中国科技核心期刊
美国化学文摘社(CAS)数据库
美国EBSCO学术数据库
日本科学技术振兴机构数据库(JST)
In recent years,significant progress has been made in studying the relationship between Yunshan complex rock mass and tin mineralization in Yunshan Mining Field,but major breakthroughs in finding large-scale tin polymetallic deposits have yet to be achieved.Tin mineralization in the mining field primarily occurs in the contact zones of Yunshan complex rock mass,such as rock intrusions,rock tongues,concave valleys of rock mass,and NNE faults.The main types of deposits formed are contact metasomatic type,magmatic hydrothermal type,and metamorphic hydrothermal type.Among these,the contact metasomatic type and magmatic hydrothermal type deposits are characterized by considerable orebody thickness,intense alteration,and high grades.Currently,several small tin deposits have been discovered in the Yunshan Mining Field,with orebodies found in the contact zones of the rock mass and NNE faults.Many areas within the mining field exhibit similar mineralization conditions,suggesting that increased geological exploration efforts could lead to significant breakthroughs in prospecting.