High-pressure experiments and the varying depths of rock metamorphism

Geological Society Special Publication

Volumn 150, Issue , 1999, Pages 59-74

  Schreyer, Werner ^a  

^a RUHR UNIVERSITY BOCHUM   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

HISTORY OF GEOLOGY; METAMORPHISM; P-T CONDITIONS;

EID: 0032804923     PISSN: 03058719     EISSN: None     Source Type: Book Series    
DOI: 10.1144/GSL.SP.1999.150.01.04     Document Type: Article

References (13)

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3. 5 polymorphs. Reviews in Mineralogy, 22.
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5. 2 component on the low quartz-coesite transition. Journal of Geophysical Research, 85, 6983-6990.
6. SCHREYER, W. 1986. The mineral cordierite: structure and reactions in the presence of fluid phases. Berichte der Bunsen-Gesellschaft für physikalische Chemie, 90, 748-755.
7. _ 1988. Subduction of continental crust to mantle depths: petrologic evidence. Episodes, 11, 97-104.
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10. THEYE, T., CHOPIN, C., GREVEL, K.-D. & OCKENGA, E. 1997. The assemblage diaspore + quartz in metamorphic rocks: a petrological, experimental and thermodynamic study. Journal of Metamorphic Geology, 15, 17-28.
11. 2O. Geological Society of America Memoir, 74.
12. WAIN, A. 1997. New evidence for coesite in eclogite and gneisses: defining a ultrahigh-pressure province in the Western Gneiss region of Norway. Geology, 25, 927-930.
13. WYLLIE, P. J. 1999. Hot little crucibles are pressured to reveal and calibrate igneous processes. This volume.