摘要
蔡凹锑矿位于陕豫锑矿带的西段，为矿带中典型的锑矿床。其控矿岩系主要为秦岭群中部雁岭沟组石墨大理岩。区内构造发育。用深变质地层多期变质变形的观点和方法，重点讨论矿区的4期构造组成型式、控矿构造及容矿构造的特征，阐明蔡凹锑矿属典型的构造控矿类型。
The Caiwa middle - sized antimony deposit is located on the western Shanxi-Henan antimony ore belt, The hosting rocks are Yanlinggou Formation graphite marble of the Qinling Group. The structures are well developed. The structural styles of four periods, ore -controlling structures and ore- hosting structures are described.
出处
《矿产勘查》
1999年第1期53-59,共7页
Mineral Exploration
关键词
锑矿
秦岭
陕西
Antimony ore depsit
Qinling
Shaanxi
