We propose a review to discuss the large number of studies dealing with the fluid history in
extensional and compressional sedimentary basins that evolved along the Iberian-Eurasian …

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

Cambrian dolostone reservoirs in the Tarim Basin, China, have significant potential for future
discoveries of petroleum, although exploration and production planning is hampered by …

Fault‐controlled hydrothermal dolomitization in tectonically complex basins can occur at any
depth and from different fluid compositions, including 'deep‐seated','crustal'or …

Dolomitization is one of the most significant diagenetic reactions in carbonate systems,
occurring where limestone (CaCO 3) is replaced by dolomite (CaMg (CO 3) 2) under a wide …

Abstract Ultra-deep (7300 m–8900 m) condensed and volatile oil reservoirs have been
discovered in the Ordovician reservoirs of the Shunbei oilfield, in the Tarim Basin. This study …

A revised chronostratigraphy of the Barremian-Early Albian sedimentary record of the
Maestrat Basin (E Iberian Peninsula) is provided based on a comprehensive synthesis of …

Foreland fold and thrust belts always represent a complex diagenetic history of carbonate
succession, particularly multiphase dolomitization, due to the multi-sourcing nature of fluids …

Dolomite reservoirs formed by dissolution are significant for hydrocarbon exploration, but
their origins are poorly understood because of their complexity. This study investigated the …

Early marine diagenetic dolomite is a rather thermodynamically‐stable carbonate phase and
has potential to act as an archive of marine porewater properties. However, the variety of …