摘要
招掖金矿带金矿床受断裂构造控制的特点十分明显，研究表明这些控矿断裂具有复杂的演化历史，经历过至少四期变形作用，但金矿化主要发生在控矿断裂的张性演化阶段。断裂构造不仅控制着金矿化的时间，而且控制着金矿体（床）的空间分布及产状，同时也控制着金矿化类型。
The ore-controlling faults in the Zhaoye Gold Belt have complex activity history, which have undergone at least four phases of deformations. Gold mineralization in the belt took place at the tensile deformation phase of the faults. The faults not only controlled the timing and the type of gold mineration, but also the distribution and occurrence of gold ore bodys.
出处
《地质找矿论丛》
CAS
CSCD
1997年第1期26-35,共10页
Contributions to Geology and Mineral Resources Research
