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该文通过s-t过程线上某些测点间间距的突变推断两测点间有软弱夹层、裂隙或断层存在 ,并通过小浪底工程进水口边坡F4 2 1断层产状的佐证 ,认为s -t过程线参与不明地质构造的判断是可行的
This paper deduces the existence of weak sandwiches, fissures or faults between two measuring points through the sudden change of the spacing between some measuring points in the st process line. Through the evidence of the fault shape of the F4 2 1 fault at the inlet of the Xiaolangdi Project, s -t Process line to participate in the determination of unknown geological structure is feasible