Strike-slip tectonics formed possibly in Himalayan Period when the boundary faults thrusted and right lateral strike slipped concurrently, intersect the boundary faults of the central geotectogene and collocate like the en-echelon faults.
英
美
- 在中央拗陷帶內走滑斷層與邊界主斷層斜交并呈“雁列式”排列，表明走滑構造可能在邊界斷層發(fā)生大規模逆沖兼右行走滑時(shí)形成，其形成時(shí)期可能為喜山期。
