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

The occurrence of fault-controlled hydrothermal dolomitization (HTD) is ubiquitous across
stratigraphic records and has been extensively studied due to its association with economic …

The interplay between dolomitizing fluids, tectonically-controlled saddle dolomite and calcite
cements in Lower-Cambrian to Furongian strata in the Tazhong Uplift, Tarim Basin were …

The establishment of extensive carbonate platforms characterized the Ediacaran period
during CaCO3 oversaturation events and the exceptional creation of accommodation space …

The formation of large igneous provinces (LIPs) seems to require a series of conditions
conducive to massive dolomitization; however, the specific mechanisms remain unclear …

Rare earth elements and yttrium (REE+ Y), with stable and predictable chemical
characteristics, serve as important proxies for diagenetic fluids, but the effect of …

Lithological heterogeneity can be an important factor in regulating the spatial distribution of
hydrothermal dolostone (HTD) geobodies. Understanding HTD genesis is crucial for …

This study presents, for the first time in the southern Apennines (Southern Italy), evidence of
fault-driven hydrothermal dolomitization during the late Triassic rifting of the western Adria …

Basin-scale dolomitization of carbonate sequences occurs over long time spans and results
from diagenesis, burial, and tectonically driven fluid fluxes. Depicting the different geological …

Dolomitization is a critical diagenetic alteration that impacts the formation of carbonate
hydrocarbon reservoirs. In the offshore Bohai Bay Basin, the Lower Paleozoic carbonate …