Sulfur and lead isotope tracing for sources of ore-forming material and ore-forming age of the Meixian-style Pb-Zn(-Ag) deposits in the central Fujian rift, south east China

Acta Geologica Sinica (English Edition)

Volumn 81, Issue 7, 2007, Pages 906-916

  Feng, Chengyou ^a   Feng, Yaodong ^b   Zhang, Dequan ^a   She, Hongquan ^a   Li, Daxin ^a   Li, Jinwen ^a   Dong, Yingjun ^a  

^a INSTITUTE OF MINERAL RESOURCES   (China)

^b No3 Institute of Geological and Mineral Resources Survey of Henan   (China)

Author keywords

Central Fujian rift; Meixian style deposit; Ore forming age; Sources of ore forming material; Sulfur and lead isotope

Indexed keywords

LEAD; LEAD ISOTOPE; MASSIVE SULFIDE; METALLOGENESIS; MINERALIZATION; ORE DEPOSIT; SULFUR ISOTOPE; ZINC;

ASIA; CHINA; EURASIA; FAR EAST; FUJIAN;

EID: 35948960661     PISSN: 10009515     EISSN: 17556724     Source Type: Journal    
DOI: None     Document Type: Article

References (29)

1. Chinese source.
2. Chinese source.
3. Chinese source.
4. Chinese source.
5. Chinese source.
6. Chinese source.
7. Chinese source.
8. Chinese source.
9. Chinese source.
10. Chinese source.
11. Chinese source.
12. Chinese source.
13. Chinese source.
14. Chinese source.
15. Chinese source.
16. Chinese source.
17. Chinese source.
18. Chinese source.
19. Chinese source.
20. Chinese source.
21. Chinese source.
22. Chinese source.
23. Chineses source.
24. Chinese source.
25. Chinese source.
26. Andrew W M,Pablo M, Anne P L. 1990. Lead isotope provinces of the Central Andes inferred from ores and crustal rocks. Econ. Geol., 85(8):1857-1880.
27. Franklin J M, Roscoe S M, Loveridge W D, Sangster D F. 1983. Lead isotope studies in superior and southern provinces. Geological Survey of Canada, Bulletin 351:1-35.
28. Ohmoto H. 1983. Stable isotope geochemistry of ore deposits. Rev Minerology, 16:491-560.
29. Solomon M, Eastoe C J, Walshe J L. 1988. Mineral deposits and sulfur isotope abundances in the Mount Read Volcanics between Que River and Mount Darwin, Tasmania. Econ. Geol. 83: 1307-1328.