Geochemical evidence for the production of granitoids through reworking of the juvenile mafic arc crust in the Gangdese orogen, southern TibetMarkYu-Wei TangLong ChenZi-Fu Zhao (赵子福)[0]Yong-Fei Zheng (郑永飞)[0]2019.Cited by: 0|Bibtex|Views105|Code: Data: Full Text (Upload PDF)PPT (Upload PPT)Upload PDFUpload PPTYour rating :0 TagsCommentsSubmit