Why most 'dry' rocks should cool 'wet'

American Mineralogist

Volumn 84, Issue 4, 1999, Pages 570-580

  Kohn, Matthew J ^a,b  

^a LAWRENCE LIVERMORE NATIONAL LABORATORY   (United States)

^b UNIVERSITY OF SOUTH CAROLINA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

COOLING; ISOTOPES; ROCKS;

CLOSURE TEMPERATURES; DIFFUSION EXPERIMENTS; DIFFUSION MODEL; DIFFUSION RATE; FRACTIONATION FACTORS; HYDROUS FLUIDS; MINERAL ASSEMBLAGE; OXYGEN ISOTOPES;

DIFFUSION;

COOLING; METAMORPHIC ROCK; MINERAL ALTERATION; OXYGEN ISOTOPE;

EID: 0032822653     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am-1999-0411     Document Type: Article

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