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

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,

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Veröffentlicht in:中国科学通报:英文版 1991 (24), p.2069-2072
1. Verfasser: 徐士进 沈渭洲 王银喜 杨杰东 李惠民
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Sprache:eng
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Zusammenfassung: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,
ISSN:2095-9273