斷層的 的英文怎麼說
中文拼音 [duàncéngde]
斷層的
英文
faulted-
For a long time researchers believed that etna ' s position at the crossroads of these faults was the explanation for its volcanism
長久以來，研究人員相信埃特納火山活動的原因，正是因為它位處這些斷層的交會處。Combined with the complexity of 3d fem analysis of seepage field of underground project, the simulation of faultage was comprehensively discussed
摘要結合地下工程滲流場三維有限元分析復雜性的實際，對斷層的處理進行積極探討。The results of 2 - d resistivity inversion of the yishui - tangtou and the liujazhuang faults indicate that electrical structures on both sides of the fault zone present obvious difference, the resistivity of the hanging wall is low and partially high, while that of the foot wall is high, and the faults are high - obliquity faults
沂水湯頭斷裂、劉家莊斷裂的二維電阻率反演結果表明，斷裂帶兩側的電性結構呈現出整體性的差異，正斷層的上盤為低阻區和局部高、低阻擾動區；而斷層下盤多為均勻的高阻區；斷層為高角度斷層。Gouge or infilling is the material between two faces of a structural discontinuity such as a fault.
斷層泥或充填物是指一個不連續面（如斷層）的兩個表面之間的物質。The study area is composed of sandstone & conglomerate reservoir of alluvial fan & fan delta, which belong to sha3 lower member and sha4 upper member of lower tertiary of yong " an town oilfield in dongying depression. the target stataum develops in the hanging wall of the synsedimentary fault in the scarp zone of dongying depression. the frequently intense movements result in the variation of sandstone and conglomerate reservoir and the evolution of the time and space of sha3 lower member and sha4 upper member in yong " an town oilfield
研究區是東營凹陷永安鎮油田沙三下段、沙四上段的沖積扇和扇三角洲砂礫巖體，目的層發育在東營凹陷陡坡帶同生斷層的下降盤，因斷層多期強烈活動，導致永安鎮油田沙三下段、沙四上段的砂礫巖體成因類型多，時空演化變化大，在扇根一帶小層對比難度大，給油田開發帶來很大的難題，在這種背景下進行流動單元研究難度更大。Infrared imagery, being sensitive to differential heat capacity of the ground, has proved useful in mapping faults which behave as aquicludes.
紅外成像對于地面不同熱容量是敏感的，對于作為阻水的斷層的填圖證明是有效的。However, it is still often to draw the thrust isoline graph manually during the data processing
但是，在實際工作中，進行數據處理和制圖時，半手工繪制帶逆斷層的等值線圖的現象還普遍存在。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域構造解釋分析，論述了柏各莊地區的構造樣式，是中新生代渤海灣裂谷盆地的幕斷陷發育階段，同時由於盆地內凸起邊界?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，發育一系列ne （ nee ）向，傾向nw或sw的正斷層。Explanation method and application of 3d seism to explore small - fault
三維地震勘探小斷層的解釋方法及應用By using color doppler ultrasonography and blood cell counter, the recovery of blood cell counts and hypersplenism in 2 patients, undergoing orthotopic liver transplantation, who were diagnosed having hepatocirrhosis with portal vein hypertension and congestive splenomegaly before the transplantation were clinically observed
採用全血細胞計數監測和彩色多普勒超聲斷層的方法對兩例因肝硬化合併門脈高壓脾功能亢進而行同種異體原位肝移植術的患者進行了臨床觀察。The initiation and maintenance of faults will depend upon the contemporary system of tectonic stresses in the earth's crust.
斷層的發生和保持取決于地殼的構造應力的同代體系。Based on the simple describle of the basic principle of anti - disturbance high - resolution shallow seismic exploration, all the sources, the properties of digital seismic instruments, the receive method and conditions, the observation system, and the data processing and interpretation of the urban active fault detecting are discussed emphasizedly
在簡述抗干擾高解析度淺層地震勘探基本原理的基礎上，重點論述了城市活斷層的抗干擾高解析度淺層地震勘探的震源激發、數字地震儀性能、接收方式與接收條件、觀測系統以及數據處理與資料解釋等。After recombination of faults according to new penetrated breakpoints data, the number, extension length and trend of some faults controlled by original patterns changed
根據新鉆遇中斷點資料對斷層進行重新組合，原井網條件下控制的部分斷層的數量、延伸長度、走向發生了變化。The effects of fault activity and earthquake on vertical migration of hydrocarbons are further discussed
兩者通常是伴生的，後者更有利於油氣沿斷層的垂向運移，規模也較大，而前者差些。The fault at the east boundary of tangyuan fault basin is a basin - controlling fault, and the faults at both the east and the west boundaries of fangzheng fault basin are also a basin - controlling fault, with the west boundary fault at fangzheng being the major one
斷層的生長指數分析表明，依舒地塹內部的北西向斷裂與邊界斷裂的活動具有一致的規律性，都起到協調邊界斷裂演化發展的作用。Through the parametric studies, the inelastic behavior of a buried pipeline differs so much from that of the beam or ca
由於實際中針對每一個通過斷層的管子做三維的殼模型有限元分折是頗費時間的，為了Being primarily controlled by northwest faults, cretaceous of jiyang depression contained several isolated basins, and lake levels of these isolated basins were instable, but on the whole, shore and shallow lake sub - facies is in the majority
北西向斷層的活動對沉積起到主要的控製作用，在其控制下，白堊紀濟陽坳陷為一相互分割的山間盆地，湖盆范圍時大時小，湖水深度不斷變化，總體湖水較淺，主要發育濱淺湖亞相。Together with the localization of seismicity on faults, this leads to the conclusion that a fraction of the crust is susceptible to rupture, while presently being quiescient
與斷層的局部地震活動性一起考慮，可以得出如下結論地殼的一部分，在目前處于靜止狀態條件，它實際處於一種易受影響導致破裂的敏感狀態。According to the re - analyses on pollen assemblages and archeological evidences in the site and related documents, this paper reconstructs the sequence of fossil pollen - pollen - vegetation - paleoclimate during the prehistoric period, emphatically discussing environment changes, the space - time distributed law on archaeological sites, the origin of culture fault and formation mechanism
本文根據孢粉學和考古學證據，結合相關文獻資料，從古地理學、考古學、歷史學等綜合研究的角度，重建史前時期化石花粉? ?孢粉植被? ?古氣候環境的演變序列，著重探討太湖流域新石器時期的環境變遷與古文化遺址的時空分佈規律、文化斷層的成因及其機制。Tertiary structures are developed in mesozoic - palaeozoic tectonic settings, the general framework is faulted depression faulted in the north and onlapped on the south and arch bounded by faults. they are controlled and affected by three sets of large successive - active faults ( nw, ne and nee strike ), they are successive and segmented, with multiples types and zoning distribution
第三系的構造是在中、古生界構造的背景上發育起來的，它以北斷南超的箕狀斷陷和斷層為界的凸起為總的構造格架，受北西、北東和北東東向三組繼承性活動大斷層的控制和影響，構造具有繼承性和分割性、類型具有多樣性、分佈具有分層分帶性。分享友人