normal faulting造句
例句與造句
- Analysis on distribution features of gas outburst from two walls of normal fault and geological origin
正斷層兩盤的瓦斯突出分布特征及其地質成因淺析 - The fault faults from basemet to quaternary system , and has the feature of contemporaneous and normal fault
該斷裂自基底一直斷到第四系，具同生正斷特征。 - The focal mechanism is mainly left - lateral strike - slip , with a very small normal fault slip component
這次地震的震源機制基本上是左旋走滑，帶有微小的正斷層滑動分量。 - The extensional and transtentional structure existed in huabei belongs to vent fault , fracture is mainly stepwise normal fault , whose preservation condition is not good
華北地區(qū)多為張性，張扭性構造，屬于排氣斷層，形成的斷裂多為階梯狀，以正斷層為主，保存條件欠佳。 - Several normal faults within the hainan fault zone constitute a fault - step zone and form a narrow and steep zone , which controlled the development and distribution of depositional systems in this area
研究認為，海南斷裂帶的幾個北掉斷層構成斷階帶，形成湖盆邊緣陡且窄的地貌特點，控制了該區(qū)沉積體系的展布規(guī)律。 - It's difficult to find normal faulting in a sentence. 用normal faulting造句挺難的
- According to the relative membership degree of normal fault mode to needing checking mode , fuzzy optimum selecting theory is application to transformer fault diagnosis . it may judge fault more explicit than fuzzy even weight model
本文提出的模糊優(yōu)選法進行變壓器故障診斷，是根據標準故障模式對待檢模式相似的相對隸屬度的大小來判斷故障，比模糊平均加權模型對故障的判別更為清晰。 - The extensional activities of hefei basin occurred in the period between late cretaceous and paleogene . as a result , the extensional normal faults were took place along the pre - existing nearly ew faults and the tan - lu fault zone . the deposition of half - graben was formed
合肥盆地的伸展活動發(fā)生于晚白堊世至早第三紀，伸展活動是疊加在前兩期走滑構造之上，形成了以半地塹式楔形為主的沉積。 - The thesis sets up a diagnose knowledge base , which considers the normal fault of hydroelectric unit and the characteristics of the no . 3 unit of guizhou dongfeng hydropower plant . with this condition , the system can diagnose the elementary fault of the unit to assist in operation and servicing
同時針對水輪發(fā)電機組的一般故障及東風水力發(fā)電廠3 #機組的特性,總結了一套故障診斷數據庫,在此基礎上對機組進行初步的故障診斷以輔助電廠進行檢修決策 - 2 . tazhong ancient uplift originated from normal fault in paleozoic , hydrocarbon formed in ordovician period , structure reverse made tazhong uplift form from the middle ordovician period to the late ordovician period , and it provided geologic background for the deposit of silurian - devonian stratum . tazhong uplift formed at the end devonian , ancient reservoir was destroyed and asphaltum sandstone formed , structure deformation more destroyed ancient reservoir in early permian , after then the major of structure deformation is regulation
塔中隆起源于早古生代拉張背景下的正斷層，寒武-奧陶紀為其烴源巖形成的重要時期；早奧陶世末-晚奧陶世末的構造反轉是塔中隆起的主要形成期，同時也為志留系形成地層及復合圈閉提供了古地理背景；志留?泥盆紀塔里木盆地南北緣均轉為活動大陸邊緣，形成了大量的斷裂和不整合；泥盆紀末塔中鼻狀隆起基本定型，古油藏遭受破壞，形成了瀝青砂巖；早二疊世晚期的構造變形使古油藏遭受進一步的破壞；二疊紀后構造變動主要以調節(jié)為主。 - Analyzing the propagation behaviors for open and close crack , the author gain that normal fault is more dangerous to earthquake than reverse fault and glide fault . 3 . appling fracture mechanics to discuss reservoir - induce earthquake mechanism , the author observes the characteristic of surface crack and gains the stress intensity factor induced by the pressure of rock , water and osmosis
針對庫區(qū)斷層為表面裂紋這一特點，研究水庫地震的斷裂特點，得出地應力作用下的應力強度因子、庫水作用下的應力強度因子和滲壓作用下的應力強度因子以及它們的應力強度因子之合，并且合理的解釋了構造型水庫地震的誘發(fā)機理。 - 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，后期經走滑作用改造，至今仍以正斷層形式出現，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底微構造組合模式；并研究了微構造與沉積相的關系，發(fā)現它們之間存在一定的成因聯系，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。