特提斯洋 的英文怎麼說

中文拼音 [tèdīsīyáng]
特提斯洋 英文
tethys ocean
  • 特 : Ⅰ形容詞（特殊; 超出一般） particular; special; exceptional; unusual Ⅱ副詞1 （特別） especially; v...
  • 提 : 提動詞（垂手拿著） carry （in one's hand with the arm down）
  • 斯 : Ⅰ名詞（古代驅疫時用的面具） an ancient maskⅡ形容詞[書面語] （醜陋） ugly
  • 洋 : Ⅰ名詞1 （海洋） ocean 2 （洋錢） silver coin 3 （姓氏） a surname Ⅱ形容詞1 （盛大; 豐富） vast; m...
  • 提斯 : dino de laurentiis
  1. In the northwest pacific domain, the folding age is from late jurassic to middle eocene, and in the tethys domain it is between middle and late eocene

    主要褶皺時代很晚，在南北太平洋大地構造域是晚侏羅世至中始新世，在特提斯大地構造域是中晚始新世之交。
  2. Is there a neo - tethys subduction record earlier than arc volcanic rocks in the sangri group

    存在比桑日群弧火山巖更早的新特提斯洋俯沖記錄么
  3. Thus, it can be clearly recognized that the global continents located at near equator and southern hemisphere, showed the characteristics of range along latitude ; chinese continental blocks still located among the laurentia, siberia and gondwana in paleozoic ; following the fast moving of siberia plate to northwards, the amalgamation in north - south direction at the western parts of laurentia and gondwana, subducted the lapetus and rheic oceans, until to form the uniform pangea in the late stage of paleozoic ; however australia and india plates in eastern gondwana move and disperse gradually to southwards, to extend crust and form the paleo - tethys ocean ; the chinese continental blocks and adjacent blocks still located in paleo - tethys ocean, preserved the status of dispersion, gradually moving to northwards, showed the characteristics of range along north - south orientation, until carboniferous and triassic a series of local collisions happened in tianshan - hing ' anling, kunlun, qinling - dabie, jingshajiang and shaoxing - shiwandashan zones, thus the most part of chinese continental blocks amalgamated to eurasia continent

    由此可以清晰地看出，在古生代早期全球各大陸的主要部分都位於赤道附近及南半球，大致表現為沿緯度、呈東西向排列的特徵，中國及鄰區的小陸塊群在古生代始終都處在勞倫大陸、西伯利亞與岡瓦納大陸之間；隨著西伯利亞大陸的快速北移，在勞倫大陸與岡瓦納大陸的西部地區發生南北向拼合，亞皮特斯洋和里克洋的消亡，到古生代晚期形成統一的泛大陸；而岡瓦納大陸的東部（澳大利亞和印度等）則逐漸向南移動、離散，地殼張開，構成古特提斯洋；中國及鄰區的小陸塊群則一直處在古特提斯洋中，保持離散狀態，總體上緩慢地向北運移，並逐漸轉為近南北向的排列方式，石炭紀到三疊紀才在天山興安嶺、昆侖山、秦嶺大別、金沙江和紹興十萬大山等地段發生一系列局部性的陸陸碰撞，使中國大陸地塊的大部分逐漸併入歐亞大陸。
  4. The marginal ocean basin ' s formation and evolution model may be as follows : early triassic, rift was formed by extension and splitting in india ( gondwana ) continental margin during it was drifting southward ; late triassic, the rift had been joined in the neo - tethys ocean in the east and converted into initial ocean basin, and ayila - zhongba micro - continental was formed in north of the rift

    洋盆的演化模式是：早三疊世，隨著印度（岡瓦納）大陸向南漂移，其北部邊緣因引張裂解產生裂谷，于晚三疊世向東開口與新特提斯洋主體連通，洋盆初具洋殼性質，北側形成阿依拉仲巴微陸塊。
  5. By analyzing runyang ' s musicological analysis of prelude and finale of tristan and isolde, the author made some suggestion on discipline development of musical analysis

    摘要通過分析于潤洋先生的《歌劇特里斯坦與伊索爾德前奏曲與終曲的音樂學分析》一文，提出關于音樂分析學科發展的建議。
  6. Then war will start all over again, and then our civilization might be gone, just like the ones that have been discovered recently from the atlantic dig or ancient atlantis, or the ancient alien people

    只會使彼此誤會，小事一樁卻釀成大禍，變得一發不可收拾，於是又燃起戰火，人類的文明可能因此付之一炬。好比最近發現到的沈沒于大西洋的古代亞特蘭提斯城，或是所謂的古代的外星人。
  7. Since twenty years, with the information accumulation, geologists had already cognizant that the transformation of the asia - australia - pacific ocean area during entire virtually is a process of disorganization of gawana landmass and hyperplasia of asia continent. the most complex and important terra segment in the area is the location which links up the eastern part of tethyan and pacific ocean

    近二十年來，隨著資料的積累，地質學家已經認識到，亞洲?澳洲?太平洋地區在整個顯生宙期間的變化實質上是一個岡瓦納大陸解體和亞洲大陸增生的過程（黃汲清等， 1987 ；殷鴻福等， 1988 ；鐘大賚等， 1993 ） ，其中最為復雜和重要的地段就是特提斯東段與太平洋的銜接處。
  8. The research base on the theories of plate tectonics, use the method that oil and gas basin is analyzed integrally, dynamically and comprehensively, and obey the principle that intersection, superposition and compound of the three tectonic domains ( the paleo - asian, the tethyan and the circum - pacific ) control and influence the formation and development of ordos basin in different tectonic stages

    本文以板塊構造理論為基礎；以含油氣盆地整體、動態、綜合分析研究為原則；以古亞洲、特提斯、濱太平洋三大構造域交切、疊合和復合，控制和影響著鄂爾多斯盆地在不同構造演化階段的形成和發育為指導思想。
  9. The strike - slip event in early cretaceous made the largest contribution to the basin was that it broke the basin pattern of foreland and strike - slipping flexure in indosinian and went into a newly nne structure pattern. this indicated that the tectonic scenario of the basin had been changed from teties structure to the pacific tectonics

    該期走滑事件對合肥盆地的最大貢獻在於它打破了印支期，前陸+走滑的盆地格局，而進入到一個全新的北北東向的構造格局，標志著盆地的構造背景由特提斯為主的構造域向以太平洋構造域為主的轉化。
  10. The authors put forward that daba - xiugugabu ophiolite belt originated from an ancient oceanic crust fragment of india continental northern marginal ocean basin, that was approximately synchronous with the formation and evolution period of the neo - tethys ocean

    筆者提出該區蛇綠巖來源於印度大陸北緣洋盆的洋殼碎片，這個陸緣洋盆與新特提斯洋主體的形成和演化準同步。
  11. During subduction northward of neo - tethys oceanic plate, ayla - zhongba micro - continental, the marginal ocean basin and india continental drifted northward all together, the marginal ocean basin was gradually contracted and closed by compressed of india continental

    在新特提斯洋板塊向北俯沖消減過程中，阿依拉仲巴微陸塊、陸緣洋盆和印度大陸一起隨著向北漂移，在印度大陸向北擠壓作用下洋盆逐漸收縮以致最終閉合。
  12. Shrimp dating of carboniferous jinshajiang ophiolite in western yunnan and sichuan : geochronological constraints on the evolution of the paleo - tethys oceanic crust

    古特提斯洋殼演化的同位素年代學制約
  13. The internal mineral separates and whole - rock sm - nd isochron age for gabbro dikes from the dangqiong ophiolite is 373 ? 8ma, inferring a magmatic activity during late devonian, which end ( t ) = + 3. 3 suggests that its tectonic setting was probably oceanic island

    其nd （ t ） = + 3 . 3 ，認為其時形成環境為洋島，可能代表了新特提斯蛇綠巖形成時所攜帶的古老洋殼。
  14. Pettitte has also pitched 1, 943 1 / 3 innings with the bombers and needs 8 2 / 3 more to tie jack chesbro for ninth place in team history

    派提特在洋基一共出場19431 / 3局，只要在8又3分之2局就可以追平由傑克?錢斯伯保持洋基隊隊史上出賽局數最多的第九名（ 1953局） 。
  15. All in all, in carboniferous nujinshan ophiolite melange, petrographic category and their geochemical characteristics can be correlated with representative ophiolite melange in the world. this discovery offered a convincing evidence from petrology, it tes

    這一發現提供了一個令人信服的巖石學證據，它表明了昌寧?孟連構造帶的確是古特提斯洋的殘跡。
  16. Our research work was carried out effectively and fruitfully. this will give exact chronology and sedimentary evidence to the research of the biostratigraphy and thrust slice type stratigraphy of the nongba area ; will provide more full and accurate geological gist for the tectonic evolutions of paleotethyan located in southern part of " three rivers " ; and will provide new reference to the paleolithofacies palaeogeography pattern reconstruction of the changning - menglian oceanic basin

    這些工作將為滇西南耿馬弄巴地區生物地層學和造山帶地層學的研究提供準確的時代和沉積學證據；為「三江」南段古特提斯的構造演化提供更為翔實的地質依據，也為恢復昌寧?孟連洋盆的古地理格架提供了新的參考。
  17. Based on the geological, stratigraphic and geochemical characteristics of the ophiolitic melange, island - arc and rift volcanic rocks from the jinshajiang zone, an archipelagic tectonic model with multi - rift and multi - subduction is proposed to explain the evolution of jinshajiang paleo - tethys. the ophiolitic melanges of the jinshajiang zone are mainly outcropped at baimangxueshan, tongduo, gongka, dongzhulin and jiyidu in the deqin county. the geochemistry of major and trace elements of the jinshajiang ophiolite shows its geochemical characteristics are similar to those of the more and island - arc volcanic rocks, but different from those of the typical n - mopjb

    金沙江蛇綠混雜巖主要分佈在德欽縣的白茫雪山、通多、共卡、東竹林和吉義獨地區，主量和微量元素地球化學特徵研究表明，金沙江蛇綠巖不具有典型n - morb的地球化學特徵，而具有介於morb和島弧之間的地球化學特徵，暗示它並非形成於寬闊的大洋環境，不是古特提斯在滇西北地區的主縫合帶，可能是古特提斯多島洋體系中的一個弧后盆地。
  18. The main continent rift developed in mid - late proterozoic ; the paleo - asian tectonic dynamic system played an important role in the paleozoic period ; the combination of tethys - paleopacific tectonic dynamic system influenced the basin in mesozoic. during that period, the tethyan dynamic system affected the basin in the early stage ( t ) while paleo - pacific dynamic system affected it in the latter stage ( js - k ) ; the new tethyan - circum pacific tectonic dynamic system dominated in cenozoic period

    中新元古代為大陸裂谷集中發育階段；古生代主要受控于古亞洲構造動力學體系；中生代主要受控于中特提斯?古太平洋構造動力體系的聯合作用和影響，其中早期（ t ）主要受特提斯動力體系影響，晚期（ j _ 3 - k ）主要受古太平洋動力體系影響；新生代主要受控于新特提斯?今太平洋構造動力體系的聯合作用和影響。
  19. Kashan block of iran is the first oversea risk exploration block of chinese petrochemical co. ltd. kashan block is located in the south - west edge of iranian basin. on the structure, it belongs to alpines - himalayan orogeny belt controlled by dynamic system of tethys - indian ocean

    伊朗卡山探區是中石化海外的第一塊風險勘探區塊，位於中伊朗盆地西南邊緣，構造上屬于特提斯?印度洋動力體系作用控制的喜馬拉雅-阿爾卑斯造山帶。
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