Over the past century a number of models have been developed to explain the vast
stratigraphic distribution of authigenic dolomite. These models include hydrogeological …

Dolomite can form as a major mineral component of marlstones and limestones and is an
important sink for magnesium in the marine environment. Dolomite is widely distributed in …

Stable carbon and oxygen isotopes (δ18O and δ13C values) and trace elements have been
applied to the study of diagenesis of carbonate rocks for over 50 years. As valuable as these …

针对白云岩成因, 原生白云石沉淀, 白云岩孔隙成因等问题, 在前人认识的基础上,
补充四川和塔里木盆地典型案例的岩石学和地球化学特征分析工作, 取得3 项进展: ① …

Some species of sulphate‐reducing bacteria (SRB) are known to mediate the formation of
dolomite and Mg‐calcite. However, their exact role in the mineralization process remains …

The origin of sedimentary dolomite is a subject of long-standing enigma that still awaits
resolution. Previous studies have shown that room temperature synthesis of abiotic dolomite …

A series of laboratory-controlled microbial experiments using gram-negative sulphate-
reducing bacteria (Desulfovibrio brasiliensis) inoculated with natural uranium were …

Although most modern dolomites occur in hypersaline environments, the effects of elevated
salinity on the microbial mediation of dolomite precipitation have not been fully evaluated …

Lacustrine microbialites record evidence of their depositional environments in their
morphology, mineralogy and geochemistry. This synthesis reviews geochemical data both …

To find out the origin of dolomite, the precipitation of primary dolomite, and the formation of
pores in dolomite, petrologic and geochemical characteristics of typical samples from …