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1)  The Bozhang fault zone
渤张断裂带
1.
The Bozhang fault zone being a transtensional fault zone, was formed in Mesozoic, which has been active and controlled the distribution of Mesozoic and Cenozoic sediments since Mesozoic.
渤张断裂带形成于中生代，为剪张性断裂带。
2)  Zhangjiakou-Bohai fault zone
张家口-渤海断裂带
1.
The activity of Zhangjiakou-Bohai fault zone was analyzed with GPS data by cluster method.
利用GPS资料,采用聚类分析方法分析张家口-渤海断裂带(简称张渤带)的活动性,分析表明:张渤带是首都圈地壳运动最强烈的断裂带。
3)  Zhangdong-Qidong faulted structural belt
张东一歧东断裂构造带
4)  Huayuan-Zhangjiajie fault belt
花垣-张家界断裂带
5)  Zhangjiakou-Penglai Fault Zone
张家口-蓬莱断裂带
1.
Characters of the Zhangjiakou-Penglai Fault Zone Activity in the Bohai Sea Since Late Quaternary
张家口-蓬莱断裂带渤海段晚第四纪活动特征
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6)  extension torsional fault
张扭断裂
补充资料：渤渤
1.流水声。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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