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 |
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Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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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, |
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ISSN: | 2095-9273 |