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Age Data on Pegmatites Of South Kerala and their Tectonic Significance


Affiliations
1 Department of Geology, Friendship University, Moscow, Russian Federation
2 Centre for Earth Science Studies, Trivandrum 695010, India
3 IGEM, Academy of Sciences, Moscow, USSR, Russian Federation
     

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K/Ar mica age of chrysoberyl-bearing pegmatites from four localities of Trivandrum district, Kerala ranges from 445 to 474 m.y., with a mean around 460 m.y. There is a close agreement between the ages of the concordant and cross-cutting pegmatites, between muscovite and biotite ages, as also between various size fractions. Chrysoberyl occurs within feldspars in association with quartz and muscovite. Since the formation of chrysoberyl-quartz association requires a higher pressure or temperature, the reported age would indicate the time of emplacement of the chrysoberyl-bearing pegmatites at the closing phase of a major tectonomagmatic event. It is interesting to note that these pegmatites of south-western India are younger compared to those of other localities viz., Rajasthan, Bihar. Nellore and Mysore.
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  • Age Data on Pegmatites Of South Kerala and their Tectonic Significance

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Authors

K. Soman
Department of Geology, Friendship University, Moscow, Russian Federation
N. G. K. Nair
Centre for Earth Science Studies, Trivandrum 695010, India
V. N. Golubyev
IGEM, Academy of Sciences, Moscow, USSR, Russian Federation
M. M. Arakelyan
IGEM, Academy of Sciences, Moscow, USSR, Russian Federation

Abstract


K/Ar mica age of chrysoberyl-bearing pegmatites from four localities of Trivandrum district, Kerala ranges from 445 to 474 m.y., with a mean around 460 m.y. There is a close agreement between the ages of the concordant and cross-cutting pegmatites, between muscovite and biotite ages, as also between various size fractions. Chrysoberyl occurs within feldspars in association with quartz and muscovite. Since the formation of chrysoberyl-quartz association requires a higher pressure or temperature, the reported age would indicate the time of emplacement of the chrysoberyl-bearing pegmatites at the closing phase of a major tectonomagmatic event. It is interesting to note that these pegmatites of south-western India are younger compared to those of other localities viz., Rajasthan, Bihar. Nellore and Mysore.