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交错层理的英文

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"交错层理"怎么读用"交错层理"造句

英文翻译手机手机版

  • cleap
  • cro edding
  • cross bedding
  • cross stratification
  • cross stratum
  • cross-bedding
  • cross-stratification
  • current bedding
  • currentbedding
  • diagonal stratification
  • discordant bedding

例句与用法

  • This channel is filled with cross-bedded sandstone .
    该河边充填着具交错层理的砂岩。
  • Bimodal cross - bedding
    双向交错层理
  • The dark - gray traction current deposits belong to internal - tide deposits , it develops sandstones and siltsands , and charactered with lenticular , wave , flaser bedding , bimodal cross - bedding and ripple mark
    深水牵引流沉积为内潮汐沉积类型,岩性为细砂岩、粉砂岩,以发育透镜状、波状、脉状层理、双向交错层理、波痕等沉积构造为特征。
  • Typical depositional structures of tempestite , such as radically arrangement of plate - like micrite gravel , hummocky lamination , load structure , grading bedding and ripple bedding are presented in the succession , indicating its accumulation in an offshore environment
    该风暴沉积的底面侵蚀构造清楚,板片状泥晶灰岩砾石呈菊花状排列,发育丘状交错层理、负载构造、递变层理和小波纹层理等沉积构造,为典型的浅海风暴岩。
  • Furthermore , sorting of the sandstones in the braided river is better compared with that of in the meandering river system . in the same subfacies , grain size is larger and sorting is better in the channel sandstones which developed with large - scale cross - beddings such as trough cross - bedding , compared with sandstones in the flood microfacies . in the same microfacies , better sorting and coarser grained sandstones are distributed in the middle and lower part of the unit
    与曲流河亚相相比,辫状河亚相砂岩的粒度较粗,分选性较好,砂体多次叠置而规模更大;相同河流亚相的河道微相与泛滥平原微相相比,前者的砂岩粒度较粗、分选性较好,发育槽状交错层理等大型层理构造;在同一微相内,处于中下部的流体单元其粒度较粗,分选较好。
  • However , the authors discovered recently that the top and bottom surfaces of the loushanguan formation are palaeokarst unconformity interfaces , and there are a lot of interbeds of granular ( oolite , pisolite and oncolite ) dolomite and algae - mat dolomite , especially sedimentary structures such as the bird ? s eye , stromatolite , cross bedding and tepee structures
    但笔者新近研究发现,其顶、底均为古岩溶不整合面,并有大量颗粒(鲕、豆、核形石)白云岩和藻纹层白云岩夹层,还有许多鸟眼构造、叠层石构造、交错层理、帐蓬构造存在。
  • The time corresponding to the four parts along the section are as follows : the top lake - swamp sediments : holocene ; the uppart fine sand : later late pleistocene ; the middlepart sandy clay : middle - early late pleistocene ; the lowpart clayer silt : later - middle - pleistocene . the fossils and stone artifacts found in salawusu site should be formed during the last but one glacier , its age range is about 0 . 13 - 0 . 19 ma , and belongs to later middle - pleistocene
    分析q曲线与氧同位素曲线的一致性以及以上研究结果,包含萨拉乌苏地层的这套沉积物的沉积时代为:顶部湖沼相沉积物:全新世;上部具交错层理的细砂:晚更新世晚期;中部粉砂质粘土:晚更新世中期至早期;下部粘土质粉砂:中更新世晚期。
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