Based on volcanic activities and tectonic evolution, it is suggested that the tiltedfaultblock, sliding structures in extensional setting should be developed in Cretaceous to Cenozoic age.
结合区域火山活动和构造演化认为,该滑动构造为伸展背景下的掀斜断块型,其滑动时间为白垩纪—新生代。
2
These terraces were offset and deformed by Jiazhiwan fault, along which the uplifted Xizhou-Taihang faultblock was tilted.
甲子湾断层使这些阶地错断变形,系舟山-太行山断块隆起沿该断层产生翘起运动。
3
Block faulting activities inside basin develops, forming NE and NW fracture systems, thus cutting this basin into 47 tiltedblock faulting body and a series of overlying dustpan-like fault depression.