 million years ago; it followed the Jurassic Period and was succeeded by the Paleogene Period (the first of the two periods into which the Tertiary Period was divided).
The Cretaceous is the longest period of the Phanerozoic Eon.The western margin of the Cretaceous Western Interior Seaway was Early results from the Upper Cretaceous strata of the Book Cliffs region, eastern Utah and western Colorado have revealed the out” into the basin. Study Area: Book Cliffs UT-CO + measured outcrop sections.
+ well logs.