Sedimentation in continental rifts
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Sedimentation in continental rifts

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Published by SEPM (Society for Sedimentary Geology) in Tulsa, Okla .
Written in English

Subjects:

  • Sedimentation and deposition,
  • Rifts (Geology),
  • Geology, Structural,
  • Alluvium,
  • Lake sediments

Book details:

Edition Notes

Statementedited by Robin W. Renault, Gail M. Ashley.
SeriesSpecial publication / SEPM (Society for Sedimentary Geology) -- no. 73, Special publication (SEPM (Society for Sedimentary Geology)) -- no. 73.
ContributionsRenault, Robin W., Ashley, Gail M.
The Physical Object
Pagination329 p. :
Number of Pages329
ID Numbers
Open LibraryOL15525901M
ISBN 101565760824
OCLC/WorldCa51199139

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F~G. Factors that determine the nature of the sedimentary record in continental rift settings. Long-term sedimentary sequences in rifts record the complex interplay among tectonics, climate. The group became known as the CREST working group, an acronym of Continental Rifts: Evolution, Structure and Tectonics, which not surprisingly became the title of this book. Continental Rifts: Evolution, Structure, Tectonics presents an overview of the present state of understanding and knowledge of the processes of continental rifting from a. Structural controls on sedimentation in continental rifts Article (PDF Available) in Geological Society London Special Publications 80(1) January with 1, Reads How we measure. In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics.. Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben with normal faulting and rift-flank uplifts mainly on one side. [citation needed] Where rifts remain above sea level they form a rift valley, which may be.

Many rifts commence with evenly distributed small extensional faults when they are commonly characterized by closed drainage and continental sedimentation with localized lacustrine facies. As continental rifts develop, source rocks commonly accumulate in deep lakes, especially when the rifting is rapid, and organic shales are commonly located. Sedimentation in Continental Rifts: SEPM Special Publication No. 73, Robin W. Renaut and Gail M. Ashley (Eds.), , Society for Sedimentary Geology (SEPM), Tulsa, USA, p. (Hardcover, SEPM members US $, non-mem-ber US $) ISBN: A good deal of what we know about the evolution of Earth's terres-. Publication date Series Special publication / SEPM (Society for Sedimentary Geology) ; no. 73 Note "October, " ISBN Expert petroleum geologists David Roberts and Albert Bally bring you Regional Geology and Tectonics: Phanerozoic Rift Systems and Sedimentary Basins, volume two in a three-volume series covering Phanerozoic regional geology and ence in analyzing and assessing rifts—locations where the Earth’s outer shell and crust have been stretched over time by seismic activity—is.

  A continental rift (Gregory, ; Quennell, , ) is a fault-bounded elongate trough under or near which the entire thickness of the lithosphere (see Lithosphere, Continental; Lithosphere, Mechanical Properties) has been reduced in extension during its as old mountain ranges may no longer have any topographic expression because of tectonic and/or . Gail M. Ashley is the author of Sedimentation in Continental Rifts ( avg rating, 0 ratings, 0 reviews, published ).   Continental rifts Victoria Brittain laments the west's failures of nerve in Africa Victoria Brittain. The book details how, in early , American pressure to avoid "another Somalia" allowed. Sedimentation in the African Rifts EDITED BY L.E. FROSTICK R.W. RENAUT Sedimentation and the Preservation of Fossil Faunas This book arises out of an international meeting held at the apartments of the Geological Society of London in September