strike slip 中文意思是什麼

strike slip 解釋
走向位移
  • strike : vt （struck; struck 〈古語〉 stricken;striking）1 打，敲，擊，毆；碰，撞，攻擊，沖擊。2 （用尖刀...
  • slip : SLIP ＝Serial Line Internet [Interface]Protocol 【計算機】串線網際協議。vi （slipped 〈古語〉 sli...
  1. 4 ) analyses boundary faults of the cenozoic longmenshan foreland basin, and thinks the basin boundary faults, being active fault, are thrust and dextral strike - slip. so the longmenshan foreland basin is dextral strike - slip foreland basin

    4 ）通過對新生代龍門山前陸盆地邊界斷裂的考察分析，認為盆地邊界斷裂具逆沖推覆及右旋走滑作用特點，為活動斷裂。
  2. 5 ) quantitative analysis to the dayi conglomerate in the cenozoic longmenshan foreland basin has been carried out. the results indicate that the dextral strike - slip rate is 1. 02 mm / a, the average sedimentary rate is 0. 143 mm / a, and the average decline rate is 0. 3mm / a

    5 ）對新生代前陸盆地大邑礫巖作定量分析，結果表明，大邑礫巖沉積時期，前陸盆地滑移量為1 . 02mm a ，沉積速率為0 . 143mm a ，平均沉降速率為0 . 3mm a 。
  3. Especially interesting is the serpentinous peridotite in this belt occurred as lense blocks of various sizes, and superimposed with other geological masses with faults, and in combine to constitute the mixture. system in the belt. five tectonic stage can be discerned in this area : ( 1 ) south - north ward overthrust ; ( 2 ) sinistral strike - slip ( 3 ) dextral strike - slip ( 4 ) south - north ward overthrust ( 5 ) northeast, northwest late stage fault

    本區上述的結構構造特徵先後經歷了五期構造作用，依次為： （ 1 ）南北向逆沖推覆； （ 2 ）左行走滑； （ 3 ）右行走滑； （ 4 ）南北向擠壓推覆； （ 5 ）北東向、北西向晚期斷裂；
  4. This paper was completed based on researches of orefield structures of baiyangping multi - metal mineralization concentrated field, and analysis on structure dynamics of ore - concentrated area and adjacent in lanping - weixi area, yunnan province. in baiyangping ore concentrated area, the master mineralization epoch is in lanping basin became imbricate down - warped, strike - slip and pull - apart basin

    本文是在雲南蘭坪?維西地區白秧坪多金屬礦化集中區的礦田構造研究基礎上，對礦集區及滇西較大范圍進行的構造動力學分析研究成果。
  5. Strike - slip model for altyn tagh fault developed since late mesozoic

    晚中生代以來阿爾金斷裂的走滑模式
  6. 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。
  7. The radiocarbon ages of charcoal and their implication derived from ciergou site along the haiyuan strike - slip fault

    永定河上游晚更新世晚期以來的堆積階地年代測定
  8. Visco - elastic model of interaction between parallel strike - slip faults and seismicity reduction effect

    平行走滑斷層相互作用的粘彈模型和減震作用
  9. 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
  10. The geological and geophysical studies show that there are large discrepancies for the distribution, strike - slip direction and tectonic styles of the faults in the southern and northern parts of the qinghai - xizang plateau, and for the deep crustal architectures in the eastern and western parts of the southern plateau

    摘要青藏高原南部與北部的斷裂帶走滑方向不同，斷裂帶在高原東、西兩側的展布規律和構造運動方式也存在極大的差異。
  11. The main structure style of chagan sag included four kinds, such as extension, compression, inversion and strike - slip structure, in which the extension structure was the principle part

    查干凹陷的主要構造樣式包括伸展、擠壓、反轉和具有走滑分量的構造，其中伸展構造是主體。
  12. The strike - slip faulting was caused by asymmetrical distribution of barriers on the subducting plate. the nne - ssw distributed aftershocks occurred on, or near, the fault plane of the main shock ; while the nw - se distributed aftershocks, on, or near, the mentawai fault

    北北東?南南西向分佈的餘震發生在主震的斷層面上（或其附近） ；而西北?東南向分佈的餘震則發生在明打威斷層上（或其附近） 。
  13. 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。
  14. 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。
  15. The paper gives a mechanical and history analysis on the characteristic of laojunshan metamorphic core complex in southeastern yunnan and its structural environment, and considers that metamorphic core complex is actually a nuclear column of a vortex structure, which was caused by the wenshan ? malipo strike - slip fault

    通過滇東南老君山變質核雜巖特徵及周圍構造環境的力學分析及歷史分析認為，該變質核雜巖實質上是旋扭構造的砥柱，而旋扭構造又源於文山?麻栗坡斷裂的走滑運動，拆離伸展構造晚于旋扭構造。
  16. In the overlap part of the right side of two main faults, the left - lateral strike - slip movement of them in quaternary has formed the embryonic rhombochasm

    在兩條主要左行走滑斷裂的右側疊覆區，兩條主斷裂第四紀的左行走滑運動產生一個胚胎期的菱形斷陷。
  17. It has been found that there are strike - slip downfaults along the shiting river between the shifang city and mianzhu city by the remote - sensing geological interpritation and geochemical and geogas surveys

    摘要利用遙感地質解譯以及土壤地球化學測量和地氣測量，發現沿四川綿竹市和什邡市之間的石亭江發育走滑斷裂。
  18. In himalayan, the first era ( 45ma ) the basin is titled ; the second era ( 23ma ) it is differential uplift and denude ; the third era it is brittle defonnation. in eastern ore belt, ore - controlling is mainly strike - slip fault and fold ; but in western ore belt, it is block

    喜馬拉雅運動第一期45ma盆地掀斜；第二期23ma以差異隆升剝蝕為主；第三期4ma為脆性變形期，東礦帶近盆邊以走向斷裂及褶皺控礦為主，西礦帶為斷塊控礦。
  19. 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。
  20. Multi - stage strike - slip motion and uplift along the altyn tagh fault since the late cretaceous

    晚白堊世以來沿阿爾金斷裂帶的階段性走滑隆升
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