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1Sediments

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Book's cover

“Sediments” Metadata:

  • Title: Sediments
  • Author:
  • Language: English
  • Number of Pages: Median: 424
  • Publisher: ➤  Lewis Publishers - CRC - Taylor & Francis Group
  • Publish Date:
  • Publish Location: Ann Arbor

“Sediments” Subjects and Themes:

Edition Identifiers:

First Setence:

"The depletion of groundwater reserves is a growing concern in all member countries of the European Community."

Access and General Info:

  • First Year Published: 1990
  • Is Full Text Available: Yes
  • Is The Book Public: No
  • Access Status: Printdisabled

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    Wiki

    Source: Wikipedia

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    Vatera

    species (Artiodactyla, Bovidae) from the Late Pliocene of Greece. Annales Géologiques des Pays Helléniques 1e Série 39, A: 299-310. Dermitzakis MD, Eisenmann

    Richat Structure

    Holocene gravelly mud, muddy gravel, clayey sand, and silty sand. These sediments are often cemented into either concretionary masses or beds by calcrete

    Périgord noir

    Oligocene. The river valleys are infilled by alluvial sediments of Quaternary age. The Jurassic sediments belong to the inner platform facies and consist of

    Superficial deposits

    been mapped and may be separate sea-bed sediments. Most of these superficial deposits are unconsolidated sediments such as gravel, sand, silt and clay, and

    Cascade Peaks

    Géoportail (site en ligne) Source : cartes géologiques à l'échelle 1:50000 du Bureau de recherches géologiques et minières (site en ligne). Géoportail "Geologic

    Aquitaine Basin

    orientale. Guides géologiques régionaux. Masson. ISBN 2-225-44935-X. (in French) Vigneaux M. (1975). Aquitaine occidentale. Guides géologiques régionaux. Masson

    Petit Vignemale

    Coordinates verified via WikiMapia Source : cartes géologiques à l'échelle 1:50000 du Bureau de recherches géologiques et minières (site en ligne). Albert Dauzat

    Tafraout Group

    carbonate buildups developing in the Amezraï minibasin while terrigenous sediments persisted along its margins. This interval corresponds to a relative tectonic

    Calcaires du Bou Dahar

    Moving basinward, finer basinal sediments with green marls and peloidal wackestones emerge, suggesting periodic sediment starvation during the Early Pliensbachian

    Prades, Pyrénées-Orientales

    Neogene age), and by a zone of younger (Miocene and Quaternary) sediments (those sediments in fact covering the greater part of Prades commune). The Têt


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