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Panjal Trap chemistry and the birth of Tethys

Published online by Cambridge University Press:  01 May 2009

M. I. Bhat ,
Syed M. Zainuddin  and
A. Rais
M. I. Bhat
Affiliation:
Wadia Institute of Himalayan Geology, 15, Municipal Road, Dehra Dun – 248001, India
Syed M. Zainuddin
Affiliation:
Department of Geology, Aligarh Muslim University, Aligarh-202 001, India
A. Rais
Affiliation:
Department of Geology, Aligarh Muslim University, Aligarh-202 001, India
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Summary

K2O, TiO2, P205, Zr, Y, Sr and Nb data from the Panjal Traps of Kashmir indicate that the lava erupted in a rift tectonic setting. This is also suggested by the other features of these rocks and volcanic history of the area. The time of eruption represents the initial phase of break-up of the Indian plate from the Siberian plate. This conclusion is in good agreement with the current views on the tectonic evolution of the area.

Type
Articles
Information
Geological Magazine , Volume 118 , Issue 4 , July 1981 , pp. 367 - 375
Copyright
Copyright © Cambridge University Press 1981

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