滑脫構造 的英文怎麼說

中文拼音 [tuōgòuzào]
滑脫構造 英文
décollement structure
  • : Ⅰ形容詞1 (光滑; 滑溜) slippery; smooth 2 (油滑; 狡詐) cunning; crafty; slippery Ⅱ動詞(貼著物...
  • : Ⅰ動詞1 (脫落) cast; shed; drop; fall off 2 (取下; 除去) take off; strip; cast off 3 (脫離) ...
  • : 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. As a result, the weizhou - shigouyi detachment structure is bounded on the east and west by faults and occurs as a synclinorium comprising exotic sheeted rocks with simple deformation

    它在地震剖面上表現為:面以上的多層平行反射、不出現逆沖推覆前緣帶復雜變形成的雜亂反射;平面上形成與周鄰明顯的不協調性。
  2. On ceishui formation ' s bedding structure and decollement structure of lianyuan depression in central hunan province

    湘中漣源凹陷測水煤系順層滑脫構造研究
  3. Thermal deposits mainly formed during middle - late yanshanian age, related to extension structure, with main mineralization in qingfeng competent deformation zone, western shennongjia fault arch, northern huangling fault arch, xianfeng anticline of enshi platforman fold bundle

    熱液型鉛鋅礦床主要形成燕山中晚期,與拆離密切相關,礦化主要集中於青峰強變形帶、神農架斷穹西部、黃陵斷穹北部、恩施褶皺束咸豐背斜、長陽褶皺束走馬坪背斜中。
  4. The key studied areas are the paishanlou, daban, dayintaogou, wujiazi gold deposits. in terms of the study of regional structures, geophysics, and geochemistry, and necessary tectono - physical and numerical modeling, as well as studies of ore - forming and ore - controlling structures, the author holds that the detached - ductile sheari ng zone of the metamorphic core complex is the main ore - controlling structural system, and the regional mineralization is related with the regional ore - forming structural systems which are controlled by compounding of regional structural systems with different time and grade

    重點以排山樓、大板、大櫻桃溝、五家子等金礦礦田調查為基礎,以區域地質、地球物理、地球化學研究為背景,輔以成礦物理模型、數學模型,通過成礦、控礦研究,將本區金礦的成礦確認為變質核雜巖拆離剪切帶,並且是與區域成礦系統相聯系,在不同時期、不同級序、不同力學性質體系成分復合條件下成礦。
  5. The dislocation interfaces of early stage were controlled by the slide of the ne fold. the dominant dislocation interfaces, in the dam area, is the one of the second stage, which resulted from the slide of the lava layer and lagerkluftes from nw to se because of the affect of the majiaheba faultage ' s thrusting overriding to the dam area from nw to se. the dislocation interfaces of the third stage were the result of the overprint of the structure of ne to the one of nw

    早期階段形成的錯動帶受控于北東向縱彎褶皺的層間彎機制;第二階段形成的錯動帶在壩區佔主導地位,它們是由於北東向馬家河壩斷層由北西向南東的逆沖推覆影響壩區,並成壩區向南東緩傾的巖層沿原生面向南東動的結果;第三階段形成的錯動帶則是由於北西向疊加於早期北東向之上而致。
  6. From extension degree, differential lifting, sliding surface depth and modern seismic data analysis, it is concluded that the structural activity of liaohe basin moves from west to east, i, e., the rifting happens in the western depression first, it moves to the eastern depression and now it locates in bohai area

    從伸展量、差異升降、面深度及現代地震資料分析認為,遼河盆地運動從西向東運移,即裂谷作用最先在西部凹陷,后移至東部凹陷,現在位於渤海海域。
  7. Combined with geologic condition and infrastructure characteristics, balance three great structure profiles which trend sn with balance profile theory, then analyze the structure style, association form and each detachment further, and calculate 30 % shorten after the stratum deformation variant it turns out to be striking detachment in multiple tectonic levels and different structure deformation variant style in different stage, after the discussion of the structure style and relation between infrastructure and suprastructure

    結合地表地質情況和深層特徵,利用平衡剖面原理對三條地質剖面進行了平衡,通過平衡后的剖面更好地對剖面所反映出的樣式、組合形態及各個面進行分析,並且計算出變形后地層的變形縮短量為30左右。研究區內深淺層之間存在著顯著的多層次,且不同層次上變形樣式各不相同。
  8. A simple explanation of structure and coal controlling in ceshui coal - measures, zhadu mining area

    渣渡礦區測水煤系滑脫構造特徵及其控煤作用
  9. 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、多層次的順層滑脫構造、強烈發育的劈理等。
  10. Through the analysis of geological characters in huanglianken manganese ore district, such as ore potentiality, ore controlling structures, ore depositing structures, orebody characteristics, ore type and so on, the author concluded that sinian stratum is the " primary source bed ", detachment structure is the migrating channel of ore - forming materials, favorable concentration and hosting place

    通過對黃連坑錳礦區地層的含礦性、控礦及容礦、礦體特徵、礦石類型等地質特徵的論述,認為震旦系地層是「初始礦源層」 ,滑脫構造對成礦物質起遷移、富集及容礦作用。
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