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下盘的的英文

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"下盘的"怎么读用"下盘的"造句

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  • underlying

例句与用法

  • The motion of lower plate can be selected discretionarily in the few motion modes such as device prizing , hydraulic cylinder and steel wheel according to the situation of construction site and the working habit of construction unit to content construction ' s requirements .
    下盘的移位可根据施工现场情况及施工单位的工作习惯,在撬装、液压缸步标、钢轮等几种移位方式中任意选取,以满足施工的要求。
  • The first stage was characterized by ductile detachment deformations , and during 228ma - 170ma took place high temperature flow deformation and in the period of ivoma - 135ma middle - low temperature deformations occurred , as shown by deformations feature and history of mylonite granites
    亚干变质核杂岩的运动学各类构造要素产状协调一致,表明为同期构造产物。其各种宏观、微观运动学标志几乎都表现为上盘对下盘的向sse的剪切运动。
  • Through reservoir prediction , it indicated that the reservoir in mainan structure and mopan - laowan buried structure which located in short limb and bottom wall were finely developed , this two areas were the primary area for the further exploration and drill site design in dachiganjing structural belt
    通过储层横向预测,发现麦南构造和陡翼断层下盘的磨盘老湾潜伏构造储层较发育,是大池乾井构造带下一步勘探及井位部署的重点区域。
  • According to the spread of nappe and relation between the nappe and depression , oblique - thrust fault zone was divided into three parts in this paper : sertengshan , lvliangshan and xitieshan . ( 3 ) according to macroscopic characteristics of fault zone , cleavage characters of fault zone , drag folds , the reverse " s " fold in the footwall , positive flower structures and small left strike - slip fault , the kinematics characters of fault zone of sertengshan - xitieshan are concluded : thrusting in section , left - slip fault in plane and the strike - slip displacement increasing from the west to the east
    ( 3 )根据断裂断裂带的宏观特征、断层带劈理特征、断裂带附近的牵引褶皱和断层下盘的平面反“ s ”型褶皱以及断层上盘剖面正花状构造和平面左行小型平移断层,认为赛什腾-锡铁山断裂带运动学主要表现为剖面上的逆冲、平面上的左行走滑特点,并且走滑量具有自西向东增大之势。
  • Seismic inversion results indicate that the delta sandstone reservoirs occurred extensively in the 2nd and 3rd intervals of dongying formation , lower tertiary , and become poor only to the western margin of the survey area . in contrast , the fan delta sandstones in shahejie formation developed mainly in the area between fl and f2 faults , and turbidity sandstones locally in the rest of the survey area
    储层预测结果表明,东二、三段储层除工区北部西侧外,普遍发育较好;而沙河街一、二段和沙三段储层主要集中在f1断层下盘的中台阶地区及f2断层下盘,其它地区发育一些规模不等的浊积扇。
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