fault n. 1.過失,過錯;罪過,責(zé)任。 2.缺點(diǎn),缺陷,瑕疵。 3.(獵狗的)失去嗅跡。 4.【電學(xué)】故障,誤差;漏電;【地質(zhì)學(xué);地理學(xué)】斷層。 5.【網(wǎng)球】發(fā)球出界;犯規(guī)。 Faults are thick where love is thin. 〔諺語〕一朝情義淡,樣樣不順眼。 fault detection 【機(jī)械工程】探傷。 The fault is his own. 這是他自己的錯。 a grave fault in a theory 理論上的重大缺陷。 a fault in the machine 機(jī)械故障。 image fault 【物理學(xué)】像差,影像失真。 numerical faults 數(shù)值誤差。 a fault on the right side 因禍得福。 be at fault 1. (獵犬追捕獵物等時(shí))失去嗅跡,躊躇不前;不知所措,正在為難。 2. 出毛病,有故障。 3. = in fault (My memory is at fault . 我想不起來了)。 find fault in 看出…缺點(diǎn)。 find fault with 找…的岔子。 have no fault to find with 無錯可尋。 hit off a fault (獵狗)聞出(曾一度錯失的)嗅跡。 in fault 有過錯,有責(zé)任 (Who is in fault 是誰的不是?)。 to a fault 過度,極端 (He is kind to a fault. 他過分老實(shí))。 whip a fault out of sb. 鞭打某人使之改過。 with all faults 不保證商品沒有缺點(diǎn)。 without fault 〔古語〕無誤,確實(shí)。 vi. 1.【地質(zhì)學(xué);地理學(xué)】產(chǎn)生斷層;有斷層余跡。 2.發(fā)球出界;犯規(guī)。 3.〔方言〕責(zé)備,挑剔。 4.〔古語〕犯錯誤,做錯。 vt. 1.找…的岔子,挑剔;〔方言〕責(zé)備。 2.【地質(zhì)學(xué);地理學(xué)】使產(chǎn)生斷層。 3.把…做錯。 He faulted my speech in two ways. 他認(rèn)為我的講話有兩點(diǎn)不妥。 fault one's performance 表演發(fā)生失誤。
Microstructures and ages of activity of the reverse faults along the southern margin of the junggar basin 準(zhǔn)噶爾盆地南緣斷裂帶顯微構(gòu)造特征與活動時(shí)代
Structural features and evolution of contemporaneous reversed faults in gas faulted depression in western qaidam basin 柴西地區(qū)尕斯斷陷同生逆斷裂構(gòu)造特征與形成演化
The most critical factors in evaluating and predicting such traps sealed by the reverse fault are the analysis of strike closure and the estimation of fault sealing 評價(jià)和預(yù)測此類圈閉的最關(guān)鍵因素是進(jìn)行走向閉合分析和斷層封閉性的評價(jià)。
Based on the contrast of the comparability , the paper concludes that the footwalls of reverse faults in the front of altun mountain may form effective hydrocarbon traps 通過對比分析兩者之間的相似性,認(rèn)為柴達(dá)木盆地阿爾金山前帶構(gòu)造深部發(fā)育的逆沖斷裂下盤也應(yīng)該具有形成油氣圈閉的條件。
The research show that the formation of the fault is earlier than these klippen , but it is also a revived reverse fault after the klippen took themselves places from relationship between the fault and klippen , and the esr age determination 據(jù)斷裂帶與飛來峰壓覆及切割關(guān)系和esr年齡,表明斷裂的形成應(yīng)早于飛來峰的就位,而飛來峰就位后斷裂又有過再次的逆沖活動。
The tectonic style inside the basin is characterized by occurrence of anticlines from the margins to center of the basin , with two limbs mostly starting from reverse faults , developing a tectonic pattern of two faults sandwiching an uplift 盆地內(nèi)部的構(gòu)造樣式以自盆地邊緣至中心以此形成背斜構(gòu)造為顯著特徵,背斜兩翼多發(fā)育逆斷層,構(gòu)成“兩斷夾一隆”的構(gòu)造格局。
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(diǎn),研究水庫地震的斷裂特點(diǎn),得出地應(yīng)力作用下的應(yīng)力強(qiáng)度因子、庫水作用下的應(yīng)力強(qiáng)度因子和滲壓作用下的應(yīng)力強(qiáng)度因子以及它們的應(yīng)力強(qiáng)度因子之合,并且合理的解釋了構(gòu)造型水庫地震的誘發(fā)機(jī)理。
Kongxi buried hill shows following features in the seismic profiles : the structures are asymmetric . there is flexural syncline on the east side and a monocline on the west side . asymmetric repetition of stratigraphic units is present in the drill wells and the dips of beds and faults are gentle . the permo - carboniferous system of both sides almost lie in the same slope and the events of cambrian or upper proterozoic are continuous from east to west . the phenomenas suggest that kongxi buried hill could be a thrust belt been traced which consists of reverse faults . the imbricate faults mainly effect pre - jurassic strata . there are obvious angular unconformity between jurassic - cretaceous system and paleozoic involved deformation of thrust . the thrust front in some place has cut off the beds of jurassic - cretaceous system . the structural style of the thrust structure changes along the strike of the kongxi buried hill 地震和鉆井資料揭露的孔西構(gòu)造帶前第三系潛山的地質(zhì)特征可以歸納為:構(gòu)造帶總體上不對稱構(gòu)造帶內(nèi)部有地層重復(fù)現(xiàn)象石炭二疊系地層的位置明顯高于兩側(cè)的同一地層的高度。用由34條向東傾斜的逆沖斷層組成的疊瓦扇構(gòu)造模式能夠比較合理地解釋上述地質(zhì)特征。該帶向東傾斜的逆沖疊瓦狀斷層組主要影響前侏羅系地層,侏羅白堊系與卷入逆沖構(gòu)造變形的古生界地層之間有明顯的角度不整合。
They are paleozoic ~ early mesozoic - fold deformation and the appearance of reversed fault ; mesozoic - the beginning of graben faulting - block period ; early cenozoic - the phase of broke - the forming of block hill ; late cenozoic - the phase of segging - the forming of buried hill . we mark off five kinds of buried hill belts . they include three different kinds of trap on the basis of the cause of trap formation 本次研究在重新認(rèn)識濟(jì)陽坳陷區(qū)域構(gòu)造背景的基礎(chǔ)上,將濟(jì)陽坳陷古生界潛山的形成過程分為四個階段,即古生代早中生代?穩(wěn)定沉降?隆升?輕微褶皺變形及逆斷層發(fā)育階段、中生代?初步斷陷階段?塊斷期、新生代早期?斷拗階段?塊斷潛山形成期以及新生代晚期?坳陷階段?潛山定型期。