滥木厂铊矿床控矿断裂构造形成的动力学机制  

The forming dynamical mechanisms of ore-controlling faults on Lanmuchang Thalliun deport

作　　者：任大银[1] 陈代演[2] 

机构地区：[1]贵州教育学院地理系,贵州贵阳550003 [2]贵州大学资源与环境学院,贵州贵阳550003

出　　处：《贵州教育学院学报》2006年第4期50-54,共5页Journal of Guizhou Educational College(Social Science Edition)

摘　　要：滥木厂铊矿床产于NE向滥木厂鼻状背斜核部和近核部,并严格受控于与背斜关系密切的NE向断裂组。实际地质资料和模拟实验研究都表明,该矿床控矿断裂为同成矿断裂。对该矿床同成断裂形成的动力学机制研究表明,其受多种因素控制。The Lamuchang Thallium deposit occurs in the core and near the core of the NE Lanmuchang anticline,and is controlled by NE-SW faults, which have relationship with the Lanmuchang anticline. Geological data and experimental data demonstrate that：ore-controlling faults are simultaneity-metallogenesis faults in this deposit. In this paper, writer mainly stadies the forming dynamical mechanisms of simultaneity-metallogenesis faults in this deposit.

关 键 词：控矿断裂 铊矿床 滥木厂 动力学机制 

分 类 号：P61[天文地球—矿床学]