OH-bearing planar defects in olivine produced by the breakdown of Ti-rich humite minerals from Dabie Shan (China)

Contributions to Mineralogy and Petrology

Volumn 153, Issue 4, 2007, Pages 417-428

  Hermann, Jörg ^a   Fitz Gerald, John D ^a   Malaspina, Nadia ^b   Berry, Andrew J ^a,c   Scambelluri, Marco ^b  

^a AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

^b UNIVERSITY OF GENOA   (Italy)

^c IMPERIAL COLLEGE LONDON   (United Kingdom)

Author keywords

Infrared spectroscopy; OH in olivine; Ti chondrodite; Ti clinohumite; Transmission electron microscopy; UHP metamorphism

Indexed keywords

AMPHIBOLITE FACIES; CLINOHUMITE; DEFECT; EXHUMATION; FTIR SPECTROSCOPY; HUMITE; HYDROXIDE; INFRARED SPECTROSCOPY; OLIVINE; SUBDUCTION ZONE; TRANSMISSION ELECTRON MICROSCOPY; TRANSPORT PROCESS; ULTRAHIGH PRESSURE METAMORPHISM;

ASIA; CHINA; DABIE MOUNTAINS; EURASIA; FAR EAST;

EID: 33847670053     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-006-0155-7     Document Type: Article

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