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宏观构造的英文

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"宏观构造"怎么读用"宏观构造"造句

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  • macroscopic structure
  • macrostructure

例句与用法

  • Directions are obtained by two means : calculation and measure . our investigations are summed as follows : 1 the lpo relations between olivine and orthopyroxene are different from usually situations : 100ol 001opx , 010ol 100opx , 001ol 010opx ; 2 the seismic anisotropy of the ultramafic rocks in damaping is obvious . their characters are consistent with the structures of the rocks and fabrics of minerals , which means seismic anisotropy is mainly controlled by rocks fabrics ; 3 seismic velocities suggest that the composition of upper mantle in damaping region is resemble to the xenoliths , which major component is lherzolite
    不同2大麻坪地区幔源包体的波速各向异性显著,岩石的波速各向异性特征与其宏观构造和微观组构一致,说明岩石组构是造成地震波速各向异性的决定因素3由地震波速推测的大麻坪地区的上地幔成分与包体出露的情况一致,即主体为二辉橄榄岩。
  • Those two phases of conjugated shear joints are differ from each other in spatial distribution , which is a reflection of the spatial evolution of the fault zone . it can beinferredfrom the information about macrostructure , superimposed deformation of tectonites , paleotectonic stress field of joints and other related documents that there had been three stages of significant activity since zijingguan fault zone was activated . the first stage was about from middle juiassic to early cretaceous , when the fault zone activated left - laterally under nw - se striking transpression
    宏观构造组合特征、构造岩变形叠加信息、节理的古构造应力场信息及前人区域资料表明,紫荆关断裂带自古生代末开始活化以来有三次主要构造活动:第一次是中侏罗世?早白垩世,在北西?南东向近水平挤压作用下,断裂左行压扭性活动,控制太行山地区岩浆岩带及与其相关的接触交代型矿床的形成。
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