The experimental replacement of calcite and aragonite by dolomite under a variety of
conditions indicates that dolomitization can take place in marine and lacustrine …

Systematic chemical variation exists in formation water collected from a dip section through
Lower Cretaceous rocks of south-central Texas. Chemical variation can be explained by an …

The results of experiments on the hydrothermal dolomitization of calcite (between 252 and
295° C) and aragonite (at 252° C) by a 2 M CaCl 2-MgCl 2 aqueous solution are reported …

Quartz filled veins and fractures which formed late in the Alpine thrusting of the Central
Pyrenees contain inclusions of hypersaline Na-Ca-Cl brines with total dissolved salts of up …

Carbon and carbon dioxide always played an important role in the geobiosphere that is part
of the Earth's outer shell and surface environment. The book's eleven chapters cover the …

The recrystallization of dolomite was investigated experimentally from 50° to 200° C for
durations up to approximately one year. A synthetic, mixed Ca Mg carbonate (41.7 mol …

Two parameters have been added to the Extended UNIQUAC model of Thomsen and
Rasmussen [Thomsen, K., Rasmussen, P., 1999. Modeling of vapor–liquid–solid equilibrium …

Sedimentary minerals are generally metastable phases that, given time and changing
environmental conditions, recrystallize to more stable phases. The actual pathway of …

Natural and synthetic dolomites exhibit large scatter of structural and compositional
characteristics with respect to variations in their stoichiometry and cation ordering degree …

The 'dolomite problem'has a long history and remains one of the most intensely studied and
debated topics in geology. Major amounts of dolomite are not directly forming today from …