Dolomitization by hypersaline reflux into dense groundwaters as revealed by vertical trends in strontium and oxygen isotopes: Upper Muschelkalk, Switzerland
Author:
Affiliation:
1. Institute of Geological Sciences; University of Bern; Baltzerstrasse 1+3 3012 Bern Switzerland
Funder
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung
Publisher
Wiley
Subject
Stratigraphy,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/sed.12530/fullpdf
Reference101 articles.
1. Early diagenesis driven by widespread meteoric infiltration of a Central European carbonate ramp: a reinterpretation of the Upper Muschelkalk;Adams;Sed. Geol.,2017
2. Aigner , T. 1982 Calcareous tempestites: storm dominated stratification in Upper Muschelkalk Limestones (Middle Trias, SW Germany). In: Cyclic and Event Stratification G. Einsele A. Seilacher 180 198 Springer-Verlag Berlin
3. Sequence-stratigraphic framework of the German Triassic;Aigner;Sed. Geol.,1992
4. Der Trigonodus-Dolomit im Oberen Muschelkalk von SW-Deutschland;Alesi;Arbeiten Inst. Geol. Paläontol. Univ. Stuttgart,1984
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