摘要
湘西花垣—张家界断裂带显逆冲压扭性，与其分枝断裂古丈—张家界断裂带关系密切，平面上在张家界市后坪复合，具有类似的地质特征。形成时代较古丈—张家界断裂带晚，时间上有先后及成生关系，向上呈叠瓦状，深部收敛在一起。具有明显的控矿作用。
Huayuan-Zhangjiajie fault zone showing thrust and compress-shear,has a close relationship with its branch falut:Guzhang-Zhangjiajie fault zone.On Plane,they compounded at Houping,Zhangjiajie city.They have the analogous geological characteritics.Its formation time is later than Guzhang-Zhangjiajie fault zones.In formed time,they have the relationship of the early or late and origin,upper,presents imbricate,and deep,does convergence.It has the obvious deposit-controlled.
出处
《湖南地质》
1998年第2期96-99,104,共5页
Hunan Geology
