芬兰塔维瓦拉巨型黑色片岩型镍-铜-锌矿床地质特征及成因

Full-Text   Cite this paper   Add to My Lib

Abstract:

References

[1]	李胜荣,高振敏. 2000. 湘黔寒武系底部黑色岩系贵金属元素来源示踪[J]. 中国科学(D辑), 30(2): 169-174.
[2]	Eilu P. 2012. Mineral Deposits and Metallogeny of Fennoscandia[C]. Geological Survey of Finland, Special Paper, 53:401.
[3]	Loukola-Ruskeeniemi K and Heino T. 1996. Geochemistry and genesis of the black shale-hosted Ni-Cu-Zn deposit at Talvivaara, Finland[J]. Econ. Geol., 91: 80-110.
[4]	Loukola-Ruskeeniemi K, Uutela A, Tenhola M and Paukola T. 1998. Environmental impact of metalliferous black shales at Talvivaara in Finland, with indication of lake acidification 9000 years ago[J]. Journal of Geochemical Exploration, 63(1-3): 395-407.
[5]	Loukola-Ruskeeniemi K and Hannu L. 2013. Multiphase evolution in the black-shale-hosted Ni-Cu-Zn-Co depositat Talvivaara, Finland[J]. Ore Geology Reviews, 52: 85-99.
[6]	Peltonen P, Kontinen A and Huhma H. 1996. Petrology and[JP] geochemi-stry of metabasalts from the 1.95 Ga Jormua Ophiolite, northeastern Finland[J]. Journal of Petrology, 37(6): 1359-1383.
[7]	Young S A, Loukola-Ruskeeniemi K and Pratt L M. 2013. Reactions of hydrothermal solutions with organic matter in Paleoproterozoic black shales at Talvivaara, Finland: Evidence from multiple sulfur isotopes[J]. Earth and Planetary Science Letters, 367:1-14.

Full-Text