The eastern part of the Yangtze craton (eastern China ) is marked by a number of medium to small size porphyry Cu-(Au-Mo) deposits. A detailed geochronological study and existing data suggest that these deposits were emplaced in the 144 - 136 Ma interval. They are spatially and temporally related to voluminous mafic and alkaline magmatic rocks ranging in composition from gabbros, syenites, A-type granites and their volcanic counterparts. This indicates that the porphyry Cu-(Au-Mo) deposits in the eastern Yangtze craton were generated in an intra-craton extensional tectonic setting, which is distinctly different from the compressive environment of oceanic or continental arcs of the Pacific Rim where numerous giant porphyry Cu deposits were formed._x000D_
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