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reversed fault中文是什么意思

  • 逆沖斷層
  • 逆斷層

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  • 例句與用法
  • 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。
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