Oxygen isotope fractionation between calcite and fluid as a function of growth rate and temperature: An in situ study

Chemical Geology

Volumn 306-307, Issue , 2012, Pages 92-102

  Gabitov, Rinat I ^a   Watson, E Bruce ^b   Sadekov, Aleksey ^c,d  

^a UNIVERSITY OF CALIFORNIA   (United States)

^b RENSSELAER POLYTECHNIC INSTITUTE   (United States)

^c UNIVERSITY OF EDINBURGH   (United Kingdom)

^d UNIVERSITY OF CAMBRIDGE   (United Kingdom)

Author keywords

Calcite; Equilibrium; Growth rate; Oxygen isotopes; SIMS; Temperature

Indexed keywords

ANALYTICAL UNCERTAINTY; EQUILIBRIUM CONDITIONS; EQUILIBRIUM VALUE; EXPERIMENTAL FLUIDS; FRACTIONATION FACTORS; IN-SITU; IN-SITU STUDY; ISOTOPIC FRACTIONATIONS; NEAR SURFACE REGIONS; OXYGEN ISOTOPES; RARE EARTH ELEMENTS (REE); STABLE ISOTOPES;

CARBONATE MINERALS; CRYSTAL GROWTH; GROWTH RATE; ISOTOPES; OXYGEN; PHASE EQUILIBRIA; RARE EARTH ELEMENTS; SECONDARY ION MASS SPECTROMETRY; TEMPERATURE;

CALCITE;

CALCITE; CRYSTALLIZATION; ISOTOPIC FRACTIONATION; LATTICE DYNAMICS; MASS SPECTROMETRY; OXYGEN ISOTOPE; TEMPERATURE;

EID: 84859868586     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2012.02.021     Document Type: Article

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