Sea-water circulation on an oolite-dominated carbonate system in an epeiric sea (Middle Jurassic, Switzerland)
Author:
Affiliation:
1. Geologisch-Paläontologisches Institut; Universität Basel; Bernoullistrasse 32; CH-4056; Basel; Switzerland
2. Geologisches Institut; ETH-Zentrum; CH-8092; Zürich; Switzerland
Publisher
Wiley
Subject
Stratigraphy,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/sed.12007/fullpdf
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4. Spatial patterns of Mesozoic facies relationships and the age of the Rhenish Lineament: a compilation;Allenbach;Int. J. Earth Sci.,2006
5. Circulation in large ancient epicontinental seas: what was different and why?;Allison;Palaios,2006
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