Skip to Main Content
Skip Nav Destination

The Shrinagar–Ajmer section of the South Delhi Fold Belt exposes a package of medium-grade metasedimentary rocks intruded by synkinematic granite, and the entire package was thrust on top of the basement gneisses occurring further east. The metamorphic history is best developed in the staurolite schist that shows an overall increase in modal abundance of staurolite towards the east. Textural analyses, garnet zoning profiles, thermobarometric data and phase equilibria analyses show an increase in metamorphic pressure and temperature, reaching peak conditions of 592 ± 12°C and 7.7 ± 0.11 kbar. In situ monazite dating of a staurolite schist sample yields...

You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Figures & Tables





Citing Books via

Close Modal

or Create an Account

Close Modal
Close Modal