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Author(s): P.V.N. Rao, A.T. Rao

Email(s): Email ID Not Available

Address: Department of Geology, Nagarjuna University, Nagarjunanagar-522510, Guntur, A.P
Department of Geology, Andhara University, Waltair-530 003, A.P.

Published In:   Volume - 5,      Issue - 1,     Year - 1992


Cite this article:
Rao and Rao (1992). Radioelement distribution in Leptynites from Eastern Ghat Granulite Terrain. Journal of Ravishankar University (Part-B: Science), 5(1), pp.77-83



Journal of  Ravishankar University  Vol. 4-5  No. B (Science) 1991-92   pp.77-83  ISSN  0970 5910

Radioelement distribution in Leptynites from Eastern Ghat

Granulite Terrain

P.V.N.  Rao and A.T. Rao

Department of Geology, Nagarjuna University,  Nagarjunanagar-522510, Guntur, A.P.

*Department of Geology, Andhara University, Waltair-530 003, A.P.

Ms:  Received 16.6.92; Revised 26.11.92.

Abstract: Leptynites are important   rock type in the Visakhapa1nam   area and they are categorised into grey and cream varieties. At a glance it is noticed from the data that the radioelement concentrations in grey leptynites are lower while they are higher in the cream leptynites.   The concentrations    of U, Th,   K and  Th/U  ra1ios  of grey  leptynites  do not  represent   the  primary  distribution   but  indicate  their  expulsion   in a hydrous  partial melt  from  the  destabilised   mineral   sites/  dislocations   of k-feldspar,   biotite  and  other accessory   phases.   The expelled U, Th, K and other LIL elements during granulite facies metamorphism     were  carried   up  in  hydrous   granitic   partial  melts   along   weak  shear planes/zones and crystallized in surrounding cream leptynites. The enrichment of radioelements in the cream leptynites may be po5$ible by two reascne: 1. Crystallization of  radioelement    bearing   partial   melts in the  cream leptynites. 2. The radioelement already resided in the accessory   phases present in cream  leptynites.   The expulsion of U, Th and K from grey leptynites during granulite facies metamorphism is simultaneously followed by the crystalization of partial melts in the cream variety.  The higher rediogenic heat generatlon (2.17) values of leptynites   reveals that the Precambrian   crust  of the Eastern  Ghats  Granulite  Terrain  characterised   by high radioactivity.

Keywords: Leptynites, VisaKhapamacn, Radioelements, Metamorphism-partial melting, Radiogenic Reat Generation.

NOTE: Full version of this manuscript is available in PDF.



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