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锡矿山是我国最大的锑矿产地,具有八十七年的开采历史。该矿床规模巨大,类型独特,为我国唯一的整合型锑矿床,矿床学上称之为“锡矿山式锑矿”。矿床的成矿控制因素,“主要是背斜加断层,容矿层上覆盖遮挡层。西部大断层是矿液的主要通道,背斜轴部是矿化富集的主要部位,长龙界页岩是矿化富集不可缺少的条件,七里江硅化灰岩是本区唯一的含矿层位。”这一成矿规律从五十年代至今,一直为中外地质学者所公认,有效地指导了本区的评价勘探工作。本区的评价勘探工作持续了二十余年,投入了大量钻探和坑道工程,积累了丰富的地质资料,并探明了一定的锑矿储最。但以往的勘探工程基本上集中在整合型的似层状矿床上,而对西部大断层下盘的矿体,
Tin mine is China’s largest antimony mine, with 87 years of mining history. The deposit is huge in scale and unique in type. It is the only integrated antimony deposit in China. The ore deposit is called “tin mine antimony mine”. The metallogenetic control factors of the ore deposits are mainly anticline plus faults and overburden on the ore-bearing layers.The major faulting in the western part is the main channel of ore fluid, and the anticline axis is the main part of mineralization enrichment. The Changlongjie shale is The mineralization enrichment indispensable conditions, Qili River silicified limestone is the only ore-bearing layer in this area. "Since the 1950s, the metallogenic regularity has been recognized by Chinese and foreign geologists and effectively guided the Evaluation of exploration work. Evaluation of the region’s exploration work lasted more than 20 years, invested a lot of drilling and tunneling project, has accumulated rich geological data and proved a certain amount of antimony ore reserves. However, the previous exploration projects basically concentrated in the integrated stratified deposit, and the large faults in the western ore body,