洋盆 的英文怎麼說

中文拼音 [yángpén]
洋盆 英文
ocean basin
  • : 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...
  • : 1. (盛東西或洗東西用的器具) basin; tub; pot 2. (姓氏) a surname
  1. Abyssal oceanic basin

    深海大洋盆
  2. This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement, whose tectonic deformation and magma intrusion is fiercely, and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian, it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area, such as a - granite ' s stock, batholiths and diabase ' s dike. there are many fault depressions possible

    按照不同構造層,研究了各構造層的構造特徵:基底構造層:受早海西期構造作用的影響,與準噶爾洋盆俯沖閉合、而後陸-陸碰撞的區域擠壓構造作用有關,為一構造變形和巖漿侵入活動強烈的古生代褶皺基底。二疊系構造層:受中海西區域性伸展斷陷作用的影響,地及其周緣地區發育與伸展構造有關的構造-巖漿組合,如呈巖株、巖基狀侵位的a型花崗巖以及呈巖墻狀侵位的輝綠巖等。
  3. Distant effect of jurassic collisions of qiangtang terrane, lasa terrane and paleo - pacific land onto the eurasian land made east qinling - dabie mountains in a compressional circumstance for a long time, and suppressed its orogenic extension ; whereas, cretaceous late - collisional extension and appearance of west pacific trench - arc - basin system relieved east qinling - dabie mountains of external compression, instantly result in violent orogenic lithosphere delamination - extension and depressurized - calefactive melting, and consequently, led to the formation of large scale early cretaceous granitoids and intermediate - acidic volcanic rocks

    羌塘地體拉薩地體和西太平古陸在侏羅紀與歐亞大陸拼貼碰撞的遠距離效應使東秦嶺大別造山帶長期處于擠壓環境,伸展作用被抑制白堊紀的碰撞晚期伸展和西太平溝弧體系的遠距離效應使東秦嶺大別地區的外部擠壓消失,導致造山帶巖石圈迅速強烈拆沉伸展和減壓增溫熔融,從而形成大規模早白堊世花崗巖類和中酸性火山巖。
  4. Over ages, hot convection currents in this sea, as well as gravitational forces, move the plates and their superimposed continents and ocean basins, tearing them apart and rearranging them like pieces of a giant jigsaw puzzle

    隨著歲月流逝,海中熱對流及重力移動板塊及覆蓋在上面的大陸塊和海洋盆地,將它們撕裂再重新組合,如大拼圖游戲的碎片。
  5. On the declivity of the atlantic basin the first streams, branches of the north platte river, already appeared

    在大西洋盆地的山坡地區,分佈著許多由北普拉特河分出來的支流小河。
  6. The geochemical characteristics of gabbros from the jinshajiang ophiolitic melange indicate that they were derived from a mantle source different from that of volcanic rocks, which may be a product in the ocean rift in the earlier stage

    東竹林蛇綠混雜巖中輝長巖地球化學特徵表明,它與火山巖不同源,可能是洋盆裂谷初期的產物。
  7. By physiognomy feature, it could be divided into three types of thermal structure : positive dome model, negative collapse model and border dome core collapse model. based on the depth degree or magma - thermal influenced, it could be divided into five types of thermal structure : ( ancient ) geothermal anomaly focus region model, superficial volcano eruption hydro - thermalism and hypabyssal intrusive model, thermal anticline ( thermal dome ) model, mid - deep intrusive model, deep mantle ( crust ) thermal plume model ; and put forward a perfect model of the thermal structure. there are many interaction system could be induced into a systematic thermal interaction, include : ocean - continent system, basin - mountain interaction, superficial and mid - deep crust - mantle interaction, crust - mantle commingle interaction, vertical thermal interaction ( delamination ) etc.

    依據地貌形態分為三類:正向穹窿型、負向塌陷型、邊隆核陷型:依據巖漿-熱力作用影響的深淺程度或深度分為五類: (古)地熱異常群集區、表淺層火山噴發-熱液活動與淺成侵入型、熱力背斜(熱穹窿) 、中深層侵入型、深部地幔(地殼)熱柱型;提出了熱力構造作用空間分佈的理想模式,將陸系統、山作用、淺表與中深部殼幔作用、殼幔混合、垂向熱力作用(拆沉)等納入一個整體統一的熱力作用系統中,為地動力學研究打開了一個新窗口;研討了熱力構造研究方法。
  8. The geochemistry characteristic of fuchsia radiolarian silicalite indicates that they deposited in the of edge of oceanic basin near the continental margin, not the typical caontinental margin environment

    從硅質巖的地球化學特徵表現來看,紫紅色放射蟲硅質巖部分不是形成於典型的大陸邊緣環境中,而是形成於近大陸邊緣的洋盆邊緣環境。
  9. The difference accounts for the existence of continents and ocean basins.

    這種差別解釋了大陸和海洋盆地存在的原因。
  10. 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主體連通,洋盆初具殼性質,北側形成阿依拉仲巴微陸塊。
  11. Jurassic and cretaceous, the marginal ocean basin was in the stage of ocean crust evolution and had a setting similar to mid - ocean ridge

    侏羅白堊紀為洋盆殼演化期,處于類似中脊的構造環境。
  12. This suggests that the paleo - ocean represented by qom, separating the south kunlun massif from north kunlun massif, might be a smaller ocean basin other than a bigger one

    這說明昆北地塊和昆南地塊具有相當的親緣性,分隔它們的其曼于特蛇綠巖所代表的洋盆不大。
  13. These ophiolites may be originated from the small spreading oceanic ridges of back - arc or inter - arc restricted oceanic basins, and finally emplaced into the deep - sea sediments constituting the ophiolites in orogenic zones

    蛇綠巖可能形成於孤后或孤間有限洋盆小擴張脊;最後侵位到深海沉積物中,形成了造山帶中的蛇綠巖。
  14. These intrusive rocks are the products of the closure of the yarlung zangbo and banggonghu - nujiang oceanic basins and may represent three magma - induced thermal disturbance events of plate subduction, collision, and post - collision

    它們是雅魯藏布江洋盆和班公湖-怒江洋盆關閉的產物,主體代表了板塊俯沖、碰撞和碰撞后三個時期的巖漿熱擾動事件。
  15. 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殼碎片,這個陸緣洋盆與新特提斯主體的形成和演化準同步。
  16. 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。
  17. Weertman ' s troubling conclusion was that any ice sheet that fills a marine basin is inherently unstable when global sea level is on the rise, which most scientists agree has been the case for the past 20, 000 years

    惠特曼提出憂心的結論,他認為當全球海平面上升時(絕大多數科學家同意過去兩萬年來正是這種情況) ,任何填積海洋盆地的冰原本質上都不穩定。
  18. That ' s one area of the earth where gravity is weakest, thanks to the deep mid - indian basin

    那裡屬于深陷的中印度洋盆地,是地球重力最弱的地區。
  19. In addition to the above appointments, mr. he is the chairman of the board of chiyu banking corporation limited, chairman of the board of nanyang commercial bank limited, designated representative of bochk for the hong kong association of banks, member of the hong kong monetary authority exchange fund advisory committee and banking advisory committee, member of the board of airport authority hong kong, director of hong kong interbank clearing limited, director of hong kong note printing limited, president of the hong kong chinese enterprises association and general committee member of the hong kong general chamber of commerce

    此外,還擔任集友銀行董事長南商業銀行董事長香港銀行公會之中銀香港指定代表香港金融管理局外匯基金諮詢委員會及銀行業諮詢委員會委員香港機場管理局董事會成員香港結算有限公司董事香港印鈔有限公司董事香港中國企業協會會長香港總商會理事中國國債協會常務理事及太平洋盆地經濟理事會中國委員會委員等職。
  20. 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。
分享友人