Structurally controlled hydrothermal dolomite (HTD) reservoir facies and associated
productive leached limestones are major hydrocarbon producers in North America and are …

Dolomitization requires not only favourable thermodynamic and kinetic conditions, but also a
fluid-flow mechanism to transport reactants to and products from the site of dolomitization …

In the past decade, more than 20 new natural gas fields have been discovered in laterally
discontinuous dolomites of the Upper Ordovician Black River Group in south-central New …

Mississippi Valley-type (MVT) deposits are epigenetic, stratabound, carbonate-hosted
sulphide bodies composed predominantly of sphalerite, galena, iron oxides (pyrite …

Stable isotope compositions of methane (δ 13 C and δD) and of short-chain alkanes are
commonly used to trace the origin and fate of carbon in the continental crust. In continental …

Large-scale, massive burial dolomitization affected Upper Carboniferous carbonates of the
southwestern Variscan Cantabrian Zone (Spain). Replacive and void-filling dolomites …

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

The Upper Jurassic of the eastern Swabian Alb is composed of oolitic platform sands with
associated microbe-siliceous sponge mounds at the platform margins. They are surrounded …

Ordovician carbonates near the Wisconsin arch represent the type locality in ancient rocks
for the Dorag, or mixing-zone, model for dolomitization. Field, petrographic, and …

The" topographic recharge" and" tectonic compaction" models for subsurface fluid flow may
have been over-applied to the question of the origin of regional hydrothermal dolomite …