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东秦岭钼多金属成矿带,横跨陕西、河南两省。是我国重要的钼矿资源基地之一。自本世纪50年代发现以来,对矿带的基本地质特征,构造控制条件,岩体的成因和成矿专属性,以及热液蚀变等方面,进行了广泛深入的研究。发表了不少的论文和新的见解。深化了对本区的认识,促进了地质找矿工作。但以往的研究,对地层在成矿过程中的作用,均未给予应有的重视。笔者在研究本成矿带的成矿条件和控矿因素时,认为地层在成矿过程中的作用是不可忽视的。本文仅就此讨论,以补当前之不足,不妥之处,请予指正。
East Qinling molybdenum polymetallic metallogenic belt, across Shaanxi and Henan provinces. It is one of the important molybdenum resource bases in China. Since its discovery in the 1950s, extensive studies have been carried out on the basic geological features of ore belts, the tectonic control conditions, the genesis of the rock mass and its metallogenic specificity, as well as hydrothermal alteration. Published a lot of papers and new insights. Deepen the understanding of this area and promote geological prospecting work. However, previous studies have not given due attention to the role stratigraphy plays in metallogenesis. When studying the metallogenic conditions and ore-controlling factors in this metallogenic belt, the author thinks that the role of strata in the mineralization process can not be neglected. This article only on this discussion, to make up for the current problems, inappropriate, please correct me.