Abstract
P-T conditions of sapphirine bearing granulites from a new locality from the north eastern part of Gujarat range from 8.2–8.8 kbars at T of 950°C. The discovery of this UHT assemblage in the north western part of the Indian shield bordering the Aravalli-Delhi fold belt provides additional evidences for India-Madagascar connection, linking the Aravalli- Malani sequences to similar lithologies in northern Madagascar.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
