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Geothermobarometry of mafic granulites and metapelite from the Palghat Gap, South India: petrological evidence for isothermal uplift and rapid cooling
Author(s) -
KUMAR C. R. RAVINDRA,
CHACKO T.
Publication year - 1994
Publication title -
journal of metamorphic geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.639
H-Index - 114
eISSN - 1525-1314
pISSN - 0263-4929
DOI - 10.1111/j.1525-1314.1994.tb00037.x
Subject(s) - granulite , mafic , geology , geochemistry , charnockite , geothermobarometry , plagioclase , terrane , gneiss , petrology , massif , hornblende , anorthosite , metamorphism , biotite , metamorphic rock , geomorphology , facies , seismology , tectonics , paleontology , quartz , structural basin
The Palghat Gap region is located near the centre of the large southern Indian granulite terrane. at the northern edge of the Kodaikanal charnockite massif. The dominant rock types in the region are hornblende‐biotite ± orthopyroxene gneisses and charnockites along with minor amounts of intercalated mafic granulite, metapelite and calc‐silicate. The P‐T estimates from garnetiferous mafic granulites and metapelite samples are generally in the range 9‐10 kbar and 800‐900d̀ C using both conventional thermobarometric methods and the TWEEQU thermobarometry program. These P‐T estimates, which should be taken as minimum values, are among the highest yet reported for South Indian and Sri Lankan granulites. The occurrence of orthopyroxene + plagioclase symplectites around embayed garnet grains in the mafic granulites and cordierite rims around garnet grains in metapelite suggest an isothermal decompression‐type path. Similarly, a core‐rim P‐T trajectory indicates c. 3 and 7 kbar decompression at high temperature in the mafic granulites and metapelite, respectively. In both rock types, the key to the determination of the retrograde P‐T path was the recognition of small amounts of second generation plagioclase with a more anorthitic composition than the matrix plagioclase. The preservation of high garnet‐pyroxene temperatures in the mafic granulites (despite small garnet grain size) suggests rapid cooling of the terrane. Calculated minimum cooling rates range from 8 to 80d̀ C Ma ‐1 . Such cooling rates are more rapid than those associated with normal isostatic processes and suggest that the terrane was tectonically exhumed at high temperature.