Sedimentary rock - Evaporites, Deposits, Minerals | Britannica
Evaporite - an overview | ScienceDirect Topics
The Dolomite Problem: A Matter of Time | ACS Earth and Space Chemistry
A) Stratigraphic column showing several carbonate-evaporite... | Download Scientific Diagram
Geotechnical Characteristics of Anhydrite/Gypsum Transformation in the Middle Miocene Evaporites, Red Sea Coast, Egypt – topic of research paper in Earth and related environmental sciences. Download scholarly article PDF and read for
Thermodynamic evidence of giant salt deposit formation by serpentinization: an alternative mechanism to solar evaporation | Scientific Reports
Dolomite (mineral) - Wikipedia
Sedimentary rock - Limestones, Dolomites, Calcite | Britannica
Dolomite (rock) - Wikipedia
Typical evaporites from the Lower-Middle Cambrian in the Tarim Basin.... | Download Scientific Diagram
Modern dolomite formation caused by seasonal cycling of oxygenic phototrophs and anoxygenic phototrophs in a hypersaline sabkha | Scientific Reports
Evaporites
Evaporite - an overview | ScienceDirect Topics
Massive dolomites in the Messinian evaporitic sequence (Sicily, Italy): multi-analytical characterization and implications for the dolomitization processes | SpringerLink
Dolomitization, gypsum calcitization and silicification in carbonate– evaporite shallow lacustrine deposits - Bustillo - 2017 - Sedimentology - Wiley Online Library
Visean, Carboniferous Evaporites in Leitrim, Ireland - by Ian West
Ordovician deep dolomite reservoirs in the intracratonic Ordos Basin, China: Depositional model and Diagenetic evolution - Anqing Chen, Shenglin Xu, Shuai Yang, Hongde Chen, Zhongtang Su, Yijiang Zhong, Sihan Hu, 2018
Structure, genesis and resources efficiency of dolomite: New insights and remaining enigmas - ScienceDirect
KGS--Geological Log Analysis--Evaporites
Dolomite (Mineral) - an overview | ScienceDirect Topics
Evaporite-dolomite Member of the Luka~ section is composed of well... | Download Scientific Diagram
Burial-stage dolomite; Porosity at depth?
