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• W2058658546 abstract "Origin of charnockites granulites is one of the most fashionable and important problems in Earth s sciences It has a key signi cance for understanding the na ture of the lower continental crust and creates one of the most active elds of present day research Really the deep continental crust all over the world includes within it a close association of charnockitic granulites and metasediments of Archean Proterozoic age As a result of extensive uplift and erosion parts of the for mer deep crust are exposed now in some places on old cratons such as granulite terranes of Canadian Baltic and Guyana shields But only in the southern India and nowhere else a continuous cross section through the middle to the lower crust is available for studying the processes operating over the full thickness of the conti nental crust The practical importance of this problem is determined by the fact of close association of gold mineralization with uid transport during formation of charnockites and really many gold rich bearings are found in charnockitic terranes Although there is a long history of studies and a large number of publication on this subject including several outstanding monographs and reviews the problem of origin of charnockitic rocks is still far from the solution and di erent points of view on their origin are discussed by petrologists In our opinion the verifying of these hypotheses based on the petrological and geochemical data could be done only by studying of physical aspects of charnockites forma tion modelling of the thermal processes in the crust and mechanisms of uid heat and mass transfer during the charnockitization Here we make a rst step in such a testing based on the best and most comprehensive set" @default.
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• W2058658546 date "1999-08-20" @default.
• W2058658546 modified "2023-10-14" @default.
• W2058658546 title "Physical approach to the problem of origin of charnockitic rocks of southern India: Mechanisms of crustal heating and transfer of carbon dioxide" @default.
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• W2058658546 doi "https://doi.org/10.2205/1999es000019" @default.
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