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Home > english-chinese > "正断层" in Chinese

Chinese translation for "正断层"

down fault
downthrow fault
normal fault
normal gravity fault
normal slip fault
normalfault
ordinary fault
trap-down
true fault


Related Translations:
断层方向:  fault trend
断层前锋:  fault front
沉积断层:  depositional faultsedimentary fault
活断层:  active fault
断层迹:  fault tracetrail of a faulttrail of faulttrail of the fault
辐射断层:  radial faults
界面断层:  boundary-fault
开张断层:  open fault
顺向断层:  consequent fault
断层片:  laminagramstratigram
Example Sentences:
1.Analysis on distribution features of gas outburst from two walls of normal fault and geological origin
正断层两盘的瓦斯突出分布特征及其地质成因浅析
2.The focal mechanism is mainly left - lateral strike - slip , with a very small normal fault slip component
这次地震的震源机制基本上是左旋走滑,带有微小的正断层滑动分量。
3.The faults consist of three groups : one is nw direction , others are ne to nee direction and sn direction . the group which is nw direction is the most important one
断裂构造十分发育,均为正断层,主要有三组,北西向、北东北东东向和南北向,其中以北西向一组最为发育。
4.The extensional and transtentional structure existed in huabei belongs to vent fault , fracture is mainly stepwise normal fault , whose preservation condition is not good
华北地区多为张性,张扭性构造,属于排气断层,形成的断裂多为阶梯状,以正断层为主,保存条件欠佳。
5.Different tectonic style exists in the upper and lower layers of the yanshanian boundary . the lower layers takes on the tectonic style of thrust fault and nappel . the upper layers hi step positive fault
2 、盆地燕山期构造界面上下不同构造层具有完全不同的构造样式,构造界面下伏构造层呈现冲断褶皱、推覆构造样式,构造界面上覆构造样式为阶梯状正断层,整体呈现“双层”结构型式。
6.2 . tazhong ancient uplift originated from normal fault in paleozoic , hydrocarbon formed in ordovician period , structure reverse made tazhong uplift form from the middle ordovician period to the late ordovician period , and it provided geologic background for the deposit of silurian - devonian stratum . tazhong uplift formed at the end devonian , ancient reservoir was destroyed and asphaltum sandstone formed , structure deformation more destroyed ancient reservoir in early permian , after then the major of structure deformation is regulation
塔中隆起源于早古生代拉张背景下的正断层,寒武-奥陶纪为其烃源岩形成的重要时期;早奥陶世末-晚奥陶世末的构造反转是塔中隆起的主要形成期,同时也为志留系形成地层及复合圈闭提供了古地理背景;志留?泥盆纪塔里木盆地南北缘均转为活动大陆边缘,形成了大量的断裂和不整合;泥盆纪末塔中鼻状隆起基本定型,古油藏遭受破坏,形成了沥青砂岩;早二叠世晚期的构造变形使古油藏遭受进一步的破坏;二叠纪后构造变动主要以调节为主。
7.The results of 2 - d resistivity inversion of the yishui - tangtou and the liujazhuang faults indicate that electrical structures on both sides of the fault zone present obvious difference , the resistivity of the hanging wall is low and partially high , while that of the foot wall is high , and the faults are high - obliquity faults
沂水汤头断裂、刘家庄断裂的二维电阻率反演结果表明,断裂带两侧的电性结构呈现出整体性的差异,正断层的上盘为低阻区和局部高、低阻扰动区;而断层下盘多为均匀的高阻区;断层为高角度断层。
8.The regional structure interpretation with 3d seismic data shows that the graben and shied mode faults of the baigezhuang , which developed a series of normal faults which stroked in ne ( nee ) and dipped nw or nw , came into being in the rift development stage of ii act of the bohai bay rift basin in mesozoic and cenozoic and resulted from the protrudent boundary of the basin , i . e . the strike - slip and stretch processes of baigezhuang fault
同时,用三维地震资料进行区域构造解释分析,论述了柏各庄地区的构造样式,是中新生代渤海湾裂谷盆地的幕断陷发育阶段,同时由于盆地内凸起边界?柏各庄断层的走滑兼伸展作用,使柏各庄凸起的中生界形成垒、堑断块群构造样式,发育一系列ne ( nee )向,倾向nw或sw的正断层
9.The extending major fault has a strike of north - east , controlling the forming of depressions and evolution of sedimentation . the nature of the fault is normal in the early stage . later with the reformation of sliding effect , normal faults are still the main faults , and the plane distribution of the faults occurs sectionally
取得了一系列的研究成果:辽河滩海地区主要有三种构造样式,即伸展构造样式、走滑构造样式及反转构造样式,其中,以伸展构造样式为主,伸展主干断裂走向以北东走向为主,控制凹陷形成和沉积演化,断裂性质早期为正断层,后期经走滑作用改造,至今仍以正断层形式出现,断裂平面展布具有分段性。
Similar Words:
"正端" Chinese translation, "正端钮,正接线柱" Chinese translation, "正端子" Chinese translation, "正段" Chinese translation, "正断" Chinese translation, "正断层;相对误差" Chinese translation, "正断层带" Chinese translation, "正断层地堑" Chinese translation, "正断层谷" Chinese translation, "正断层活动" Chinese translation