Low-pressure decomposition of chrysotile as a function of time and temperature

American Mineralogist

Volumn 92, Issue 10, 2007, Pages 1704-1713

  Candela, P A ^a   Crummett, C D ^a   Earnest, D J ^a   Frank, M R ^b   Wylie, A G ^a  

^a UNIVERSITY OF MARYLAND   (United States)

^b NORTHERN ILLINOIS UNIVERSITY   (United States)

Author keywords

Asbestos; Brake wear debris; Chrysotile; Reaction products; Thermal stability

Indexed keywords

ASBESTOS; BRAKES; DEBRIS; GRAIN SIZE AND SHAPE; HEATING; OLIVINE; PARTICLE SIZE; REACTION INTERMEDIATES; REACTION PRODUCTS; REFRACTION; REFRACTIVE INDEX; SILICA; SYNCHROTRON RADIATION; TALC; THERMODYNAMIC STABILITY; WEAR OF MATERIALS; X RAY DIFFRACTION;

CHRYSOTILE; CONSTANT TEMPERATURE; DECOMPOSITION PRODUCTS; DECOMPOSITION TEMPERATURE; DIFFERENT PARTICLE SIZES; HYDROTHERMAL DIAMOND ANVIL CELL; INTERMEDIATE REACTIONS; WEAR DEBRIS;

SERPENTINE;

ASBESTOS; DECOMPOSITION; DIAMOND ANVIL CELL; EXPERIMENTAL MINERALOGY; LOW PRESSURE; MICROSCOPY; PARTIAL PRESSURE; PARTICLE SIZE; RECRYSTALLIZATION; X-RAY DIFFRACTION;

CALIFORNIA; CANADA; NORTH AMERICA; QUEBEC [CANADA]; UNITED STATES;

EID: 35448976924     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2007.2559     Document Type: Article

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