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fault displacement中文是什么意思

  • 斷層位移
  • 斷層移距

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  • 例句與用法
  • The fault displacement may be vertical, horizontal, or any combination of these .
    斷層位移可能是垂直的、平行的、或者是兩者的綜合。
  • For each parametric study case , the fault displacement ( a ) is up to 7 meters
    當(dāng)管子與斷層的交角大于90度時(shí),壓縮應(yīng)變主導(dǎo)著管子的變形。
  • From the results of constraining fault displacement and correlation between the sediments in these trenches , we found a complete paleoseismic activity history on the fault segment during that period of time
    由斷層位移量限定法和多探槽校驗(yàn)法判定,這一時(shí)期該斷裂的古地震活動(dòng)歷史是完整的。
  • The source faults control oil gas accumulation and distribution in the research area : 1 ) the nearer to the source faults is , the higher the oil - gas accumulation degree is ; 2 ) the smaller fault displacement of the source fault is , the higher oil gas output near the source fault is
    源斷裂控制著貝爾凹陷布達(dá)特群油氣成藏與分布,主要表現(xiàn)在距源斷裂越近油氣富集程度越高及斷距越小的源斷裂附近油氣產(chǎn)量越高2個(gè)方面。
  • By means of kiba formation , k . ibt " and kibt2 segments analysis on the equivalent time stratigraphic framework , subtle traps will be predicted on stratigraphic traps and lithological traps . the results from the research indicated that : ( 1 ) this paper further indicates the control significance of southern boundary fault displacement component , which downthrown side forms syncline or anticline , and points out that 4 anticlines in south are adjustment zone and are the entering lake position of ancient river
    本論文的主要認(rèn)識(shí)和結(jié)論如下: ( 1 )進(jìn)一步認(rèn)識(shí)南緣邊界斷層位移量對(duì)下降盤形成次凹或橫向突起的控制意義,認(rèn)出南緣的4個(gè)突起是調(diào)節(jié)帶之所在,也是古河流入湖處。這種格局導(dǎo)致凹陷強(qiáng)烈分割,并以橫向搬運(yùn)為主。
  • The main conclusions are as follows . cross - fault displacement observation can directly reflect the recent activities of the major faults in the region . present fault movement and earthquake activity have a temporal correspondence with each other , they all show alternately quiet and active periods . the intensity of fault movement is a manifestation of the strength of regional principal compressional stress , it also indicates the strength of an earthquake in preparation
    認(rèn)為: 1 )跨斷層位移觀測(cè)資料能夠直接反映區(qū)內(nèi)主要斷層的最新活動(dòng)情況; 2 )斷層現(xiàn)今活動(dòng)與地震活動(dòng)在時(shí)間序列上相互對(duì)應(yīng),均有活躍期與平靜期相互交替出現(xiàn)的活動(dòng)特徵; 3 )斷層活動(dòng)強(qiáng)弱是區(qū)域主壓應(yīng)力強(qiáng)弱的表現(xiàn),亦是孕震強(qiáng)度的標(biāo)志。
  • The regularity of accumulation distribution is ascertained and directs the exploration orientation . the main results obtained in this paper are : 1 . the analyses of hydrocarbon - bearing rock , reservoir , caprock and oil & gas reservoir indicate the source of oil & gas , the space for reservoir , requirement for preservation , reservoir type and its basic characters . 2 . it is realized by the analyses of sealing up capability of caprock and faults , and fault ' slatter stability from microcosmic and macroscopic that the wide - spread regional caprock of nm t prevented oil & gas of neogene from diffusing fault movement in neogene less violated and fault displacement decreased , which are advantageous for the preservation of oil & gas reservoir . and latter structure movement usually formed the accunulation of oil & gas in neogene . 3 . the research of history of hydrocarbon generation and expulsion of main hydrocarbon - bearing rock in qikou depression reveals the threshold depth and the fime of hydrocarbon generation and expulsion
    項(xiàng)目研究取得了如下認(rèn)識(shí): 1 、對(duì)烴源巖、儲(chǔ)集層、蓋層及油氣藏展開分析,明確了歧口凹陷上第三系油氣藏的油氣來源、儲(chǔ)集場(chǎng)所、保存條件和油氣藏類型及其基本特征; 2 、從微觀和宏觀上對(duì)蓋層的封蓋能力以及斷層封堵和后期穩(wěn)定性進(jìn)行分析,認(rèn)識(shí)到明下段區(qū)域蓋層的廣泛分布阻止了上第三系油氣藏的油氣逸散,同時(shí)上第三系斷層活動(dòng)減弱,斷距較小,對(duì)油氣藏的保存較為有利。
  • Based on the characteristics of the quaternary tectonic activities of babaoshan - huangzhuang - gaoliying fault and the regional principal compressional stress direction and regional tectonic activities derived from the recent cross - fault displacement observation data in the capital area , we have analyzed the relationship between the fault movements at 7 cross - fault observation sites on the babaoshan - huangzhuang - gaoliying fault and the seismicity , conclude that the capital and adjacent area is soon to enter upon the next active period of earthquakes
    摘要根據(jù)八寶山黃莊高麗營(yíng)斷裂第四紀(jì)地質(zhì)構(gòu)造活動(dòng)特徵和利用首都圈地區(qū)跨斷層位移最新的觀測(cè)資料求得的北京地區(qū)區(qū)域主壓應(yīng)力方向和區(qū)域構(gòu)造活動(dòng)特徵,分析了八寶山黃莊高麗營(yíng)斷裂上7處跨斷層位移測(cè)點(diǎn)的斷層活動(dòng)與地震活動(dòng)的關(guān)系,得出了首都圈及鄰近地區(qū)即將進(jìn)入下一個(gè)地震活躍期的結(jié)論。
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