Most carbonates deposited in continental environments are subjected to the effects of
meteoric diagenesis. This process includes all postdepositional changes that occur under …

Dedolomitization converts a dolomite into a calcite, and conventionally is interpreted to form
in an eogenetic or telogenetic diagenetic environment where meteoric water dissolves …

This study is based on petrographic examination (optical, scanning electron microscope,
cathodo-luminescence, backscattered electron imaging, and fluorescence) of 1,350 thin …

Early diagenetic dolomitization is a common feature in cyclic shallow-water carbonates
throughout the geologic record. After their generation, dolomites may be subject to …

CM chondrites are primitive solar‐system materials that have undergone high degrees of
aqueous alteration, resulting in the formation of secondary minerals including carbonates …

Karst processes may be critical for develo** secondary porosity and permeability within
carbonate reservoirs and aquifers. Karstification can significantly influence reservoir storage …

There is ongoing debate on whether stylolites act as barriers, conduits, or play no role in
fluid transport. This problem can be tackled by examining the spatial and temporal …

Carbonate rocks contain prolific hydrocarbon reserves all over the world, particularly in the
Middle East. For exploration and production strategies, it is essential to understand …

Santonian–Paleocene marls and fine grained carbonates have been sampled in Hasbayya
locality, south Lebanon, in order to evaluate their organic matter (OM) content, petroleum …

Shallow marine to peritidal carbonates of the Triassic Csukma Formation in the Mecsek Mts.
of SW Hungary are made up of dolomites, limestones and dolomitic limestones that show …