steep fault
1.The frontal structure of Longmenshan in the west of Sichuan is very complex, showing intense structure deformation in overthrust belt, high structure amplitude, steep stratigraphic dip, developed fault blocks, complex seismic wave field, frequent change of lateral velocity, and poor image of post-stack time migration processing.
2.Thestructural top and close-to-fault parts of macro-axis of the high and steep anticline on the ancient updeclivity formed during Caledonian Movement are the favourable regions for explorating natural gas.
3.The main conclusions are as follows; Firstly, under the influence of three phases of episodic activities, three two-order sequences is composed of three depositional cycles and three regional unconformities; Secondly, under the control of structure activities such as fault-block activities and the influence of three-order climate cycles and source recharge, lower Cretaceous can be divided into six three-order sequence; Thirdly, because fault activities is weak and fault slope is gently, fan deltas exist in steep slopes in early and later stages and subaqueous fans exist and turbidite fans exist in troughs in middle stage.
4.In the light of independent bogie control and current-slip control for AC locomotive, the paper Discusses the menthod of fault judging & disposing for speed transducer, as well as solutions to main problems Such as slide/slip depression utilizing steep characteristics of asynchronous motor during speed signalProcessing.
5.Palaeogene Biyang fault depressed lacustrine basin experiences four evolutionary phases:foothill flooding depression→sulfate coastal/shallow lake→normal lake→carbonate or sulfate coastal/shallow lake, in pace of this, the evolutionary process of sedimentary wedge is from fluvial fan→steep slope fan delta→gentle slope fan delta→fluvial fan in southern margin which belongs to steep slope zone, and is fluvial fan→delta→fluvial fan in northern margin which belongs to gentle slope zone.
