Genesis and significance of component zones in pyrites from Penglai gold deposit, Shandong Province

Scientia Geologica Sinica

Volumn 35, Issue 2, 2000, Pages 168-174

  Yang, Jinhui ^a   Ma, Hongmei ^b   Zhou, Xinhua ^a   Feng, Benzhi ^c  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b Beijing Elec Eng Group Corporation   (China)

^c CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY   (China)

Author keywords

Component zones; Dissipative structure; Gold mineralization; Penglai gold deposit; Pyrite; Shandong Province

Indexed keywords

GOLD; METALLOGENESIS; ORE DEPOSIT; PYRITE;

CHINA;

EID: 0033934828     PISSN: 05635020     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (18)

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. Arehart G B, Chryssoulis S L and Kesler S E. 1993. Gold and arsenic in iron sulfides from sediment-hosted disseminated gold deposits: implications for depositional processes. Economic Geology, 88(1) : 171-185.
14. Crank J. 1975. The Mathematics of Diffusion (2nd ed. ). Oxford: Clarendon Press, 1-414.
15. Cygan R T and Lasaga A G. 1982. Crystal growth and formation of chemical zoning in garnets. Contrib. Miner. Petrol. , 79:187-200.
16. Chinese source
17. Spear F S and Selverstone J. 1983. Quantitative P-T paths from zoned minerals: Theory and tectonic application. Contrib. Mineral. Petrol. , 83:348-357.
18. Yang J H, Zhou X H, Feng B Z and Zhou Y W. 1999. Petrology and geochemistry of dike rocks in Penglai County, Shandong Province: Constrains on Au metallogenic dynamics. Scientia Geologica Sinica, 8(4): 391-398.