The southern boundary of the Singhbhum Craton witnessed multiple orogenies that juxtaposed thin slice of granulite suite of the Rengali Province against the low
We report here rare evidence for the early prograde PeT evolution of garnetesillimaniteegraphite gneiss (khondalite) from the central Highland Complex, Sri Lank
The Hala’alat Mountains are located at the transition between the West Junggar and the Junggar Basin.In this area,rocks are Carboniferous,with younger strata a