5406084
9781402058905
The authors suggest an alternative model for the origin of granite in terms of in-situ meltingintracrustal convection that determines the process from partial melting of mid-upper crustal rocks to the formation of a convecting magma layer. This is conveyed through international geological, geochemical and geophysical studies.Chen, Guo-Neng is the author of 'Granite Genesis In-situ Melting and Crustal Evolution', published 2007 under ISBN 9781402058905 and ISBN 140205890X.
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