新生洋盆 的英文怎麼說

中文拼音 [xīnshēngyángpén]
新生洋盆 英文
nascent ocean
  • 新 : Ⅰ形容詞1 （剛出現的或剛經驗到的） new; fresh; novel; up to date 2 （沒有用過的） unused; new 3 （...
  • 生 : Ⅰ動詞1 （生育; 生殖） give birth to; bear 2 （出生） be born 3 （生長） grow 4 （生存; 活） live;...
  • 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...
  • 盆 : 1. （盛東西或洗東西用的器具） basin; tub; pot 2. （姓氏） a surname
  • 新生 : 1 （剛產生的） newborn; newly born 2 （新生命） new life; rebirth; regeneration; a new lease of [...
  1. On the influence of global change of cenozoic climate and uplift of himalayas, the area began to present a distinct seasonal climate on the basis of previous warmth and humidity in pliocene

    受新生代全球氣候變冷和喜馬拉雅運動的影響，該盆地一方面受印度洋季風的影響增強，干濕季節交替明顯；另一方面受地形地貌影響，沿襲了溫暖濕潤的氣候條件。
  2. 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。
  3. During this evolution, seven second - order tectonic units were formed ; from north to south are the mingqianri cretaceous residual sea basin, the arsuo tectonic melange zone, the taricuo - wenbu yenshan magmatic arc belt, the cuoqin - bangduo late paleozoic composite back - arc basin, the jiangrang - geerdi faulted uplift, the gangdise - chazi himalayan magmatic arc belt, and the xigaze - anba fore - arc basin. these units comprise important parts of a poly - arc - basin system and exhibit evolutional features of mesozoic to cenozoic arc - basin systems. mosaic pattern of these tectonic units delineates the lithosphere coupling processes of the gangdise tectonic belt under mechanisms such as back - arc basin attenuation and arc - continent collision

    自中新生代以來，岡底斯構造帶經歷了洋殼俯沖、弧陸碰撞、陸內俯沖-碰撞、走滑和塊段隆升的多階段構造演化歷程，形成了由北向南七個二級構造單元，即岷千日白堊紀殘余海盆、阿索構造混雜巖帶、它日錯?文部燕山期巖漿弧帶、措勤?幫多晚古生代復合弧后盆地、江讓?格爾耿斷隆、岡底斯?查孜喜馬拉雅期巖漿弧帶、日喀則?安巴弧前盆地。
  4. Based on the study of geological background and structural settings, and with the geological event as the main thread, the author analyzed the development history of the regional ore - forming structures, especially, the new - forming and inherited structural systems since yanshanian movement, and the range - basin structures of marginal - pacific ore - forming domain, and the thermo - uplifting structure of the lushan ore - body as well as the yiwulushan metamorphic core complex, which are three different scale ore - forming structural systems

    論文在緊密結合地質背景、構造背景研究的基礎上，以地質事件為主線，分析該地區域成礦構造的成生歷史，特別是燕山運動以來繼承及新生的構造體系格架與濱太平洋成礦構造域的盆嶺構造、閭山巖體熱隆、變質核雜巖等3個不同級別的區域成礦構造系統。
  5. 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。
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