摘要
通过对中国大量硫矿床地质工作的丰硕成果、大范围野外实地考查研究等实际资料的分析,进行了硫矿床的分类,同时考虑到地球发展演化中各地质时代(主要集中在晚太古代、中上元古代、震旦-寒武纪、泥盆-二叠纪及中新生代地层中)的成矿环境和构造控矿条件,在此基础上,对中国硫矿床在滨大平洋构造成矿域、古亚洲构造成矿域、特提斯-喜马拉雅构造成矿域中提出了24个成矿带(区)。
Systematic analysis of the rich results obtained from researching on and the objective records achieved from investigating into large numbers of the sulfur deposits in China was performed, thereby permitting their classification of deposit types. At the same time, minerlizing conditions and ore controlling structures for the various stages of the earth’s evolution, mainly such geohistorial stages as Late Archean, Middle to Late Proterozoic, Sinian to Cambrian, Devonian to Permian and Middle Cenozoic, were taken into full consideration so as to forecast the most potential mineralizing provinces amounting to 24 mineralizing belts and further 72 mineralizing zones which are all scattered about three main metalogenetic tectonic regions: circum Pacific, Palaeoasian and Tethyan Himalayan.
出处
《化工矿产地质》
CAS
1996年第3期173-178,共6页
Geology of Chemical Minerals
关键词
硫矿床
预测研究
成矿带
成矿预测
sulfur deposit, teclonic mineralizing region, circum pacific region, palaeoasian region, tethyan himalayan region