Increased Magmatic Water Content--The Key to Oligo-Miocene Porphyry Cu-Mo   Au Formation in the Eastern Gangdese Belt, Tibet 论文

2014Economic Geology引用 227
DOI
Geological and Geochemical AnalysisGeochemistry and Geologic Mappingearthquake and tectonic studies
Geochemistry and Geologic MappingGeological and Geochemical Analysisearthquake and tectonic studies
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Increased Magmatic Water Content--The Key to Oligo-Miocene Porphyry Cu-Mo   Au Formation in the Eastern Gangdese Belt, Tibet · 相关文章

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