Microfabric and cathodoluminescence characteristics of the dolomitized

Geochemical constrains on dolomitization pathways of the Upper

Minerals, Free Full-Text

Origin of a microbial-dominated carbonate reservoir in the Lower

Dolomitization of reservoir rocks in the Smackover Formation

Geochemical characteristics of the Ediacaran Dengying Formation in

Detailed diagenetic investigation and their impact on the

Effects of progressive dolomitization on reservoir evolution: A

SE - Diagenetic evolution of fault zones in Urgonian microporous

Geochemical characteristics of Upper Jurassic-Lower Cretaceous

PDF) Origin of fabric-selective dolomitization recognizable in the

Porosity enhancement potential through dolomitization of carbonate

Microscopic and cathodoluminescence characteristics of dolomite

Dolomitization by hypersaline reflux into dense groundwaters as

Diagenesis of meteoric water for the Dengying Formation. a The coating

Geochemical constrains on dolomitization pathways of the Upper