normal faulting中文是什么意思

發(fā)音:

中文翻譯
造句

正斷層活動

normal adj. 1.正常的，平常的，普通的；平均的。 2.正規(guī) ...
fault n. 1.過失，過錯；罪過，責任。 2.缺點，缺陷，瑕疵 ...
conjugate normal faulting 共軛正斷裂作用
listric normal faulting 鏟狀正斷層作用
faulting 垂直錯; 斷層錯動; 斷層作用；斷裂; 斷裂運動; 擠壓誘發(fā)逆斷裂活動
antithetic faulting 反向斷層作用
area of faulting 斷層區(qū)
axial faulting 軸斷層; 軸向斷層作用
badly faulting 強烈斷層活動
block faulting 塊斷運動; 塊斷酌; 塊斷作用; 塊狀斷層作用
brittle faulting 脆性斷裂作用
compressional faulting 擠壓斷裂作用
core faulting 核部斷層作用
crest faulting 脊部斷層作用
deformation faulting 層內(nèi)斷層作用
disharmonic faulting 不一致斷裂作用
distributive faulting 分枝斷裂
ductile faulting 延性斷層作用
episode of faulting 斷裂作用幕
evidence of faulting 斷裂證據(jù)
extensional faulting 張性斷裂
faulting episode 斷裂幕
faulting plane 斷層面
faulting recurrence 斷層復活; 斷裂復活
faulting stress 斷裂應力

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例句與用法

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(qū)域構造解釋分析，論述了柏各莊地區(qū)的構造樣式，是中新生代渤海灣裂谷盆地的幕斷陷發(fā)育階段，同時由于盆地內(nèi)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(fā)育一系列ne ( nee )向，傾向nw或sw的正斷層。
The extending major fault has a strike of north - east , controlling the forming of depressions and evolution of sedimentation . the nature of the fault is normal in the early stage . later with the reformation of sliding effect , normal faults are still the main faults , and the plane distribution of the faults occurs sectionally
取得了一系列的研究成果：遼河灘海地區(qū)主要有三種構造樣式，即伸展構造樣式、走滑構造樣式及反轉構造樣式，其中，以伸展構造樣式為主，伸展主干斷裂走向以北東走向為主，控制凹陷形成和沉積演化，斷裂性質早期為正斷層，后期經(jīng)走滑作用改造，至今仍以正斷層形式出現(xiàn)，斷裂平面展布具有分段性。
Typical examples include the xidatan palaeo - seismic fracture zone , seismic fracture zone of the kunlun ms 8 . 1 earthquake occurred in november 14 , 2001 , the south hohxil palaeo - seismic fracture zone , seismic fracture zone of the bengcuo ms 8 . 0 earthquake occurred in 1951 and seismic fracture zones along normal fault in east of the nyainqentanglha mts . caused by jiuzila ms 7 . 5 earthquake occurred in 1952 and yangbajain ms 8 . 0 earthquake occurred in 1411
典型地震破裂包括西大灘古地震破裂、昆侖山南緣地震破裂、可可西里古地震破裂、崩錯地震破裂、谷露盆西地震破裂、羊八井當雄盆西地震破裂；地震破裂規(guī)模大，產(chǎn)狀穩(wěn)定，與地震鼓包、地震陡坎、地震凹陷有序組合，是地表構造變形的重要形式，屬內(nèi)動力成因地裂縫。
3 , logging curve comparison results show that in the west part of south region there is a grade 4 normal fault , and the separation is 4 - 6 meters . five microstructure types and 8 top and bottom composition patterns have been proposed . the relationship between microstructure and deposition facies was studied and the genesis relationship was confirmed , that is , top microstructure is mainly corresponding to nature levee , contrasting to that of the bottom microstructure
提出了五種微構造類型及八種頂?shù)孜嬙旖M合模式；并研究了微構造與沉積相的關系，發(fā)現(xiàn)它們之間存在一定的成因聯(lián)系，即頂面微構造中高點、鼻狀和斷鼻構造主要對應于邊灘微相，低點與溝槽微構造則主要對應于天然堤微相，而底面微構造正好與之相反。

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