構造陸塊 的英文怎麼說

中文拼音 [gòuzàoliùkuāi]
構造陸塊 英文
tectonic land
  • : 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...
  • : 陸數詞(六的大寫) six (used for the numeral 六 on cheques, etc. to avoid mistakes or alterations)
  • : 名詞(古時佩帶的玉器) penannular jade ring (worn as an ornament in ancient china)
  • 構造 : structure; construction; constructional detail; tectonic; structural; makeup; anatomy; constituti...
  1. Four tectonic evolution phases have been made out in this area. they are original crust formed in the archean - early proterozoic era, continental crust shearing in the middle - new proterozoic era, plate tectonic developed in sinian - triassic period and intracontinental orogeny in the middle cenozoic period

    將區內演化歸納為太古?早元古代原始地殼形成、中新元古代大地殼裂解、震旦?三疊紀板體制、中新生代山等四個演化階段。
  2. Based on the principles to respect believable and higher precise paleomagnetic data of blocks and to pay attention to the similarity of paleo - biogeography and the coordination of tectonic evolution, the paleomagnetic data of chinese continental blocks and adjacent areas for paleozoic and triassic were collected, the chinese continental blocks were laid up on the reconstruction of global paleo - continents with similar scale

    摘要在尊重比較可靠的、測試精度較高的地古地磁數據,重視生物古地理與地質演化史的相似性和協調性等原則的基礎上,筆者編制了中國大及鄰區各古生代和三疊紀的古地磁數據表,並採用類似的比例尺,將中國各放到相應的全球古大復原圖上去。
  3. Chagan sag is a secondary tectonic unit in chagandelesu depression, northeastern yingen - eji ' naqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate, with the character of erogenic belt. in working area and its adjacent area, the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly, intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase

    查干凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級單元,其盆地基底為古生代時期華北板、哈薩克斯坦板和塔里木板交接部位形成的緣或島弧褶皺帶,具有古生代山帶的性質。研究區及鄰區印支期侵入巖形成於山帶強烈擠壓內俯沖的環境;燕山早期侵入巖形成於由擠壓轉向拉伸、山帶的增厚殼開始發生伸展垮塌的環境;早白堊世火山巖形成於山期后進一步發生伸展垮塌的區域環境。
  4. Chagan fault depression is a secondary tectonic unit in chagandelesu subbasin, northeastern yingen - ejinaqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc with the character of erogenic belt at the connection region of north china plate, tarim plate and kazakstan plate

    查干德勒蘇凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級單元。其基底為古生代時期華北板、塔里木板和哈薩克斯坦板交接部位的緣或島弧褶皺帶,具有古生代山帶的性質。
  5. Continental drift is now believed to reflect the movement over geological time of underlying plates in the earth ' s crust - the theory of plate tectonics

    學說提出后,大漂移說又獲得了新的含義,它反映了地殼運動和大州大洋的分佈規律。
  6. The most important tectonothermal event in the ncc took place at ca. 1800 ma. the event was traditionally interpreted as the " luliang movement ", marking the finial cratonization of the ncc

    華北最重要的一次-巖漿-變質活動發生在1800ma ,傳統上被稱之為「呂梁運動」 ,並作為華北克拉通基底穩定化的標志。
  7. Tectonic framework of north china block and its cratonization in the early precambrian

    華北基底格局及早期大克拉通化過程
  8. The tectonism in this area can be divided into three phases, that is the folded basement formation and stable ancient land in pre - mesozoic, ancient land cracking phase in mesozoic, the faulted activity and subsidence phase in cenozoic

    本區變動劃分為三個大的階段,即:前中生代褶皺基底的形成和穩定古發育階段、中生代古裂解階段、新生代斷活動及整體沉降階段。
  9. The tectonic subsidence curves on the southeastern margin of the yangtze plate are drawn out using of backstripping method for the basin formation and evolution. the basins located in the southern margin of the yangtze plate, in the basin dynamic computer simulation, is explored and constituted to be a typical foreland basin which is of not rather high mountain and thermal situation to be lower in this older orogeny belt

    在沉積盆地分析方面,基本查明揚子板東南邊緣早古生代被動大邊緣沉積特徵及沉積演化,同時運用反剝法技術對揚子板東南大邊緣沉積盆地形成,演化的沉降動力學進行探討,運用計算機模擬方法,定量動力沉積學對揚子東南邊緣奧陶紀到志留紀前地進行計算機模擬分析,探索並建立這個古老山帶前盆定量參數和動態定量模擬。
  10. Scanning the formation - evolutionary histories of continental orogenic belts in both our country and whole workd, an orogenic belt has often undergone numerous and various tectono - evolutionary stages, such as palaeo - continental break - up, ocean - land transition, continental matching - collision, intracontinental extension - basin - range coupling, new tectonic uplift ( intracontinental orogeny ), etc., which are respectively companied with characteristic volcano - magmatism

    縱觀我國以至全球的大山帶形成-演化歷史,一個山帶往往經歷了古大裂解、洋轉換、拼合-碰撞、內伸展-盆山耦合和新隆升(山)等?多不同的演化階段,這些不同的演化階段和不同的環境均有特定火山巖漿作用與之相伴。
  11. Along with the eroding mountains and sediment filling the seas, smaller bits of the continents - islands and archpelagos - are drawn closer to the continental edge and compressed onto its margins

    山上沖洗下的沉積物填充了大架上的淺海,為大增添了更多的地。大運動在活動帶移動大,重復著大成。
  12. The formation age and tectonic setting of the kangding complex in the western margin of the yangtze block

    揚子西緣康定雜巖的形成時代和環境
  13. According to the characteristics of strata, tectonization and magmatism within the research area in the southwest margin of north china paleocontinent, and under the ideological guidance of mobilism and systematology, the geotectonic framework of the area could be divided as follows : ( 1 ) the longshoushan mountains continental margin ; ( 2 ) the hexi corridor back - arc basin ; ( 3 ) the northern qilianshan mountains suture zone ; ( 4 ) the central qilianshan mountains dispersion type island arc terrane ; ( 5 ) the southern qilianshan mountains back - arc basin ; ( 6 ) the qaidam massif

    根據本區地層、、巖漿作用特點,在「系統論」 、 「活動論」思想指導下,釐定華北古大西南邊緣的格局如下:龍首山緣帶、河西走廊弧后盆地、北祁連縫合帶、中祁連離散型島弧地體、南祁連弧后盆地、柴達木地
  14. The study areas are located in the jinshajiang zone, nw yunnan and sw part of the shizong - mile zone ( jianshui ), se yunnan respectively, and tectonically belong to the east part of the paleo - tethys tectonic domain. the jinshajiang zone in nw yunnan was a joint terrain between the yangtze and the gondwana blocks, and the shizong - mile zone delineates a suture line between the yangtze and cathaysian blocks

    研究區分別位於滇西北金沙江帶和滇東南師宗-彌勒帶西南段建水地區,上位於古特提斯域的東段,其中滇西北金沙江帶是揚子與岡瓦納的交匯部位,而師宗-彌勒帶則分隔了揚子與華夏
  15. It is difficult to explain these characteristics by the plate tectonic theory based on the heat convection in earth mantle

    想用板理論解釋遍布大內部的褶皺,在形位特徵與動力機制上都有難以解決的矛盾。
  16. Forecasts of future continental motion developed slowly as offshoots of the theory of plate tectonics, which won acceptance in the 1960s and 1970s, shattering old dogmas of continental immobility

    預測未來大的動態,漸漸發展成地板論的分支,在1960和1970年代成為定論,並粉碎大靜止不動的舊說。
  17. The continental orogenesis is characterized with the following features, such as sudden start, global synchronicity and horizontal movement, occurring mainly in the upper part of the crust and weakening with depth, and so on

    摘要大山運動具有突發性、全球同步性,以水平運動為主,主要表現在地殼上部且具有上強下弱等特徵,除水平運動一項外,與基於地幔對流的板理論缺少共同之處。
  18. Several important tectonic events took place in the chinese continent during the early paleozoic, such as the amalgamation of xiyu plate, forming a unified crystalline basement with the cathaysian plate, development of widespread intraplate deformations in southern yangtze plate, and the occurrence of altay - ergun collision zone

    它們與蘇格蘭阿帕拉契亞的加里東事件完全不同,在中國大出現了西域板完成拼合,華夏板成統結晶基底,南揚子板廣泛發育板內褶皺,此時還形成了阿爾泰額爾古納碰撞帶等重要事件,而以中朝和北揚子板為代表的其他板則主要表現為穩定沉積,地運移,並呈離散狀態。
  19. This thesis is relied on the subject " analysis of prospecting foreground and evaluation of favourable play of oil and gas in santanghu basin " and based on areal geology, gravity, magnetism, electricity, seism, rock - core etc, and it ' s guiding ideology is the plate tectonic theory, the continental dynamics. the new achievements and the new understandings of the international exploitation of oil and gas fields. in light of the elementary analytic principles " integrated, dynamic, comprehensive ", it studies the structural features and the formation and evolution of santanghu basin on the the basis of obtaining abundant first - hand data

    本文以「三塘湖盆地油氣勘探前景分析與有利區帶評價」項目為依託,以板理論、大動力學研究以及國際油氣田開發的新成果和新認識為指導思想,以區域地質、重磁電、地震、巖芯等等資料為基礎,獲取扎實的第一手資料, 「整體、動態、綜合」地研究三塘湖盆地特徵及其形成演化。
  20. Based on the theory of plate tectonics and the new knowledge of continental dynamics, this paper starts mostly with tectonic analysis and then makes a comprehensive view on the characteristic of stratum composition, gold mine mineralized, magmatic activity as well as ruptures activity to discuss the yanshanian tectonic evolution of the xiaoqinling area under the regional tectonic framework of qinling orogenic belt

    本文以板理論和大動力學研究的新認識為指導,採用以分析為主線,結合區內地層沉積、金礦成礦、巖漿活動以及南北兩側斷陷盆地形成演化等綜合分析,在秦嶺區域大框架下對小秦嶺燕山期的演化特徵進行探討。
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