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Thursday, July 30, 2020 | History

3 edition of Tracing tectonic deformation using the sedimentary record found in the catalog.

Tracing tectonic deformation using the sedimentary record

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  • 20 Currently reading

Published by Geological Society, AAPG Bookstore [distributor] in London, Tulsa, OK .
Written in English

    Subjects:
  • Geology, Structural.,
  • Sedimentary basins.,
  • Rock deformation.

  • Edition Notes

    Includes bibliographical references and index.

    Statementedited by T. McCann and A. Saintot.
    SeriesGeological Society special publication ;, no. 208
    ContributionsMcCann, T., Saintot, A.
    Classifications
    LC ClassificationsQE604 .T73 2003
    The Physical Object
    Paginationvi, 356 p. :
    Number of Pages356
    ID Numbers
    Open LibraryOL3769977M
    ISBN 101862391297
    LC Control Number2003501338
    OCLC/WorldCa52391598

    Tracing Tectonic Deformation Using the Sedimentary Record Tracing Tectonic Deformation Using the Sedimentary Record But even then, one figure will never be precise for very long; Everest rises roughly five millimetres each year due to tectonic deformation, and it occasionally moves when there are earthquakes, the most recent of which occurred in   Tectonics of Sedimentary Basins: Recent Advances focuses on key topics or areas where the greatest strides forward have been made, while also providing on-line access to the comprehensive book. Breakthroughs in new techniques are described in Section 1, including detrital zircon geochronology, cosmogenic nuclide dating, magnetostratigraphy.

    The interplay between volcanic and sedimentary processes is examined at this locality, while deformation of the basin makes it ideal for examining structural and tectonic aspects. Broader-scale tectonism is observed in the hanging wall (Ordovician carbonates) and footwall (Jurassic sandstone) rocks to the Keystone thrust fault. CiteScore: ℹ CiteScore: CiteScore measures the average citations received per document published in this title. CiteScore values are based on citation counts in a given year (e.g. ) to documents published in three previous calendar years (e.g. – 14), divided by the number of documents in these three previous years (e.g. – 14).

    The geologic record in stratigraphy, paleontology and other natural sciences refers to the entirety of the layers of rock is, deposits laid down by volcanism or by deposition of sediment derived from weathering detritus (clays, sands etc.). This includes all its fossil content and the information it yields about the history of the Earth: its past climate, geography, geology and the. Tracing Tectonic Deformation Using the Sedimentary Record. The Sedimentary Record of Sea-Level Change. Geochemistry: an Introduction. Geochemistry of Sediments and Sedimentary Rocks: Evolutionary Considerations to Mineral Deposit-Forming Environments. The World According to Rock. Bryan, T. Scott. Geysers: What They Are and How They Work.


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Tracing tectonic deformation using the sedimentary record Download PDF EPUB FB2

: Tracing Tectonic Deformation Using the Sedimentary Record (Geological Society Special Publication) (Geological Society Special Publication) (): T McCann and A Saintot: BooksAuthor: T McCann and A Saintot. Tracing Tectonic Deformation Using the Sedimentary Record (Geological Society Special Publication) T McCann and A Saintot The study of sediments and sedimentary basins in terms of their tectonic environment requires a multidisciplinary approach and has increasingly drawn both techniques and objectives from fields outside sedimentology.

Use up arrow (for mozilla firefox browser alt+up arrow) and down arrow (for mozilla firefox browser alt+down arrow) to review and enter to select. Click or Press Enter to view the items in your shopping bag or Press Tab to interact with the Shopping bag tooltipPrice: $   Tracing Tectonic Deformation Using the Sedimentary Record Edited by Tom McCann and Aline Saintot The Geological Society of London (UK), Special Publication No., p.

ISBNHardback, $ US (list price); $ US (GSL member price); $ US (AAPG/SEPM/GSA member price). McCann, T & Saintot, ANTracing tectonic deformation using the sedimentary record. Geological Society, London. Tracing tectonic deformation using the sedimentary by: for variations in the rate of tectonic subsidence occurring without any significant sea-level changes Index It is recommended that reference to all or part of this book should be made in one of the following ways: MCCANN, T.

& SAINTOT, A. (eds) Tracing Tectonic Deformation Using the Sedimentary Record. Scribd is the world's largest social reading and publishing site. The range of structural deformation within a region extends from the plate tectonic scale, governing, for example, rift initiation, to the basin scale, with the formation of basin- bounding faults.

The range of structural deformation within a region extends from the plate tectonic scale, governing, for example, rift initiation, to the basin scale, with the formation of basin-bounding faults. Tracing tectonic deformation using the sedimentary record: an overview Tectonic activity, on a range of scales, is a fundamental control on sedimentary activity.

The range of structural deformation within a region extends from the plate tectonic scale, governing, for example, rift initiation, to the basin scale, with the formation of basin.

Tectonic activity, on a range of scales, is a fundamental control on sedimentary activity. The range of structural deformation within a region extends from the plate tectonic scale, governing, for example, rift initiation, to the basin scale, with the formation of basin-bounding by: DANS is an institute of KNAW and NWO.

Driven by data. Go to page top Go back to contents Go back to site navigationCited by: Tracing tectonic deformation using the sedimentary record: an overview / T. McCann & A. Saintot --Middle Jurassic to Cretaceous extensional tectonics and sedimentation in the eastern external zone of the Betic Cordillera / E.

Fernandez-Fernandez [and others] --Sedimentary response to tectonics in extensional basins: the Pechelbronn Beds (Late Eocene to Early Oligocene) in the Northern Upper. Tracing tectonic deformation using the sedimentary record. [T McCann; A Saintot;] -- The study of sediments and sedimentary basins in terms of their tectonic environment requires a multidisciplinary approach and has increasingly drawn both techniques and objectives from fields.

The Sedimentary Record is published quarterly in online and paper formats by SEPM. It contains peer-reviewed science articles on topics of broad and current interest to the membership of SEPM, as well as shorter, editor-reviewed articles addressing a variety of topics, including Society business and.

tracing tectonic deformation using the sedimentary record (mccann, t.) (pulsar en la imagen para ver el libro). Also available: Tracing Tectonic Deformation Using the Sedimentary Record (Geological Society Special Publication) - ISBN Deformation of the Continental Crust: The Legacy of Mike Coward - Special Publication no - ISBN The Geological Society of LondonFounded inthe Geological Society of London is the oldest.

In: McCann T, Saintot A (eds) Tracing tectonic deformation using the sedimentary record. Geol Soc London Spec Publ – Google Scholar Golonka J, Krobicki M, Pająk J, Van Giang N, Zuchiewicz W (a) Global plate tectonics and paleogeography of Southeast Asia.

The term 'glacitectonite' was introduced by Banham as it was analogous to the metamorphic petrology term 'tectonite', which referred to the tectonic imprint in a rock unit as recorded by structures a. Section 4 examines the origin of plate interior basins, and the sedimentary record of supercontinent formation.

This book is required reading for any advanced student or professional interested in sedimentology, plate tectonics, or petroleum geoscience. Sedimentary Record of Regional Tectonic Events in the Mahogany Oil Shale Zone of the Lacustrine Green River Formation (Eocene), in Colorado and Utah Balázs Törő*, Brian R.

Pratt, Robin W. Renaut Department of Geological Sciences, University of Saskatchewan, Canada Summary.In: Tracing Tectonic deformation using the Sedimentary Record, Eds. McCann. (Geological Society of London, Special Publication)", abstract = "The Oligocene to Miocene Tertiary Piedmont Basin (TPB) is located in the NW part of Italy at the junction between the Apennine and the Alpine thrust belts.Quaternary sedimentary record in the northern Okinawa Trough indicates the tectonic control on depositional environment change.

Along with the deformation of the Asian continent and the westward subduction of the Pacific plate during the late Cenozoic Based on previous studies of sediment source tracing in the northern Okinawa Trough.