Implications of S and Pb isotopic compositions of the Gangdise porphyry copper belt for the ore-forming material source and material recycling within the orogenic belt

QU Xiaoming; HOU Zengqian; LI Youguo

doi:10.12097/gbc.2002011172

Geological Bulletin of China > 2002 > 21(11): 768-776. > DOI: 10.12097/gbc.2002011172

QU Xiaoming, HOU Zengqian, LI Youguo. 2002: Implications of S and Pb isotopic compositions of the Gangdise porphyry copper belt for the ore-forming material source and material recycling within the orogenic belt. Geological Bulletin of China, 21(11): 768-776. DOI: 10.12097/gbc.2002011172

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Implications of S and Pb isotopic compositions of the Gangdise porphyry copper belt for the ore-forming material source and material recycling within the orogenic belt

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Revised Date: April 17, 2002

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Abstract

- Tibetan Plateau,
- Gangdise magma arc,
- porphyry-type copper belt,
- S-Pb isotopic tracing

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Implications of S and Pb isotopic compositions of the Gangdise porphyry copper belt for the ore-forming material source and material recycling within the orogenic belt

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Implications of S and Pb isotopic compositions of the Gangdise porphyry copper belt for the ore-forming material source and material recycling within the orogenic belt

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