Os isotopic evidence for a carbonaceous chondritic mantle source for the Nagqu ophiolite from Tibet and its implications

引用方式:

Huang, Q.S., Shi, R.D., Liu, D.L., Zhang, X.R., Fan, S.Q., &Ding, L. (2013). Os isotopic evidence for a carbonaceous chondritic mantle source for the Nagqu ophiolite from Tibet and its implications. Chinese science bulletin, 58(1), 92-98.