The Great Proterozoic Fold Belt of India (GIPFOB) is the inferred accretion zone between the North India Block (NIB) and the South India Block (SIB). Mesoscopic structures, phase petrology, and U-Th-Pb (total) monazite ages in the Bangriposi Shear Zone (BSZ) located in the eastern syntaxis of the GIPFOB along the fringe of the Paleo/Mesoarchean Singhbhum Craton (SC) are examined to constrain the time of NIB-SIB assembly. The BSZ at the eastern fringe of the Archean Singhbhum Craton is a NNE-trending west-vergent 0.95-1.0 Ga greenschist-facies (<0.6 GPa at 500-30 degrees C) sinistral-reverse shear zone. The BSZ is dominated by Meso/Neoarchean (2.6-3.1 Ga) cratonic lithologies and an overlying suite of intensely to weakly deformed cobble/gran...
The amphibolite facies Moyar, Bhavani and Palghat shear zones separate the South Indian Dharwar Crat...
AbstractSubstantial part of the northern margin of Indian plate is subducted beneath the Eurasian pl...
The timing and extent of polymetamorphism in the Mangalwar and Sandmata Complexes from the Aravalli-...
The Great Proterozoic Fold Belt of India (GIPFOB) is the inferred accretion zone between the North I...
The Aravalli–Delhi and Satpura Mobile Belts (ADMB and SMB) and the Eastern Ghat Mobile Belt (EGMB) i...
The Archean cratonic nuclei in India are hemmed by Proterozoic mobile belts or fold belts. These mob...
AbstractThe Aravalli–Delhi and Satpura Mobile Belts (ADMB and SMB) and the Eastern Ghat Mobile Belt ...
The supracrustal rocks in the easternmost part of the Proterozoic fold belt of North Singhbhum, east...
The Singhbhum craton of eastern India preserves an extensive record of basin formation spanning the ...
The Himalayan orogen has experienced intense Cenozoic deformation and widespread metamorphism, makin...
© 2019 Elsevier B.V. The Singhbhum Craton and supracrustal provinces in eastern India are one of a f...
The Meghalaya Gneissic Complex (MGC) of northeast India is a little-studied high-grade metamorphic t...
International audienceThe Godhra-Chhota Udepur (GC) sector (west-central India) is the zone of conve...
This item is only available electronically.The central Eastern Ghats Province is part of a series of...
The Singhbhum Craton in eastern India preserves a depositional record from the Palaeo-Mesoarchaean t...
The amphibolite facies Moyar, Bhavani and Palghat shear zones separate the South Indian Dharwar Crat...
AbstractSubstantial part of the northern margin of Indian plate is subducted beneath the Eurasian pl...
The timing and extent of polymetamorphism in the Mangalwar and Sandmata Complexes from the Aravalli-...
The Great Proterozoic Fold Belt of India (GIPFOB) is the inferred accretion zone between the North I...
The Aravalli–Delhi and Satpura Mobile Belts (ADMB and SMB) and the Eastern Ghat Mobile Belt (EGMB) i...
The Archean cratonic nuclei in India are hemmed by Proterozoic mobile belts or fold belts. These mob...
AbstractThe Aravalli–Delhi and Satpura Mobile Belts (ADMB and SMB) and the Eastern Ghat Mobile Belt ...
The supracrustal rocks in the easternmost part of the Proterozoic fold belt of North Singhbhum, east...
The Singhbhum craton of eastern India preserves an extensive record of basin formation spanning the ...
The Himalayan orogen has experienced intense Cenozoic deformation and widespread metamorphism, makin...
© 2019 Elsevier B.V. The Singhbhum Craton and supracrustal provinces in eastern India are one of a f...
The Meghalaya Gneissic Complex (MGC) of northeast India is a little-studied high-grade metamorphic t...
International audienceThe Godhra-Chhota Udepur (GC) sector (west-central India) is the zone of conve...
This item is only available electronically.The central Eastern Ghats Province is part of a series of...
The Singhbhum Craton in eastern India preserves a depositional record from the Palaeo-Mesoarchaean t...
The amphibolite facies Moyar, Bhavani and Palghat shear zones separate the South Indian Dharwar Crat...
AbstractSubstantial part of the northern margin of Indian plate is subducted beneath the Eurasian pl...
The timing and extent of polymetamorphism in the Mangalwar and Sandmata Complexes from the Aravalli-...