On the evolution of dolomite stoichiometry and cation order during high-temperature synthesis experiments: An alternative model for the geochemical evolution of natural dolomites

Sedimentary Geology

Volumn 240, Issue 1-2, 2011, Pages 30-40

  Kaczmarek, Stephen E ^a   Sibley, Duncan F ^a  

^a MICHIGAN STATE UNIVERSITY   (United States)

Author keywords

Cation order; Dolomite; Experimental dolomitization; Stoichiometry

Indexed keywords

CARBONATE ROCK; CATION ORDER; CHEMICAL EVOLUTION; CRYSTAL SURFACES; CRYSTAL TEXTURE; DOLOMITE; DOLOMITIZATION; EXPERIMENTAL CONDITIONS; EXPERIMENTAL DOLOMITIZATION; FASTER RATES; FIELD OBSERVATIONS; FLOW PATH; GEOCHEMICAL EVOLUTION; HIGH TEMPERATURE; HIGH-TEMPERATURE SYNTHESIS; INITIAL SOLUTION; INTERSTITIAL PORES; NEW MODEL; OVERALL REACTIONS; RATE OF REPLACEMENT; REACTION PROGRESS; REACTIVE TRANSPORT MODELS; SOLUTION CHEMISTRY; SPATIAL VARIATIONS; STOICHIOMETRIC COMPOSITIONS;

CALCITE; CALCIUM; CALCIUM CARBONATE; CARBONATE MINERALS; CHLORINE; EXPERIMENTS; MAGNESIUM; REACTION RATES; ROCKS; STOICHIOMETRY; SYNTHESIS (CHEMICAL);

POSITIVE IONS;

CARBONATE ROCK; CATION; CHEMICAL COMPOSITION; CHEMICAL REACTION; DOLOMITE; DOLOMITIZATION; GEOCHEMISTRY; REACTIVE TRANSPORT; SOLUTION; SPATIAL VARIATION; STOICHIOMETRY;

EID: 80052780447     PISSN: 00370738     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.sedgeo.2011.07.003     Document Type: Article

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