破裂巖 的英文怎麼說

中文拼音 [lièyán]
破裂巖 英文
cataclasite
  • : Ⅰ動詞1 (完整的東西受到損傷) be broken; be damaged 2 (使損壞) break; break down; damage 3 (使...
  • : 裂動詞[方言] (東西的兩部分向兩旁分開) open
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • 破裂 : break; fracture; burst; split; rupture; crack
  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帶內形成碎程度最強達到碎的碎系列構造,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,斷在北東?南西向近水平擠壓作用下右行張扭性活動,斷帶兩主斷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,而斷體區也發育兩組典型的共軛剪節理,斷內形成初碎為主的構造;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,在基中,主斷層兩側圍出現微
  2. The cataclastic rocks appeared in the fault zone include structural lenticles, fault breccias, protocataclasite and cataclasite. the microscopical cataclastic deformation mechanisms involved are microcracking, frictional sliding and pressure - solution, but there might have had ductile deformation relating to dislocation sliding in feldspar and quartz of the plutons

    帶內碎系列構造主要是碎石(包括構造透鏡體和構造角礫) 、初碎和碎,顯微變形機制主要有作用、摩擦滑動和壓溶作用。
  3. Chunks of the overlying rock may break off and become a part of a sill.

    上復石的碎塊可能並成為床的一部分。
  4. The rock formations break with cracks into new positions.

    層產生縫而移位。
  5. Keywords : fractography, brittle material, failure mode, model rock

    關鍵詞:形學、脆性材料、模式、人工石。
  6. Study on fracture pattern of open surface - flaw in gabbro

    輝長中張開型表面模式研究
  7. The sounds of rocks breaking in the desert have been compared to gunfire.

    在沙漠地區的聲音常被誤會為槍聲。
  8. But at the present, because of chronic geomorphy disintegration, altitude and ascent of bank slope have been built down and palliated. especial rock mass mechanics condition has not been existent, so all kinds of rock mass fracturing deformation was stopped to developing and steady

    但目前因長期的地貌剝蝕作用,壩肩岸坡的高度及坡度均已大為降低減緩,特殊的體力學條件已不復存在,體內部的各類張變形亦停止發展,處于發展穩定階段。
  9. Experimental investigation in rock rupture with the co - operation between chinese and russian seismologists

    1999年度中俄合作實驗研究
  10. A sharp crack might remain fairly sharp in granite, but degenerate into a dull thud in sand.

    在花崗中尖銳的聲可以保留相當的強度,而在砂中則易變成低沉的轟響。
  11. According to the stress wave theory on explosive exploding propagating in the rock, it builds up mathematical model of fractural ranges in the rock, and carry out actual calculation and analysis on fractural range of bench shooting in deep - hole. as a result of calculation, the lateral and bottom fractural range are about 1. 9m

    根據炸藥爆炸在石中傳播的應力波理論,建立石爆范圍數學模型,並對深孔梯段爆范圍進行了實行計算分析,計算結果為:混裝乳化炸藥石深孔梯段爆側向底部范圍為1 . 9m 。
  12. It is coupling action between seepage and stress makes the failure mechanism of rock very complex. the investigations on this problem have pervasive theoretical meaning and practical value

    滲流與應力耦合作用使得石的機制十分復雜,這一問題的研究具有更普遍的理論意義和更接近實際的應用價值。
  13. Centered on the investigation on the evolvement of permeability as well as the coupling action between seepage and stress, the following work is carried out : 1. a further examination is given to classical biot seepage theory to discover the basic assumption to form the coupling seepage equation, and discuss the variety of coupling equations between seepage and stress and their adaptabilities. the physical meanings, adaptability, testing method of seepage parameters used in equation of continuum are analyzed based on the experimental investigations on complete relationship between stress, strain and permeability of rock and engineering test on permeability of rock at different depth

    本文圍繞過程中滲透性的演化規律及其滲流-應力耦合作用機理這一課題,開展以下方面的研究工作: 1 .對經典biot滲流力學做了進一步的考察,揭示建立耦合滲流方程的主要假設,討論了各種滲流與應力耦合方程及數學模型的適用條件,通過石應力應變-滲透率全過程實驗研究和不同深度體滲透率工程試驗研究,分析了連續介質模型耦合滲流方程參數的物理意義、適用性、測試方法。
  14. In numerical simulation, the elastic zone is only considered and the effect of blasting waves on the rock medium, after attenuating through crushing zone and ruptured zone, becomes an input load

    數值模擬僅考慮彈性區域,爆炸波對石介質的作用經粉碎區、區衰減后成為輸入荷載。
  15. Field investigations found that epigenetic reworking deformation fracture include 3 types, named normal relief fracture, fracture filled mud and epigenetic reworking of disturbed belts. and epigenetic reworking of rock mass structural also includes gradual deformation of the blocks that are made up of different attitudes structural planes besides normal relief. through field geological investigations, the features of rock mass structural planes are generalized, especially development laws of interlayer shearing belts, instrastratal shearing belts, faults and base crack

    在已有研究成果基礎上,總結了壩區玄武相特徵和構造應力場對體結構的影響;通過現場調查,總結了3種類型淺表生變形,即正常卸荷型、鬆弛夾泥型和緩傾角錯動帶表生改造;通過野外地質調查,總結了層間錯動帶、層內錯動帶、斷層和基體隙的發育規律。
  16. The fractal is a geometrical figure with self - similar symmetry, and it is an important tool for characterizing irregular structures in nature that are self - similar on certain length scales. for example, the koch curves can be viewed as a mathematical model for coastlines, percolation model can be used to mimic mixture of mental and insulator, self - avoiding walks can serve as a model for linear polymers, and rock fracture mode can stimulate the process of brittle fracture of rock, and so on

    分形是具有自相似對稱性的幾何圖形,可用來模擬自然界中在一定尺度范圍內具有自相似對稱性的不規則結構,如koch曲線可用來模擬海岸線,滲流模型可模擬金屬絕緣體混合物,自迴避無規行走模型可模擬線性聚合物,模型可模擬真實體的脆性等。
  17. The thermal cracking threshold of fine sandstone is determined primarily

    實驗初步確定了細砂的熱閾值及其熱規律。
  18. Research on transition law between eme and energy during deformation and fracture of coal or rock under compression

    受壓煤過程電磁輻射與能量轉化規律研究
  19. Numerical analysis on displacement law of underground broken rock mass

    地下工程破裂巖體位移規律數值分析
  20. Area of faulted rock

    破裂巖石區
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