Olivine [100] normal to foliation: Lattice preferred orientation in prograde garnet peridotite formed at high H2O activity, cima di gagnone (Central Alps)

Contributions to Mineralogy and Petrology

Volumn 145, Issue 1, 2003, Pages 75-86

  Frese, Katrine ^a   Trommsdorff, Volkmar ^a   Kunze, Karsten ^b  

^a ETH ZURICH   (Switzerland)

^b GEOLOGICAL INSTITUTE   (Switzerland)

Author keywords

[No Author keywords available]

Indexed keywords

FOLIATION; GARNET; LATTICE DYNAMICS; METAMORPHISM; OLIVINE; PERIDOTITE; PETROGRAPHY; PREFERRED ORIENTATION;

ALPS; CIMA DI GAGNONE; SWITZERLAND;

EID: 0038417970     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-002-0434-x     Document Type: Article

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