Abstract Dolomite [CaMg (CO3) 2] forms in numerous geological settings, usually as a
diagenetic replacement of limestone, and is an important component of petroleum reservoir …

It is very difficult to synthesize dolomite under Earth-surface conditions in the laboratory.
However, multiple carbonate phases, including low-Mg-calcite (LMC), high-Mg-calcite …

Because of its rare occurrence in modern sediments, as well as the difficulty in synthesizing
it under low-temperature conditions in the laboratory, the origin of sedimentary dolomite has …

Abstract Dolomite, an ordered Ca-Mg-carbonate mineral, is abundant in the sedimentary
record but found only rarely found in Holocene and modern marine settings. Instead …

Abstract In the late Carnian (Late Triassic), a carbonate‐clastic depositional system
including a distal alluvial plain, flood basin and sabkha, tidal flat and shallow carbonate …

In previous dissolution studies, dolomite has been commonly assumed to have an ideal
composition of CaMg (CO 3) 2. The objectives of this work are to determine (1) if dolomites …

In contrast to the prevalence of dolomite [CaMg (CO3) 2] in the geological record, there are
few instances of recent formation. This discrepancy occurs despite supersaturation with …

The mechanism of sedimentary dolomite formation has puzzled the geology community for
more than a century. Within the past several years, successful synthesis of disordered …

The study focuses on the formation of lacustrine dolomite in late Miocene lakes, located at
the East Mediterranean margins (Northern Israel). These lakes deposited the sediments of …

Nano-precipitates with tripled periodicity along the c-axis are observed in a Ca-rich dolomite
sample from Proterozoic carbonate rocks with “molar tooth” structure. This observation is …