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Quantitative geology of late Jurassi...
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SpringerLink (Online service)
Quantitative geology of late Jurassic epicontinental sediments in the Jura Mountains of Switzerland
Record Type:
Language materials, printed : Monograph/item
Title/Author:
Quantitative geology of late Jurassic epicontinental sediments in the Jura Mountains of Switzerland/ by Reinhart A. Gygi.
Author:
Gygi, Reinhart A.
Published:
Basel :Springer Basel : : 2012.,
Description:
213 p. :ill., digital ; : 24 cm.;
Contained By:
Springer eBooks
Subject:
Sedimentation and deposition - Jura Mountains (France and Switzerland) -
Online resource:
http://dx.doi.org/10.1007/978-3-0348-0136-2
ISBN:
9783034801362 (electronic bk.)
Quantitative geology of late Jurassic epicontinental sediments in the Jura Mountains of Switzerland
Gygi, Reinhart A.
Quantitative geology of late Jurassic epicontinental sediments in the Jura Mountains of Switzerland
[electronic resource] /by Reinhart A. Gygi. - Basel :Springer Basel :2012. - 213 p. :ill., digital ;24 cm.
1 Previous Work -- 2 What can be measured, calculated, or be quantified by comparison -- 3 Paleogeography and paleoclimate -- 4 Sedimentation -- 5 Sea level variations -- 6 Hermatypic coral assemblages: growth form, spatial distribution, and paleobathymetry -- 7 Age and time correlation of sediments -- 8 Rates of sedimentation varying between positive (net), zero, and negative (erosion) -- 9 Subsidence -- 10 Synsedimentary tectonics -- 11 Discussion and conclusions -- 12 Main conclusions -- References.
ISBN: 9783034801362 (electronic bk.)Subjects--Topical Terms:
882546
Sedimentation and deposition
--Jura Mountains (France and Switzerland)
LC Class. No.: QE684 / .G94 2012
Dewey Class. No.: 551.766
Quantitative geology of late Jurassic epicontinental sediments in the Jura Mountains of Switzerland
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by Reinhart A. Gygi.
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2012.
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213 p. :
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ill., digital ;
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1 Previous Work -- 2 What can be measured, calculated, or be quantified by comparison -- 3 Paleogeography and paleoclimate -- 4 Sedimentation -- 5 Sea level variations -- 6 Hermatypic coral assemblages: growth form, spatial distribution, and paleobathymetry -- 7 Age and time correlation of sediments -- 8 Rates of sedimentation varying between positive (net), zero, and negative (erosion) -- 9 Subsidence -- 10 Synsedimentary tectonics -- 11 Discussion and conclusions -- 12 Main conclusions -- References.
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Earth and Environmental Science (Springer-11646)
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