走向滑動斷層 的英文怎麼說

中文拼音 [zǒuxiànggǔdòngduàncéng]
走向滑動斷層 英文
strike-shift fault
  • 走 : 動詞1 （人或鳥獸的腳交互向前移動） walk; go 2 （跑） run 3 （移動; 挪動） move 4 （離開; 去） lea...
  • 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...
  • 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...
  • 層 : i 量詞1 （用於重疊、積累的東西 如樓層、階層、地層） storey; tier; stratum 2 （用於可以分項分步的...
  • 走向 : 1 （延伸的方向） run; trend; alignment 2 （向某方向發展） move towards; head for; be on the way t...
  • 滑動 : slither; slippage; slipping; slide; sliding; run; sliding movement [motion]; glide; slump滑動閘門...
  • 斷層 : fault; slip; slicle; fracture; dislocation
  1. According to the spread of nappe and relation between the nappe and depression, oblique - thrust fault zone was divided into three parts in this paper : sertengshan, lvliangshan and xitieshan. ( 3 ) according to macroscopic characteristics of fault zone, cleavage characters of fault zone, drag folds, the reverse " s " fold in the footwall, positive flower structures and small left strike - slip fault, the kinematics characters of fault zone of sertengshan - xitieshan are concluded : thrusting in section, left - slip fault in plane and the strike - slip displacement increasing from the west to the east

    （ 3 ）根據斷裂斷裂帶的宏觀特徵、斷層帶劈理特徵、斷裂帶附近的牽引褶皺和斷層下盤的平面反「 s 」型褶皺以及斷層上盤剖面正花狀構造和平面左行小型平移斷層，認為賽什騰-錫鐵山斷裂帶運動學主要表現為剖面上的逆沖、平面上的左行走滑特點，並且走滑量具有自西向東增大之勢。
  2. Yanqi basin is an intermont basin of tian shan, there is a nww trending right lateral strike slip active fault in southwestern basin, its maximum slip distance is 210m, and slip rate is about 10mm / yr, moreover, there is a west - east trending active anticline along northern basin

    焉耆盆地是一個天山山間盆地，盆地西南緣發育一條走向北西西的右行走滑活動斷層，最大走滑距離為210m ，走滑速率約10mm / yr ，盆地西北緣發育走向近東西的活動褶皺。
  3. Sudden rupture and displacement occurs with normal, reverse, strike-slip, or oblique-slip faulting.

    突然破裂和位移伴隨正、逆、走向滑動或斜向滑動斷層作用而發生。
  4. The ne - strike compressional faults are not intersected with the ew ma in fault zone, but a kind of transform structure resulted from its right lateral strike slip, and one of the typical example is the mesozoic thrust systerm in the northeast side of the main fault in western liaoning

    在青龍斷裂帶兩側，分佈有許多北東向壓性斷層，它們與東西向主斷裂帶不是簡單的切割關系，而是東西向主斷裂帶右行走滑活動中的分支斷裂，位於青龍斷裂帶北東側的遼西地區中生代逆沖推覆構造，也是青龍斷裂帶在右行走滑作用下，因構造方向的改變發生構造轉換的結果。
  5. The fault zone passes through the offshore between the changdong islands and the dazhudao island, and consists of a group of nw trending faults, which are dominated by normal and reverse slips with strike - slip component

    該斷裂帶由一系列北西走向的次級斷層組成，主體在長島至大竹島之間的海域，多數斷層以正斷兼有走滑運動為主，部分斷層具有逆沖運動性質。
  6. A complete suit of closely analytical expressions of stress field is presented for the strike - slip shear fault with an arbitrary dip angle in a semi - infinite medium. checking and reviewing the analytical expressions of stress field by other researchers, closely mathematical reasoning for the expressions is done again, thus this suit of expressions has become more perfect and reliable

    給出了半無限空間中任意傾角的走向滑動剪切斷層錯動產生的應力場的一套嚴密的解析表達式.對前人所做的該方面的工作進行了檢驗和回顧，重新對公式進行了嚴密的數學推導，給出了正確的結果，使得這一套公式更加完善和可靠
  7. Strike - slip seismic fault and mainshock - aftershock earthquake sequences are dominant in whole yunnan area

    總體上雲南全區地震斷層以走向滑動為主，地震序列以主餘震型為主。
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