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Quantitative geology of late Jurassi...

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Quantitative geology of late Jurassic epicontinental sediments in the Jura Mountains of Switzerland

紀錄類型:	書目-語言資料,印刷品 : Monograph/item
正題名/作者:	Quantitative geology of late Jurassic epicontinental sediments in the Jura Mountains of Switzerland/ by Reinhart A. Gygi.
作者:	Gygi, Reinhart A.
出版者:	Basel :Springer Basel : : 2012.,
面頁冊數:	213 p. :ill., digital ; : 24 cm.;
Contained By:	Springer eBooks
標題:	Sedimentation and deposition - Jura Mountains (France and Switzerland) -
電子資源:	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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505 0 $a 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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