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内碎屑的英文

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"内碎屑"怎么读用"内碎屑"造句

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  • intraclast

例句与用法

  • The microfacies characteristic of carbonate rock of suonahu formation in cuoqinin basin constitutes with the marl lithofacies , the intraclast ash lithofacies , biological detritus ash lithofacies
    措勤盆地唢呐湖组碳酸盐岩微相由内碎屑灰岩相、生物碎屑灰岩相和泥灰岩相组成。
  • Synthesizely contrasted the suonahu formation profile of the northern qiangtang basin and cuoqin basin of miocene epoch , used the intraclast ash rock as the marker bed of the suonahu formation
    对羌北盆地和措勤盆地中新世的唢呐湖组剖面作了综合对比,将内碎屑灰岩作为唢呐湖组的标志层。
  • The northern qiangtang basin suonahu formation microfacies of carbonate rock is divided for the intraclast ash lithofacies , biological detritus ash lithofacies , oncolite limestone lithofacies , contain the calcium and alga ash lithofacies , marl lithofacies and pure microlite limestone lithofacies
    羌北盆地唢呐湖组碳酸盐岩微相为内碎屑灰岩相、生物碎屑灰岩相、核形石灰岩相、含膏藻灰岩相、泥灰岩相和纯微晶灰岩相等6种微相。
  • Ore area locate on , silver factory ditch - ancient tomb ditch in west branch river set lower bench , stratigraphic succession , rock assemblage are different with circumference . most is a set of intraclast congeries silica rock . in search of it , its distribution range in the silver factory ditch - ancient tomb ditch
    矿区所在部位银厂沟?古墓沟一带,西岔河组下段地层中,地层层序、岩石组合特征与周边地区存在明显的差异。主要为一套内碎屑堆积的硅质岩。
  • The mineral rock - silica rock mostly composes of three kinds of silica qualities , and the first structure jasper silica rock , the second icrocrystal quartzite , the third the quartz grain clast . cement is carbonate , contain a little amount carbonate loach . silica rock , commonly assume edge angle or hypo - edge angle
    区内的含矿岩石?硅质岩主要由三种硅质成分构成,第一种为显脱玻?霏细结构的碧玉质硅质岩,第二种为微晶石英岩,第三种为石英颗粒内碎屑
  • Further research of lithofacies pvove : lode country output points belongs to tidal - flat facies . and the two sides belong to littoral facies - estuarine facies . ore area petrochemistry analyse also prove : intraclast congeries silica rock in basin have higher cu , ag abundance than circumference pena . the prominence inhomogeneity of the cu distribution indicates reconstruct of the late construction
    矿区内岩石化学测量也证明:盆地内发育的内碎屑堆积硅质岩比周围岩石具有更高的cu 、 ag元素地球化学丰度值, cu元素分布的显著不均一性,表明了后期构造的改造作用。
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