Gold mineralisation in the Archaean Hutti, Mangalur and Gadag greenstone belts of the northern Dharwar craton is characterised by hydrothermal wall-rock alterations with ubiquitous presence of chlorite, sericite/muscovite, biotite, carbonates, sulphides and quartz veins indicating greenschist facies mineral assemblages. Such wall-rock alterations associated with gold mineralisation in these belts post-date the peak of regional metamorphism and are retrograde with respect to regional metamorphism. There is a salient relationship between gold mineralisation and retrograde greenschist facies metamorphism in these belts.
机构:
Indian Inst Technol, Dept Geol & Geophys, Kharagpur 721302, W Bengal, IndiaIndian Inst Technol, Dept Geol & Geophys, Kharagpur 721302, W Bengal, India
Mishra, Biswajit
Pal, Nabarun
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Reliance Ind Ltd, Petr Business E & P, Bombay 400701, Maharashtra, IndiaIndian Inst Technol, Dept Geol & Geophys, Kharagpur 721302, W Bengal, India