特提斯 的英文怎麼說

中文拼音 [tèdīsī]
特提斯 英文
tethys
  • 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
  • 提斯 : dino de laurentiis
  1. While they were celebrating their victory, and jealously discussing who was to be his successor, thetis the nereid, foreseeing a civil war on olympus, hurried in search of the hundred - handed briareus

    當他們歡慶勝利並且懷著猜疑妒忌之心討論繼承宙斯王位的人選時，海上女神特提斯看到奧林波斯山將爆發一場內戰，便急匆匆把百臂巨人布里亞柔斯找來。
  2. There are 25 genera and 47 species of conodont, 4 genera and 6 species of coral and some foraminifera. ch. 4 biostratigraphical regions based on the study on the conodont, coral and foraminifera fossils in research area, it was discovered that the biota features are resemble to the south china. so a conclusion can be drawn that the research area and south china belong to the same biogeographical region

    生物地層分區本文通過對牙形刺、蜒類、珊瑚等化石的對比研究，發現研究區的生物群特徵與華南區生物群相近，這表明在該區早、晚石炭世與華南區及東古特提斯區同屬一個生物地理區系。
  3. 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。
  4. The qiongzhong and danxian granites are belong to the kcg - type ( k - rich calc - alkaline ) granitoids according to the tectonic nomenclature by barbarin ( 1999 ). these foliated kcg - type granites with original orientated structure are the results generated in a changing geodynamic orogenic environment with alternating compressional to extensional stress field. this suggests that hainan island has been a part of south china since latest permian, and been major in extrusion environment of the tethys tectonic system

    根據barbarin （ 1999 ）分類，瓊中和儋縣巖基花崗巖屬于高k及含鉀長石斑晶的鈣堿性花崗巖，同時它們具有原生定向構造，是擠壓?鬆弛?擠壓的構造演化過程的產物，表明海南島從二疊紀末期開始已經是華南大陸的一部分，主要受到了特提斯構造域的影響。
  5. 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
  6. 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。
  7. 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。
  8. 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，構造上位於古特提斯構造域的東段，其中滇西北金沙江帶是揚子陸塊與岡瓦納陸塊的交匯部位，而師宗-彌勒帶則分隔了揚子陸塊與華夏陸塊。
  9. Dawn breaks over the tethys sea, 48 million years ago, and the blue - green water sparkles with the day ' s first light

    話說4800萬年前，特提斯海上天剛破曉，藍綠色的海面閃耀著黎明的陽光。
  10. There existed several strong reformation of late - yanshan movement and himalaya movement the generation, development, disappearance and reformation are tightly related to tarim block, tianshan belt and tethyan tectonic zone, especially tianshan belt, which makes the great difference between present and original basin

    該盆地形成后經歷了燕山晚期和喜山期構造運動的多期強烈改造；其產生、發展和消亡以及改造與塔里木地塊、天山構造帶、特提斯構造域的演化息息相關。其中尤以天山構造帶的活動影響最大，從而造就盆地今古面貌差異巨大。
  11. Seen from the structure, this district belongs to the structure region of tethys - himalayas, " sanjiang " fold system, and the fracture - fold zone of lancangjiang river

    從構造上看，本區屬于特提斯喜-馬拉雅構造域，三江褶皺系，瀾滄江斷裂褶皺帶。
  12. The changning - menglian belt, located the drape belt of three river in structure territory of tethyan - himalayan, is the one of most pivotal areas which is redounded to research and resolve the problem

    昌寧?孟連構造帶位於特提斯?喜馬拉雅構造域三江褶皺帶，是研究和解決該問題的最為關鍵的地區之一（劉本培等， 1993 ；崔春龍， 1999 ） 。
  13. 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。
  14. 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。
  15. 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。
  16. 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。
  17. 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。
  18. The gold ore deposits are mainly distributed in the north china platform, yangtz platform and tethys, the three tectonic - metallogenic realms

    金礦床（點）主要分佈在華北地臺、揚子地臺和特提斯三大構造成礦域中。
  19. The term of the previous precambrian metallogenic domain is not adopted, and the precambrian metallogeny should be discussed as the metallogeny of the basement in the relevant paleo - asiatic, qinling - qilian - kulun and tethys metallogenic domains

    對於前寒武紀成礦作用地區，文章不以「成礦域」稱之，其成礦作用置於古亞洲、秦祁昆和特提斯諸成礦域中以基底成礦作用方式討論之。
  20. 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
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