Structure and SHRIMP U/Pb zircon ages of granites adjacent to the Chitradurga Schist Belt: Implications for Neoarchaean convergence in the Dharwar Craton, Southern India
Neoarchaean granites adjacent to the Chitradurga schist belt were emplaced in the inner margin of the foreland in the context of the Neoarchaean oblique convergent setting of the Dharwar craton. Two previously unreported granites, one 50 km and the other
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|Source:||Journal Geological Society of India|
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