In situ X-ray diffraction of aragonite and dolomite at high pressure and high temperature: Evidence for dolomite breakdown to aragonite and magnesite

American Mineralogist

Volumn 81, Issue 5-6, 1996, Pages 611-624

  Martinez, Isabelle ^a,b   Zhang, Jianzhong ^a   Reeder, Richard J ^a  

^a STONY BROOK UNIVERSITY   (United States)

^b UNIVERSITÉ DE LYON   (France)

Author keywords

[No Author keywords available]

Indexed keywords

CALCITE; CALCIUM CARBONATE; MAGNESITE; SYNCHROTRON RADIATION; TEMPERATURE; X RAY DIFFRACTION; X RAY POWDER DIFFRACTION;

DECOMPOSITION REACTION; ENERGY DISPERSIVE X-RAY; HIGH PRESSURE AND HIGH TEMPERATURE; IN-SITU X-RAY DIFFRACTION; MULTI-ANVIL APPARATUS; THERMAL EXPANSIVITY; THERMODYNAMIC DATA; ULTRA-HIGH PRESSURE METAMORPHISMS;

EQUATIONS OF STATE;

ARAGONITE; DOLOMITE; MAGNESITE; P/T CONDITIONS; THERMODYNAMICS; XRD;

EID: 0030454752     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am-1996-5-608     Document Type: Article

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