活動斷裂 的英文怎麼說

中文拼音 [huódòngduànliè]
活動斷裂 英文
active rift
  • 活 : Ⅰ動詞1 （生存; 有生命） live 2 [書面語]（救活） save （the life of a person）:活人無算 （of a goo...
  • 斷 : Ⅰ動詞1 （分成段） break; snap 2 （斷絕;隔斷） break off; cut off; stop 3 （戒除） give up; abstai...
  • 裂 : 裂動詞[方言] （東西的兩部分向兩旁分開） open
  • 活動 : 1 （運動） move about; exercise 2 （動搖） shaky; unsteady 3 （不固定） movable; mobile; flexible...
  • 斷裂 : break; disrupt; flying off; fracture; fragmentation; out break; rift;crack;bursting;rupture;rendi...
  1. The fault controlled the magmatism and metallization relevant to the contact zone, and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene. the fault zone deformed right - laterally under ne - sw striking transtention, and new joints zone was produced at the end of the two main faults because of local stress concentration. the fault produced inchoative cataclastic rocks, and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks, which was during the himalayan movement

    其後的繼承性活動在斷裂帶內形成碎裂程度最強達到碎裂巖的碎裂巖系列構造巖，變形帶兩側發育兩組典型的共軛剪節理；第二次在晚白堊世?始新世，斷裂在北東?南西向近水平擠壓作用下右行張扭性活動，斷裂帶兩主斷裂在斜列重疊的端部由於局部應力集中進一步擴展形成節理帶，而斷裂在巖體區也發育兩組典型的共軛剪節理，斷裂內形成初碎裂巖為主的構造巖；第三次是喜山期以西側抬升、東側下降的強烈升降為主的活動，在基巖中，主斷層兩側圍巖出現微破裂。
  2. 4 ) analyses boundary faults of the cenozoic longmenshan foreland basin, and thinks the basin boundary faults, being active fault, are thrust and dextral strike - slip. so the longmenshan foreland basin is dextral strike - slip foreland basin

    4 ）通過對新生代龍門山前陸盆地邊界斷裂的考察分析，認為盆地邊界斷裂具逆沖推覆及右旋走滑作用特點，為活動斷裂。
  3. The paper analyzes the occurrence regularity of rock burst of about 263 times in laohutai mine field by database, the osculating relations of rock burst and active faults were summarized

    摘要應用數據庫對老虎臺井田其發生的263次沖擊地壓之統計分析表明，巖體動力現象與活動斷裂有密切關系。
  4. Incorporated with the surveying of geo - stress and rock stress analysis, the feature of rock stress can be found and the strata behaviors induced by coal mining can be predicted, which will supply geology information for safe mining

    地質動力區劃方法以板塊構造理論為基礎，以區域構造形式為主要研究對家，進行活動斷裂的劃分，確定區域構造形式。
  5. With topographic map and other methods, some class i v active faults that run through laohutai mine field in modern stress environment are found out by means of geodynamic zoning

    通過逐級使用地形測量圖並結合其他方法查明了井田i v級活動斷裂，由各級斷裂所分割的斷塊結構展現出了井田現今構造運動的結果。
  6. Though there are large fault both in danjiang segment and hanjiang segment, yet the seismic activity is very different in the two areas for different geological and hydrological conditions

    雖然丹庫和漢庫均有大的活動斷裂穿過，但由於二者的地質和水文條件不盡相同，導致蓄水后的地震活動差別很大。
  7. The cover faults in daqing region are mainly developed in formation of huoshiling member late jurassic and its cover formations. according to their formation period, activity characteristics and penetrating relationship, four types of faults were divided, that is fault - depression faults, depression faults, inverted - strike - slip faults and inverted - extension faults ; according to the activity history of the faults, five types of faults were divided, that is long - term active faults, early active faults, early - medium - term active faults, medium - term active faults and terminal active faults

    大慶地區內發育在晚侏羅世火石嶺組及其以上的沉積蓋層中的蓋層斷裂，依斷層形成時期、活動特徵及切割層位可將蓋層斷層細分為四種類型，即斷陷期斷裂、坳陷期斷裂、反轉走滑斷裂和反轉張性斷層；按其活動歷史可以分為五種類型：即長期活動斷層、早期活動斷層、早-中期活動斷層、中期活動斷層和晚期活動斷層。
  8. All those faults in the yellow river delta, such as chengzikou fault, shengbei fault, gubei fault, yina fault, chengzhong fault, wudi - yidu fault, gangrao - qihe fault and so on, had been researched closely and synthetically, it was found that the shengbei fault had still been an activity one since quaternary system period, thus, all those views about the inactivity of the shengbei fault was corrected too

    系統研究了埕子口斷裂、勝北斷裂、孤北斷裂、義南斷裂、埕中斷裂、無棣?益都斷裂、廣饒?齊河斷裂、東營斷裂等區域主要斷裂的活動特徵。研究發現，勝北斷裂為一條第四紀以來仍有活動的斷裂，糾正了以往認為勝北斷裂為不活動斷裂的看法。
  9. Analyzing collected dada, the conclusion is : northwestern trending right lateral strike slip faults are predominant, other active structures include northeastern trending left lateral strike slip faults and west - east trending folds

    對上述資料分析認為：天山山間主要以北西向的右行走滑活動斷裂為主，另有一些北東向的左行走滑活動斷裂和東西向的活動褶皺。
  10. Remote sensing studies on active faults in the western south - north water transfer project area in china

    南水北調西線工程區活動斷裂構造遙感研究
  11. Under the effect of regional tectonics, there develop many raws drape anticline and active fault in the front of mountain, and they have especial motion fashion

    由於受區域構造長期作用的影響，在北天山山前地區逐步發育形成了多排褶皺背斜及活動斷裂，且運動方式具有獨特性。
  12. This paper discusses the features of active fault through data analysis by using short water level across the fault to measure and set up the monitor net of south branch of the yamalike fault deformation

    摘要利用跨斷層短水準測量，建立了跨雅瑪里克斷裂南支斷層形變監測網，通過資料分析得出該斷裂帶斷層活動特徵，確定了雅瑪里克斷裂為全新世早期活動斷裂。
  13. Using various geophysical and seismogeological data available, the present paper has probed into relationship of characteristics of gravity and magnetic field, crustal structure and active faults to earthquake and summed up spatial distribution of epicenters in crustal media

    摘要本文利用現有各種地球物理資料、地震地質資料，探討了重磁場特徵、地殼結構、活動斷裂與地震的關系，進而總結出地震震中在地殼介質中的空間分佈規律。
  14. Shallow structure earthquakes are always concurrent with fault activities. evidence testifies that earthquakes often occurred densely near the place where the faults exist. there is an intimate relationship between earthquakes and active faults. so in analyzing the danger coefficient of earthquakes, it is very important to ascertain the locations and scale of earthquakes that will occur possibly in the future

    淺源地震總是伴隨斷裂活動而發生的，已有資料證實地震確實是在已有斷裂面附近密集發生，地震與地表現有的活動斷裂帶有密切的關系。為進行地震危險性分析，確定未來可能發生地震的地段和強度是極為重要的。
  15. It is possible for the terminal activity faults to penetrate to the quaternary, but their scale is generally small and the penetrating distance is short, therefore, they can not induce earthquakes on a large scale. the remote sense images of last thirty years in daqing region show that the linear tectonics have not changed remarkbly, in the meantime, the earthquake timing figure shows that the probability of the faults inducing earthquakes, which ms is no less than 5, is little, though some terminal active faults have penetrated to the quaternary

    晚期活動斷裂有可能斷至第四系，但規模小，延伸的距離短，不會引發大規模地震，遙感解譯分析表明， 30多年來衛星遙感影像顯示的大型線性構造並無明顯變化；另外結合大慶地區地震時序圖認為，晚期活動斷裂即使斷至第四系，其活動引發5級以上地震的可能性也極小。
  16. The distribution of hypocenters shows that there are two major seismic active belts in the northwestern beijing

    震源位置分佈表明，北京西北地區存在兩條主要的地震活動斷裂帶。
  17. These phenomena indicate that heavy rainfall is a kind of trigger for the occurrence of earthquakes which occur along the fractured zones of the active faults.

    這些現象表明，大雨是發生於活動斷層斷裂區的那些地震的一種觸發因素。
  18. In this paper, relation between the dynamic evolution feature of gravity field and strong seismicity is studied, the result shows that, regional gravity field variation enjoys inhomogeneity of spatialand temporal distribution and gravity change in different regions

    摘要通過研究南北地震帶及青藏塊體東部地區多年來的重力場動態演化特徵及其與強震活動的關系，發現區域重力場變化既具有時空分佈的不均勻性和重力變化分區現象，同時又具有與活動斷裂構造密切相關並與地震孕育發展有著內在聯系的特徵。
  19. Based on fuzzy mathematics authors have developed a fuzzy comprehensive evaluation model of earth crust stability, then divided the studied region into eight a - reas with different stability of earth crust on the basis of analysing the structure of earth crust, seismic characteristics, active faults and recent tectonic stress field

    本文以模糊數學為基礎，建立地殼穩定性模糊綜合評價模式；然後按地殼結構、地震、活動斷裂和現代構造應力場等4個方面的特徵把研究區劃分為8個不同穩定性的區域。
  20. The first belt stretches from qinghe, wenquan to the nw direction and the second extends from nankou, changping to the ene direction

    一條從清河、溫泉一帶向北西方向伸展，到懷來縣以北的黃土窯一帶；另一條是自南口、昌平一帶向北東東向伸展的活動斷裂帶。
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