Multi-phase dolomitization and recrystallization of Middle Triassic shallow marine–peritidal carbonates from the Mecsek Mts. (SW Hungary), as inferred from petrography, carbon, oxygen, strontium and clumped isotope data

Author:

Lukoczki GeorginaORCID,Haas János,Gregg Jay M.,Machel Hans G.,Kele Sándor,John Cédric M.ORCID

Funder

American Association of Petroleum Geologists

Geological Society of America

International Association of Sedimentologists

Hungarian Scientific Research Fund

National Research, Development and Innovation Office

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference109 articles.

1. Dolomitization by hypersaline reflux into dense groundwaters as revealed by vertical trends in strontium and oxygen isotopes: upper Muschelkalk, Switzerland;Adams;Sedimentology,2018

2. Dolomitization by seepage refluxion;Adams;AAPG Bull.,1960

3. Stabilization of early–formed dolomite: a tale of divergence from two Mississippian dolomites;Al-Aasm;Sediment. Geol.,2000

4. Application of the trace element and isotope geochemistry of strontium to studies of carbonate diagenesis;Banner;Sedimentology,1995

5. Water-rock Interaction History of Regionally Extensive Dolomites of the Burlington-Keokuk Formation (Mississippian): Isotopic Evidence;Banner,1988

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