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Wednesday, May 6, 2020 | History

2 edition of Redefining the Lower Cretaceous stratigraphy within the central Utah Foreland Basin found in the catalog.

Redefining the Lower Cretaceous stratigraphy within the central Utah Foreland Basin

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  • 20 Currently reading

Published by Utah Geological Survey in Salt Lake City, UT .
Written in English

    Places:
  • Utah,
  • Juab County.,
  • Sanpete County.
    • Subjects:
    • Geology, Stratigraphic -- Cretaceous.,
    • Geology -- Utah -- Juab County.,
    • Geology -- Utah -- Sanpete County.

    • Edition Notes

      Includes bibliographical references (p. 17-18).

      Statementby Douglas A. Sprinkel ... [et al.].
      SeriesSpecial study / Utah Geological Survey ;, 97, Special study (Utah Geological Survey) ;, 97.
      ContributionsSprinkel, Douglas A.
      Classifications
      LC ClassificationsTN24.U8 A315 vol. 97
      The Physical Object
      Paginationvi, 21 p. :
      Number of Pages21
      ID Numbers
      Open LibraryOL6832019M
      ISBN 101557916438
      LC Control Number00325684
      OCLC/WorldCa42947403

      Author by: Christopher J. Schmidt Languange: en Publisher by: Geological Society of America Format Available: PDF, ePub, Mobi Total Read: 94 Total Download: File Size: 47,6 Mb Description: This volume emphasizes the interaction of the Cordilleran thrust belt and Rocky Mountain foreland in studies of regional structural geology, geophysics, and sedimentology from west-central. Keywords: sequence stratigraphy, foreland basins, fold and thrust belts, progradation, Book Cliffs, Utah. INTRODUCTION Several controversies have emerged in foreland-basin stratigraphy since the mids, and two key questions are at the heart of these debates. (1) Does coarse-grained detritus reflect intensified tectonic ac-.

      @article{osti_, title = {Stratigraphic overview of upper Cretaceous (early Campanian-Late Maestrichtian) Montana Group, Powder River basin, Wyoming: implications for complex interplay between eustatic sea level fluctuations, sedimentation rates, and intraforeland basin subsidence}, author = {Gustason, E.R. and Devine, P.E. and McClurg, J. and Rappold, C.J.}, abstractNote = {Isopach . @article{osti_, title = {The sequence stratigraphy of the latest Cretaceous sediments of northern Wyoming: The interplay of tectonic and eustatic controls on foreland basin sedimentation}, author = {Hicks, J.F. and Tauxe, L.}, abstractNote = {A west-east chronostratigraphic correlation has been made of the latest Cretaceous sediments of northern Wyoming.

        Sequence stratigraphy, a branch of sedimentary stratigraphy, uses the order strata accumulated in along with a framework of major depositional and erosional surfaces to interpret the depositional setting of clastic and carbonate sediments from continental, marginal marine, basin margins and down-slope settings of basins. Spieker, E.M. (editor), , The transition between the Colorado Plateau and the Great Basin in central Utah: Utah Geological Society, Guidebook to the geology of Utah, no. 4, p. Summary: Is a thick mass of coarse rubble, all of Colorado age, derived from nearby mountains and dumped into a foredeep.


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Redefining the Lower Cretaceous stratigraphy within the central Utah Foreland Basin Download PDF EPUB FB2

Redefining the Lower Cretaceous stratigraphy within the central Utah Foreland Basin (Special study / Utah Geological Survey) on *FREE* shipping on qualifying offers. Lower Cretaceous strata exposed in the foreland basin of central Utah.

Additional Physical Format: Online version: Redefining the Lower Cretaceous stratigraphy within the central Utah Foreland Basin. Salt Lake City, UT: Utah Geological Survey, PDF | OnDouglas A Sprinkel and others published REDEFINING THE LOWER CRETACEOUS STRATIGRAPHY WITHIN THE CENTRAL UTAH FORELAND BASIN REDEFINING THE LOWER CRETACEOUS STRATIGRAPHY.

REDEFINING THE LOWER CRETACEOUS STRATIGRAPHY WITHIN THE CENTRAL UTAH FORELAND BASIN Download Redefining The Lower Cretaceous Stratigraphy Within The Central Utah Foreland Basin ebook PDF or Read Online books in PDF, EPUB, and Mobi Format.

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General Information. Title: Redefining the Lower Cretaceous stratigraphy within the central Utah foreland basin Author(s): Sprinkel, D.A., Weiss, M.P., Fleming, R.W. REDEFINING THE LOWER CRETACEOUS STRATIGRAPHY WITHIN THE CENTRAL UTAH FORELAND BASIN by Douglas A.

Sprinkel1, Malcolm P. Weiss2, Robert W. Fleming3, and Gerald L. Waanders4 ABSTRACT Lower Cretaceous strata exposed in the foreland basin of central Utah were divided into two lithostratigraphic units, the Cedar Mountain and San Pitch Formations. Together these. Lower Cretaceous strata exposed in the foreland basin of central Utah were divided into two lithostratigraphic units, the Cedar Mountain and San Pitch Formations.

Together these formations correlate with both the Cedar Mountain Formation exposed on the San Rafael Swell and the lower part of the Canyon Range Conglomerate exposed in the Canyon.

Geologic unit mapped in Utah: Indianola Formation. Hintze, L.F.,Geologic map of Utah: Utah Geological and Mineral Survey, scaleIn the study area, within the central foreland basin setting, most deposition of Lower and Upper Cretaceous rocks was between the lithologic end members of very coarse terrigenous clastics and the open marine chalks.

With few exceptions, Creta-ceous rocks in the study area consist of fine- to medium-grained sandstone, siltstone, mudstone, and by: 8.

Wellbore to Outcrop Correlation and Sequence Stratigraphic Evaluation of the Late Cretaceous Lower Ferron Sandstone in East Central Utah, U.S.A.* Tore Klausen1 and John A. Howell2 Search and Discovery Article # () Posted Febru Author: Tore Klausen, John A.

Howell. Subsurface Stratigraphic Cross Sections of Cretaceous and Lower Tertiary Rocks in the Southwestern Wyoming Province, Wyoming, Colorado, and Utah By Thomas M.

Finn and Ronald C. Johnson U.S. Geological Survey Digital Data Series DDS–69–D U.S. Department of. Stratigraphic Evolution of Foreland Basins - A strong case can be made that foreland basins are where the casual links between sedimentation and tectonic events were first recognized, as evidenced by the interpretations of geologists working in classic foreland areas.

Download Citation | HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A.

| This study presents high. Progressive unroofing in the fold-thrust belt should lead to an “inverse” stratigraphic sampling of the source in foreland basin sediments as illustrated in Figure Such a pattern is well developed in the Cretaceous foreland basin deposits in eastern Utah (Lawton, ).

In this basin, early stages of uplift and erosion resulted in. Late Cretaceous depositional systems in the central Utah segment of the foreland basin, and allows inferences to be made regarding fore-land basin dynamics.

In particular, thrust tectonics is postulated to have played a major role in governing the architecture of Late Cre-taceous strata in central Utah. Marked along-strike thickening of the. Michael H. Gardner, "Tectonic and Eustatic Controls on the Stratal Architecture of Mid-Cretaceous Stratigraphic Sequences, Central Western Interior Foreland Basin of North America", Stratigraphic Evolution of Foreland Basins, Steven L.

Dorobek, Gerald M. Ross. Middle to late Campanian strata of the Book Cliffs, Utah record the Late Cretaceous deposition of three clastic wedges in the North American Cordilleran foreland basin east of the Sevier thrust belt. Variations in wedge geometries provide an opportunity to evaluate the effects of sediment supply versus accommodation on foreland basin stratal : N.

Bartschi, J. Saylor, T. Lapen, P. Copeland, M. Blum. PEABODY MUSEUM OF NATURAL HTSTORY YALE UNIVERSITY Stratigraphy and Paleontology of the Cloverly Formation n \iriiiii (Lower Cretaceous) of the Bighorn Basin Area, Wyoming and Montana John H.

Ostrom \* BULLETIN NO. 35 ORIGINALLY PUBLISHED AUGUST FACSIMILE EDITION APRI L 5 NEW HAVEN, CONNECTICUT.

Author by: Douglas A. Sprinkel Languange: en Publisher by: Utah Geological Survey Format Available: PDF, ePub, Mobi Total Read: 70 Total Download: File Size: 40,9 Mb Description: Lower Cretaceous strata exposed in the foreland basin of central Utah were divided into two lithostratigraphic units, the Cedar Mountain and San Pitch er these formations correlate with.

Abstract Stratigraphic and provenance data from Lower Cretaceous rocks in Utah and Colorado and structural evidence from the Sevier belt in west‐central Utah allow recognition of the ties between early thrust‐belt evolution and foreland‐basin system development.

Regional isopach patterns of Lower Cretaceous strata define foreland‐basin system by:. Field guide to geologic excursions in Utah and adjacent areas of Nevada, Idaho, and Wyoming, G.S.A.

field guide, Rocky Mountain Section: Redefining the Lower Cretaceous stratigraphy within the central Utah Foreland basin D. A. Sprinkel: Quaternary geology of the Scipio Valley area, Millard and Juab Counties, Utah.Stratigraphy.

The Sego Sandstone and Neslen Formation form part of the Upper Cretaceous Mesaverde Group and crop out along the Book Cliffs of eastern Utah and western Colorado ().They form a complex of estuarine and non-marine sandstone, mudstone and coal, which are interbedded to the northwest with alluvial strata of the Upper Castlegate Sandstone (), and to the southeast in Colorado Cited by: The world famous stratigraphy in the Cretaceous Foreland Basin of the North American Rockies has been producing commercial quantities of oil and gas for years and will likely still be targeted by explorers years from now.

There are few better places for a geologist to work with beautiful exposures of important reservoir rocks often only miles from locations where the same rocks are.