A holocene zinc orebody formed by supergene replacement of mosses
作者： Ian R. Jonasson , Lionel E. Jackson , Donald F. Sangster
DOI: 10.1016/0375-6742(83)90067-5
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摘要: Abstract An extensive deposit of secondary zinc minerals has been formed at Howard's Pass, Yukon by replacement mosses and as a cement within talus. The deposits are Holocene age (younger than 9610 yr. B.P.) occur in blanket peat bogs percolated zinc-rich springwaters. Buried moss strata undergo cell forming zincian clacite, smithsonite hemimorphite. last is the most important mineral both
sci-hub.se 参考文章(3)
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W.D. Goodfellow, I.R. Jonasson, J.M. Morganti, Presented paperZonation of chalcophile elements about the howard's pass (XY) Zn-Pb deposit, Selwyn Basin, Yukon Journal of Geochemical Exploration. ,vol. 19, ,(1983) , 10.1016/0375-6742(83)90044-4