有机质在层控汞矿床成因中的作用
THE ROLE OF ORGANIC SUBSTANCE IN THE ORE FORMATION OF STRATA-BOUND MERCURY DEPOSITS
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摘要: 有机质与金属矿床的关系问题,是七十年代以来国内外地质工作者所重视的研究课题之一。不少学者对这个问题作过研究,并认为某些金属矿床的形成,常与有机质参与有密切关系。我国著名的万山型层控汞矿床,在物质组份上,常以富含有机质为特色。同时,在赋存汞矿床的中、下寒武统地层中,汞丰度与有机质含量亦有密切关系。本文主要通过对万山型层控汞矿床及其所赋存地层中的有机质与汞迁移、富集关系的初步研究,探讨有机质在层控汞矿床成因中的作用。Abstract: Wanshan type of strata-bound mercury deposits in East Guizhou-West Hunan, including the deposits in Wanshan, Dadongla, Chatian, Jiudiantang, etc. areas, has the following analogous geological characteristics and ore-forming conditions.
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[1] (1)Herfert L.Window, 1976, Geochemical Interaction of Heavy Metal in South-eastern Salt March Environments Ecological Research Series EPA-600/ 3一76-023.
(2)Berge, G.et al.1972, A Polluton Survey of the Trondheim Fjord as Influenced by Sewage and the Pulp Mill Industry.(Marine Pollution and Sea Life)Ed.Merio Ruive, Fishing Dews(Books) Ltd.P, 10一15.
(3)Yoshida, T.et al.1967, Trasference Mechanism of Mercury- in Marine Environment, J, Tokyo,Uuiv。Fish, 53 P.73一84. -

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