Over the past decades, the burial realm, the most prolonged and arguably the least well‐
understood diagenetic environment, has received significant research attention. Despite …

Orogenic forelands host interactions between deformation and static or migrating fluids.
Given their accessibility and dimensions, these areas are not only historic landmarks for …

Geologic carbon sequestration (GCS) is a promising strategy to reduce the harm of CO 2
due to the rapidly increased fossil fuel combustion. Dolomitization and dissolution processes …

Various geochemical proxies are used to constrain the diagenetic origin and evolution of
ancient dolomites. Dolomite stoichiometry (mole% MgCO3) and cation ordering, two …

Abstract The Ediacaran Period (ca. 635–541 Ma) witnessed the earliest paleontological
evidence for macroscopic animals (ie, Ediacara biota) and geochemical observations of the …

Fault-controlled, hydrothermal dolomitization often occurs at margins between shallow-water
carbonate platforms and deep-water sedimentary basins. In western Canada, for example …

The formation mechanisms of multi-stage dolomites and hydrocarbon reservoirs associated
with volcanic activity are complex. This study investigated the Permian Chihsia Formation in …

Carbonate rocks undergo low-temperature, post-depositional changes, including mineral
precipitation, dissolution, or recrystallisation (diagenesis). Unravelling the sequence of these …

During the analysis of the Δ 47 values of CO 2 derived from carbonates, the acid
fractionation factor not only allows Δ 47 values produced from carbonates and reacted at …

Thermal convection arises due to a density gradient between geothermally heated formation
water within the underlying strata and the water in the overlying strata. The thermal …