劈理構造 的英文怎麼說

中文拼音 [gòuzào]
劈理構造 英文
cleavage structure
  • : 劈動詞1 (分開; 分) divide; split 2 (分裂; 使離開原物體) break off; strip off 3 (腿或手指等過...
  • : Ⅰ名詞1 (物質組織的條紋) texture; grain (in wood skin etc ) 2 (道理;事理) reason; logic; tru...
  • : Ⅰ動詞1 (構造; 組合) construct; form; compose 2 (結成) fabricate; make up 3 (建造; 架屋) bui...
  • : Ⅰ動詞1 (做; 製作) make; build; create; produce 2 (假編) cook up; fabricate; concoct 3 [書面語...
  • 構造 : structure; construction; constructional detail; tectonic; structural; makeup; anatomy; constituti...
  1. Stability of rock slopes is generally controlled by the structure of rock masses, especially the soft structure surfaces. analysis of rock mass structures is a key to establish geological models and numerical simulation and a foundation to assess the stability of rock slopes. the weak structure surfaces are mainly bedding planes, faults, joints, schistosity plane and contact zones of intrusive bodies. since they are different in genesis and scale, the rock masses are different in features and mechanical intensities. based on the combination of rock structure bodies, 15 basic modes of deformation and failure of rock slope are systematically summarized. the deformation and failure of rock masses actually result from the recombination and rearrangement of these rock bodies. there are 11 types of rock mass structures and various deformation and failure of bank slopes are present in the reservoir area of the three gorge project

    巖體結,特別是軟弱結面對基巖斜坡變形與破壞具有顯著的控製作用,巖體結模式分析是建立斜坡地質模型和數學模型的關鍵和評價斜坡穩定性的基礎。巖層層面斷裂裂隙片以及侵入體和圍巖的接觸帶等是控制基巖斜坡穩定的軟弱結面,這些成因不同大小不一的結面將巖體分割成性質各異力學強度不均的各種巖體結體,成了15種基巖斜坡變形破壞的巖體結基本模式。不同結體的重新組合與排列是斜坡失穩的內在原因。
  2. After researching the loads on dangerous rock synthetically, the author points out the development and collapse mechanism of dangerous rock : the geology foundations that forms dangerous rock are the constructional surfaces such as tectonic fracture 、 relief fissure, soft interlayer etc. the developing of dangerous rock is due to release of in - situ stress in rock 、 aeolation 、 water erosion and root flerry. the main loads leading to collapse of dangerous rock are gravity, water pressure and earthquake force

    在綜合研究危巖上的各種作用之後,本文提出了危巖的形成和破壞機:硬質巖體中裂隙、卸荷裂隙、及各種軟弱夾層,結面的的存在是危巖形成的地質基礎;地應力卸荷、風化、流水侵蝕、植物根是危巖發育的主要作用;重力、水壓力、地震力是危巖崩塌的主要荷載。
  3. According to the spread of nappe and relation between the nappe and depression, oblique - thrust fault zone was divided into three parts in this paper : sertengshan, lvliangshan and xitieshan. ( 3 ) according to macroscopic characteristics of fault zone, cleavage characters of fault zone, drag folds, the reverse " s " fold in the footwall, positive flower structures and small left strike - slip fault, the kinematics characters of fault zone of sertengshan - xitieshan are concluded : thrusting in section, left - slip fault in plane and the strike - slip displacement increasing from the west to the east

    ( 3 )根據斷裂斷裂帶的宏觀特徵、斷層帶特徵、斷裂帶附近的牽引褶皺和斷層下盤的平面反「 s 」型褶皺以及斷層上盤剖面正花狀和平面左行小型平移斷層,認為賽什騰-錫鐵山斷裂帶運動學主要表現為剖面上的逆沖、平面上的左行走滑特點,並且走滑量具有自西向東增大之勢。
  4. The characteristics and genesis of cleavage in daqingshan thrust

    大青山逆沖推覆帶中特徵及其成因
  5. The anatomy of small - scale to meso - scale deformational structures have resulted in the reconstruction of the structural framework of the yanbian group. the statistical analyses of the fold hinge and cleavages developed in the yanbian group suggest the trend of the first stage penetrating structures of the yanbian group is een - wws. 2

    基於對鹽邊群中、小尺度變形進行解析,建立了區域格架,通過對褶皺樞紐和的分析,提出鹽邊群第一期透入性變形的走向為北東東?南西西向。
  6. With the field work and plenty of references, the influence to the generation and development of the deformed slopes in badong formation is discussed in this paper

    成三峽庫區發育深厚層鬆散斜坡的主要包括褶皺、多層次的順層滑脫、強烈發育的等。
分享友人