从已发生的矿床突水情况来看，绝大多数都发生在断裂构造附近，如断层密集带、交叉处、收敛处或尖灭端等部位。
The most water gushing-out from deposit occurred in the vicinity of faults, such as fault concentrated belt, intersect spot, convergence spot, pinch-out side and so on.
转换带密集发育的断裂系统为油气的运移和聚集提供通道。
The dense faults in the zone provide channel for hydrocarbon migration and accumulation.
青藏高原东北部向东逃逸而产生左旋剪切运动使该断裂成为一条青藏高原北部强震密集带。
It has the sinistral shearing due to the eastward escaping of the northeastern part of the Tibetan Plateau, which is a famous strong earthquake belt in north Tibetan Plateau.
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