滑動礫巖 的英文怎麼說

中文拼音 [dòngyán]
滑動礫巖 英文
slide conglomerate
  • : Ⅰ形容詞1 (光滑; 滑溜) slippery; smooth 2 (油滑; 狡詐) cunning; crafty; slippery Ⅱ動詞(貼著物...
  • : 名詞(小石塊; 碎石) gravel; shingle
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • 滑動 : slither; slippage; slipping; slide; sliding; run; sliding movement [motion]; glide; slump滑動閘門...
  1. There are typical laminated structure, soft sedimentary - slipping deformed structure, syngenetic brecciated structure in the ore which are the mirror of syngenetic sedimentation. the other type of ore has the charactristic of epigenetic mineralization, which is called as telescoped ore. the ore occurs in vein, pocket, lensoid and bedd

    礦石中發育典型的紋層狀構造、軟沉積變形構造、同生角構造等反映同生沉積特徵的礦石構造;另一類礦石具有明顯的後生成礦特點,稱之為疊生改造型礦石,礦石產于脈狀、囊狀、透鏡狀及似層狀礦體中,與燕山期漿及斷裂裂隙構造關系密切。
  2. The cataclastic rocks appeared in the fault zone include structural lenticles, fault breccias, protocataclasite and cataclasite. the microscopical cataclastic deformation mechanisms involved are microcracking, frictional sliding and pressure - solution, but there might have had ductile deformation relating to dislocation sliding in feldspar and quartz of the plutons

    斷裂帶內碎裂系列構造主要是碎裂化石(包括構造透鏡體和構造角) 、初碎裂和碎裂,顯微變形機制主要有破裂作用、摩擦和壓溶作用。
  3. D ) the invasion of jinningian - chengjiangian alkali basite were unambiguous, the distribution of those rocks form " z " in shape, which similar with luoyin fracture zone and the distribution of copper deposit. it shows that copper deposits were controlled by discordogenic fault and its derived sub - structure, and there are relationship between copper deposit and jinningian - chengjiangian alkali basite. e ) most of minerogenetic age of copper deposit, which located in kunyang rift valley, belongs to jinningian - chengjiangian ( between 900 - 650ma ), similar with the time limit of breaking - up of rodinia

    東川礦區晉寧-澄江期堿基性侵入活明顯,常作為因民組復雜角膠結物和脈(體)產出,多分佈於深大斷裂及其派生的次級構造附近,明顯受南北向小江深大斷裂走引起的右行旋扭及其派生構造控制,與「落因破碎帶」和「銅礦分佈」較吻合,均為「 z 」字形。
  4. Ground - up shells of marine organisms mixed with pebbles, clay and eroded rock, deposited there over many millennia, now form a bed of muddy paste that is so soft and well lubricated that the ice streams can glide along even more easily than earlier researchers expected

    有科學家將積冰融化出一公里長的窄洞,採集古老海床的樣本,結果發現地底混雜了海洋生物殼體、石、黏土與風化,幾千年下來形成又軟又的泥床,使冰流較先前研究人員預期的更容易
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