Dolomitization by hypersaline reflux into dense groundwaters as revealed by vertical trends in strontium and oxygen isotopes: Upper Muschelkalk, Switzerland-Reference-Cited by-同舟云学术

Dolomitization by hypersaline reflux into dense groundwaters as revealed by vertical trends in strontium and oxygen isotopes: Upper Muschelkalk, Switzerland

Published:2018-10-08 Issue:1 Volume:66 Page:362-390
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Adams Arthur¹^ORCID,Diamond Larryn W.¹,Aschwanden Lukas¹

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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