A STUDY ON THE Nd-Sr ISOTOPE OF THE WUGONGSHAN MIGMATITE

1991中国科学通报：英文版Earth and Planetary Sciences被引 1

摘要

Ⅰ. GEOLOGICAL BACKGROUND Covering an area of 1200 km~2, the Wugongshan migmatite-granite batholith is located on the northwestern margin of South China Caledonian folded region and the southern flank of Pingxiang-Guangfeng deep fault. It is characterized by the trinity of meta-sediments,

引用本文（GB/T 7714）

徐士进, 沈渭洲, 王银喜, 等. A STUDY ON THE Nd-Sr ISOTOPE OF THE WUGONGSHAN MIGMATITE[J]. 中国科学通报：英文版, 1991.

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