The wall-rockalteration is complex, and the boundary line between orebody and wall-rock is obvious.
围岩蚀变复杂,矿体与围岩界线明显。
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The main purpose of this paper is to introduce a new method to study the immobile elements and mass transport of in geochemical process of wall-rockalteration.
In this paper formational environment of host rock, wall-rockalteration, sulfur, oxygen, carbon isotopes, mineralization temperatures, ore composition were studied.