Low δ18O magmas in the carboniferous intra-oceanic arc, central Tibet: Implications for felsic magma generation and oceanic arc accretion

引用方式:

Dan., W., Wang, Q., Li, X.H., Tang, G.J., Zhang C., Zhang, X.Z, & Wang, J. (2019). Low δ18O magmas in the Carboniferous intra-oceanic arc, central Tibet: Implications for felsic magma generation and oceanic arc accretion. Lithos 326-327, 28-38.