内断裂 meaning in Chinese
infaulting
Examples
- In the interim from highstand systems tract to transgressive systems tract , faulting is violent in the basin , different kind of fluids coming from dissimilar position of lithosphere enter into synsedimentary faults served as a place fluids mixed to form ore - bearing hydrocarbon alkali - fluids
在从高水位体系域向海侵体系域的盆地相迅速转化时，盆地内断裂构造活动强烈，断裂沟通不同部位的热水流体，使成矿烃碱流体沿断裂上升，在海底沉积成矿。 - The discourse discusses structure pattern , rupture - distributing law and ore - controlling action about mouru ore belt . grasping distribution rule of the fractures in ore - forming zone by remote sensing analyse and field survey , and made a research about the ruptures " ore - containing character in the different orientation , putting forward that four ne - orientation structure containing - ore zone alternate with strong and feebleness
论文详细地论述了牟乳含矿带的构造格局、断裂分布规律及控矿作用，通过遥感构造解译和实地考察，从宏观上整体把握了区域上和成矿带内断裂的分布规律，对不同方向上断裂的含矿性做了研究，并提出了牟乳矿带内北东向的四个强弱构造含矿带。 - Jiyang depression is a field where nonhydrocarbon is rich . these resources have close relation with the activities of the volcanos . at the same time , the activities of volcanos have deep contact with the activities of the faults . the growth of the faults in jiyang depression is great . by the research of the index number of the faults growth and the other researches , nw direction faults are the most ones in mesozoic , nw and ne and approximately ew directions all exist in cenozoic . the above reflects the whole geotectonic background that sinistral shearing stress field exists in mesozoic , but dextral shearing stress field exists in cenozoic
这些气藏与火山活动有密切的成生关系，同时火山活动与断裂活动也有密切的关系。济阳坳陷内断裂活动极为发育，通过断层生长指数等的分析，推断中生代断裂以北西向为主，新生代则兼有北西向北东向和近东西向的断裂，上述断裂发育特征反映了该区的大地构造背景，在中生代是左旋的剪切应力场，在新生代则是右旋的剪切应力场。 - Through the field observation and comparative seism - geologic studies , many seism - genesis soil - layer structures such as vibration - liquefied sand vein , vibration - liquefied sand dyke , sandy cobble dyke by fissure filling , seismic fall mass , seismic intra - layer fault and seism - settlement structures etc . were recognized
通过野外观测和比较地震地质学研究，识别出了振动液化砂脉、液化砂墙、裂隙充填砂质卵石墙、震塌落体、地震层内断裂及地震沉陷构造等地震成因土层构造。