斷裂滑塊 的英文怎麼說

中文拼音 [duànliègǔkuāi]
斷裂滑塊 英文
failed arm
  • 斷 : Ⅰ動詞1 （分成段） break; snap 2 （斷絕;隔斷） break off; cut off; stop 3 （戒除） give up; abstai...
  • 裂 : 裂動詞[方言] （東西的兩部分向兩旁分開） open
  • 滑 : 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...
  • 塊 : 名詞（古時佩帶的玉器） penannular jade ring （worn as an ornament in ancient china）
  • 斷裂 : break; disrupt; flying off; fracture; fragmentation; out break; rift;crack;bursting;rupture;rendi...
  1. The regional structure interpretation with 3d seismic data shows that the graben and shied mode faults of the baigezhuang, which developed a series of normal faults which stroked in ne ( nee ) and dipped nw or nw, came into being in the rift development stage of ii act of the bohai bay rift basin in mesozoic and cenozoic and resulted from the protrudent boundary of the basin, i. e. the strike - slip and stretch processes of baigezhuang fault

    同時，用三維地震資料進行區域構造解釋分析，論述了柏各莊地區的構造樣式，是中新生代渤海灣裂谷盆地的幕斷陷發育階段，同時由於盆地內凸起邊界?柏各莊斷層的走滑兼伸展作用，使柏各莊凸起的中生界形成壘、塹斷塊群構造樣式，發育一系列ne （ nee ）向，傾向nw或sw的正斷層。
  2. Sinistral strike - slip faults along the southern alashan margin and eastwards extending of the altun fault

    阿拉善地塊南緣的左旋走滑斷裂與阿爾金斷裂帶的東延
  3. Due to the west north direction subduction, fast collapse ( delamination ) may take place and the mantle plume emerged in ludong, in addition, owing to the subduction of pacific plate under eurasian, there appeared left - lateral advection and extension for tan - lu faults ( named as yishu fault in shandong ), and together with the collapse of yanshanian orogenic belts, all induced the crustal extension in shandong

    由於太平洋板塊對歐亞板塊的俯沖（ nw向） ，魯東地區巖石圈發生了快速拆沉減薄作用，同時魯東地區也可能會出現地幔柱的活動；另外，在太平洋板塊俯沖作用影響下，郯廬斷裂（山東稱沂沭斷裂）帶發生了大型左行走滑剪切和拉張活動。
  4. Through the regional background analysis in which western structures developed, it suggested that there did not exist a united and steady block to the west of ordos basin. alashan block neighboring on the north of the western margin was largely influenced by the action of qilian and tianshan - xingmeng folded belt which is respectively to the south and north of alashan block, was narrow in the steady block and was limited by the longshou mountain - zhongwei strike fracture in the south area

    通過對鄂爾多斯盆地西緣構造發育的區域構造背景分析，認為在鄂爾多斯盆地之西，一直沒有一個統一的穩定地塊相鄰，與盆地西緣北部相鄰的阿拉善地塊，受南北相鄰的祁連褶皺帶和天山興蒙褶皺帶活動的影響，較穩定地塊的范圍比較狹窄，其南又有龍首山-中衛走滑斷裂構造帶存在。
  5. Field investigation reveals that the latest time when yumen fault, western part o f qilian mountains was active is the end of the late pleistocene, and that the fa ult is coincident with other faults around west jiuquan basin. it is also found t hat yumen fault had not simply restricted to dip - slip motion ， strike - slip moti on is indicated. the results suggest that west jiuquan basin block might have rot ated clockwise

    新的證據顯示，位於祁連山西段酒西盆地南部的玉門斷裂的最新活動時代為晚更新世末，併兼有一定的走滑分量這一結果表明，酒西盆地塊體周邊斷裂的活動具有同時性的特點，酒西盆地塊體可能發生過順時針旋轉
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