造山不整合 的英文怎麼說

中文拼音 [zàoshānzhěng]
造山不整合 英文
orogenic unconformity
  • : Ⅰ動詞1 (做; 製作) make; build; create; produce 2 (假編) cook up; fabricate; concoct 3 [書面語...
  • : 名詞1 (地面形成的高聳的部分) hill; mountain 2 (形狀像山的東西) anything resembling a mountain...
  • : 名詞[書面語] (剁物所用的木墩) a block of wood
  • : Ⅰ形容詞1 (全部在內; 完整) whole; all; complete 2 (整齊) neat; tidy; orderly Ⅱ動詞1 (整理; 整...
  • : 合量詞(容量單位) ge, a unit of dry measure for grain (=1 decilitre)
  • 整合 : commensuration
  1. Kongxi buried hill shows following features in the seismic profiles : the structures are asymmetric. there is flexural syncline on the east side and a monocline on the west side. asymmetric repetition of stratigraphic units is present in the drill wells and the dips of beds and faults are gentle. the permo - carboniferous system of both sides almost lie in the same slope and the events of cambrian or upper proterozoic are continuous from east to west. the phenomenas suggest that kongxi buried hill could be a thrust belt been traced which consists of reverse faults. the imbricate faults mainly effect pre - jurassic strata. there are obvious angular unconformity between jurassic - cretaceous system and paleozoic involved deformation of thrust. the thrust front in some place has cut off the beds of jurassic - cretaceous system. the structural style of the thrust structure changes along the strike of the kongxi buried hill

    地震和鉆井資料揭露的孔西構帶前第三系潛的地質特徵可以歸納為:構帶總體上對稱構帶內部有地層重復現象石炭二疊系地層的位置明顯高於兩側的同一地層的高度。用由34條向東傾斜的逆沖斷層組成的疊瓦扇構模式能夠比較理地解釋上述地質特徵。該帶向東傾斜的逆沖疊瓦狀斷層組主要影響前侏羅系地層,侏羅白堊系與捲入逆沖構變形的古生界地層之間有明顯的角度
  2. ( 4 ) the formation and growth of structural traps and stratigraphic - unconformity traps in the area is controlled by three compressive stages of silurian - devonian, late permian - tertiary and oligocene - quaternary ; non - structural and compound traps mainly grew in the early paleozoic. structural traps mostly grew in the late paleozoic and the cenozoic and mostly grew on the north and south belts ; non - structural traps mostly grew in the northern area of the hetian concave. most traps in the area formed or typed at last in the himalayan episode, dispersed on the north and south belts

    ( 4 )研究區構與地層圈閉的形成和發育受志留-泥盆紀、晚二疊世-第三紀、漸新世-第四紀三個擠壓階段的控制;早古生代主要發育非構圈閉和復圈閉,晚古生代和新生代則主要發育構圈閉:構圈閉主要發育在南北兩帶上,其次為中帶;非構圈閉主要發育在和田凹陷以北的地區;研究區內大多數圈閉是喜期形成或最終定型的,在南北兩帶都有分佈,而海西期圈閉主要分佈於研究區中帶瑪南構帶處。
  3. On the base of fully utilizing the available data about tectonic maps and structural elements, the present paper has made synthesized research that used the ways of stratigraphic sequence edge unconformity analysis and stratigraphic thickness correlation analysis, and combined seismic - data interpretation, review of paleo - structure and ancient landform and research of tectonic evolution and petroleum system, and combined region and location, plane and profile and time and spatial. by the synthesis analysis on tectonic evolution of hetian paleo - uplift in tarim basin, the results indicate that : ( 1 ) hetian paleo - uplift is a sedimental and erosional paleo - uplift. the formation and evolution of the hetian paleo - uplift experienced three stages, that is, the uplifting and eroding stage of the caledonian period, the depositional stage of the hercynian period and the destroying stage of the himalayan period, and evolved from paleo - lift to inclining strap at last

    本文採用地質和地球物理相結的研究思路,運用多種技術手段和方法;在充分利用已有構圖資料和構要素資料的基礎上,運用地層層序邊界分析法、地層厚度對比分析法,結地震資料的精細解釋、古構和古地貌的恢復、構演化史研究、含油氣系統的研究,和區域和局部、平面和剖面、時間和空間的結研究,對塔里木盆地和田古隆起構演化及油氣關系進行了綜分析,認為: ( 1 )和田古隆起為一沉積?剝蝕性古隆起;形成於志留-泥盆紀;其構演化可分為三個階段,即加里東期的抬升剝蝕階段、海西期的沉積階段和喜期的破壞階段,最終由古隆起演變為一斜坡帶。
  4. Based on the theory of plate tectonics and principles of that hydrocarbon basin being researched integratedly, dynamicly and comprehensively, by mease of the study which ranges from the regional structure background of yili basin formed to the yili - zhongtianshan micro plate, to the yili block, to the yili basin, the formation and evolution characteristics of the different structure units and their different controlling effects to the formation of oil and gas basis are analyzed in this dissertation

    本文以板塊理論為指導,以含油氣盆地體、動態、綜研究為原則,通過伊犁盆地形成的區域構背景、伊犁?中天微板塊、伊犁地塊、伊犁盆地大到小逐級的研究,分析了同構單元的形成、演化特徵及對盆地油氣形成、演化的控製作用。
  5. Based on the wholly, dynamics and integrated principle, the guide of petroleum geology and computer technology, the research has been done as follows by the factors of geology, gravity, magnetism and electricity : ( 1 ) building chronostratic framework of wangjiang - qianshan and its neighbor, divide and compare carbonic and permain sequence. ( 2 ) studying distribution of sediment series in different period. ( 3 ) studying the basic tectonic transform style, preliminarily dividing main tectonic units. ( 4 ) describing the formation and evolution of basin

    本文以體、動態、綜分析為原則,以石油地質理論為指導,以計算機技術為手段,利用地面地質、重力、磁力、電法所獲得的各項參數,進行了以下研究工作:建立望江?潛盆地及鄰區的年代地層格架,並對石炭、二疊系地層進行層序劃分與對比;研究同時期沉積體系的展布特徵;研究盆地的基本構變形樣式,初步劃分盆地的主要構單元;描述盆地的形成演化過程;在上述研究基礎上劃分推測的含油氣系統。
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