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

In structurally-controlled dolomitization systems, there is a general consensus that the
formation of dolostone-limestone transitions, termed here as “dolomitization fronts”, is …

Natural dolomites exhibit a wide range of compositional and structural characteristics with
respect to the amount and positions of calcium and magnesium cations within the crystal …

As a new engineering technique, enzyme induced calcite precipitation (EICP) has
demonstrated significant ecological benefits for bio-cementation and bioremediation, with …

Dolomite clumped isotope compositions are indispensable for determining the temperatures
and fluid sources of dolomitizing environments, but can be misleading if they have modified …

Interactions of CO 2-rich aqueous fluids with mantle peridotite have major implications for
geochemical budgets and microbial life in the shallow oceanic lithosphere through the …

Abstract The Meillon (Callovo-Oxfordian) and Mano (Tithonian) Formations are dolomitized
carbonate reservoirs that actively produce oil and gas (Aquitaine Basin, France). In this …

Replacement reactions commonly alter the multiscale pore structures of rocks during fluid-
rock interactions. Analysis of these processes in various model fluid-rock systems during …

In laboratory experiments, the precipitation of dolomite at ambient temperature is virtually
impossible due to strong solvation shells of magnesium ions in aqueous media and …

Experimental investigation of the fractionation behavior of Cu isotopes during the
replacement of pyrite by Cu-bearing sulfides (chalcopyrite, bornite, and chalcocite) was …