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Metamorphic conditions in the Nilgiri Granulite Terrane and the adjacent Moyar and Bhavani Shear Zones: A reevaluationData were presented on pressure and temperature determinations from the Nilgiri Hills. About 70 samples were analyzed by probe and several calibrations of garnet-pyroxene thermometry and barometry applied. Most calibrations gave considerable scatter; however, a new calibration by Bhattacharya, Raith, Lal, and others, accounting for nonideality in both garnet and orthopyroxene, gave consistent results of 754 + or - 52 C and 9.2 + or - 0.7 kbar. On the regional scale, a pressure increase of 6.5 to 7 kbar in the SW to 11 kbar in the NE was related to block tilting. A continuous pressure gradient into the Moyar shear zone suggests that the zone is not a suture juxtaposing unrelated blocks.
Document ID
19890012868
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Raith, M.
(Bonn Univ. (Germany F.R.)., United States)
Hengst, C.
(Bonn Univ. (Germany F.R.)., United States)
Nagel, B.
(Bonn Univ. (Germany F.R.)., United States)
Bhattacharya, A.
(Indian Inst. of Tech. Kharagpur., United States)
Srikantappa, C.
(Mysore Univ.)
Date Acquired
September 5, 2013
Publication Date
January 1, 1988
Publication Information
Publication: Lunar and Planetary Inst., Workshop on the Deep Continental Crust of South India
Subject Category
Geophysics
Accession Number
89N22239
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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