orogen 中文意思是什麼

orogen 解釋
造山帶
  1. On the age of metamorphic rocks of the yudongzi group and the archean crystalline basement of the qinling orogen

    魚洞子群變質巖年齡及秦嶺造山帶太古宙基底
  2. ( 6 ) the geological significance of oblique - thrusting fault of sertengshan - xitieshan was discussed in this paper. the oblique - thrusting effect of sertengshan - xitieshan is the result of the long distance effction of himalayan orogenic belt intracontinent subducting, which is of great theory significance for studying regional structural framwork, relations between basins and mountains and oblique - thrusting effect of large - scale fault zone or orogen in northern qaidam basin. moreover, the result is of guidance significance for the forecast of combination gas, distributing and formation of nappe metal deposit in northern qaidam basin

    （ 6 ）論文探討了賽什騰? ?錫鐵山斜向逆沖推覆構造的地質意義，認為賽什騰-錫鐵山斷裂斜沖作用是印度板塊與歐亞板塊碰撞、會聚的遠程效應的結果，該認識對于研究柴北緣區域構造格局、盆山關系以及更大尺度的斷裂帶或造山帶的斜向逆沖作用具有理論意義，對柴達木北緣的油氣預測、推覆體金屬礦床的分佈、形成具有指導意義。
  3. A large number of studies of geochronology and geochemistry indicate that mesozoic intermediate - felsic rocks from the dabie orogen have originated from recycling of the subducted yangtze continental crust itself

    摘要大量的同位素地質年代學和地球化學研究表明，大別山中生代中酸性巖為俯沖揚子陸殼再循環的產物。
  4. The grenville - aged orogen is a tie to link most of the continental blocks in rodinia, which existed during the period from late mesoproterozoic through early neoproterozoic

    Grenville期造山帶存在於中晚元古代，是連接rodinia各陸塊的紐帶。
  5. Evolution of cenozoic collision orogen of north kalimantan and its metallogenesis

    東南亞北加里曼丹新生代碰撞造山帶演化與成礦
  6. An evaluation of zircon u - pb dating for metamorphic rocks and comments on zircon ages of dabie orogen

    兼論大別造山帶鋯石定年
  7. Multiple rotation and amalgamation processes of dabie - tanlu - sulu orogen

    蘇魯造山帶復合旋轉拼貼作用
  8. Under the strong compression from the orogenic belts on both sides, in the jurassic an atypical foreland basin developed on the southern margin of the qilian orogenic belt ; in the tertiary, a two - side foreland basin formed between the qilian orogen and kunlun orogen ; in the quaternary, the qaidam basin is a compressional, downwarped basin

    在兩側造山帶的強烈擠壓作用下，侏羅紀時期在祁連造山帶南緣形成並不典型的前陸盆地，古近紀至新近紀時期則在祁連造山帶與昆侖造山帶之間形成雙側前陸盆地，第四紀屬擠壓坳陷盆地。
  9. This stars knowledge of the ewenki nationality, the orogen nationality, the hezhen nationality and other fishing and hunting nationalities in heilongjiang valley reflects the characteristic of the human being astronomy during the embryonic times

    摘要黑龍江流域鄂溫克、鄂倫春和赫哲等漁獵民族的星辰知識體現著人類天文學萌芽時代的特點。
  10. First, the state of development of mongolian education ; second, state of development of daur education ; third, the state of development of ewenki, orogen, the han nationality, russia live abroad education ; fourth, the state of studying abroad of all minorities

    一、蒙古族的教育發展狀況；二、達斡爾族的教育發展狀況；三、鄂溫克族、鄂倫春族、漢族、俄僑的教育發展狀況；四、各少數民族的留學狀況。
  11. The residue formed by partial melting of thickened crust due to anomalous heat supply by mantle superwelling at early cretaceous is possibly easy to detach from the crust because of its high density, leading to the remove of mountain root and large scale uplift of the orogen

    早白堊世地幔超柱事件熱擾動所引起的加厚地殼部分熔融后的殘留體可能由於比重較大而拆離進入地幔，從而發生去山根作用和造山帶的大面積隆起。
  12. The middle cambrian early devonian ( 513 - 397ma ) tectonic stage was characterized by a series of tectonic events with different features, which are completely different from the caledonian event that occurred in the appalachian orogen and in scotland

    摘要中國大陸早古生代（中寒武世早泥盆世）構造期以發生系列各具特徵、分佈局限、準同時的構造事件為特徵。
  13. Therefore, liupanshan area during late triassic to mid - jurassic is not a compressional orogen

    故六盤山地區在晚三疊世-中侏羅世並不是一收縮造山帶。
  14. Himalayan orogen is by far the youngest and largest active continent - continent collision belt in the world and is the ideal place for studying the plate dynamics of intracontinental convergence and investigating the mechanism responsible for uplift of the plateau

    喜馬拉雅造山帶是世界上目前仍在進行的、最年輕的、規模最大的陸-陸碰撞造山帶，是研究陸內匯集過程板塊動力學以及探討高原隆升機制的理想場所。
  15. The qinling erogenic belt is a composite continental orogen which has evolved in different tectonic regimes during different geologic period and is characterized by complex structure and a prolonged complex history

    秦嶺造山帶是經歷了不同期構造體制演化、具有復雜結構的復合型大陸造山帶。
  16. Studies on geology of the deposits and geochemistry of trace elements, rees, isotopes, ore - forming fluids show that the ore - forming materials came from varied sources. ore - forming materials of the tianbaoshan deposit was chiefly derived from different sedimentary rocks of the upper crust and orogen, while those of the daliangzi deposit mainly from the sinian dengying formation. meteoric waters were the major source of the ore - forming solution

    礦床地質特徵以及常微量元素、稀土元素、同位素、成礦流體等地球化學特徵的研究表明，礦床成礦物質是多來源的，天寶山礦床成礦物質主要來自上部地殼和造山帶各種沉積巖，大樑子礦床成礦物質主要來自震旦系燈影組地層；兩個礦床成礦溶液主要來自大氣降水；硫大部分來源於同時期的海相沉積地層（震旦系燈影組）中被細菌還原的海水硫酸鹽。
  17. The mantle source for the mesozoic mafic volcanic rocks in yanshan area exhibit transition character in space and time : the mantle source components vary from subduction - related metasomatic components and emi components through dominant emi components and slight subduction - related metasomatic components to emi components ; spatially, mantle source of the volcanic rocks show a regular variation trend from an enriched lithospheric mantle with emi - like signatures in the western shandong province through emi and / or subduction - related metasomatic components in yanshan area to subduction - related metasomatic lithospheric mantle in the hinggan - mongolian orogen

    燕山地區中酸性火山巖則來源於地殼，與玄武質巖漿底侵作用關系密切。 3燕山地區火山巖源區組分在時空上具有一定的演化規律：在時間上，從早期俯沖交代地幔及emi的參與，經中期以emi佔主導及極少量俯沖交代組分的階段，演變到晚期以emi為主，可能有少量軟流圈貢獻的組分，再到晚白堊世以軟流圈為主。
  18. More and more evidences suggest that the fold basement of yangtze block is an integral part of the grenville - aged orogen. the yanbian group, which resulted from post - grenville orogen, outcrops in the panzhihua area, sichuan province. hence, the studies on the geological features and geotectonic implications of the yanbian group can provide some clues to refine the position of yangtze block in rodinia

    揚子陸塊在rodinia中的位置是近幾年來的熱點問題，愈來愈多的證據顯示它的褶皺基底是grenville期造山帶的重要組成部分，鹽邊群是揚子陸塊褶皺基底的組成部分，研究它的地質特徵和大地構造屬性，可以為研究揚子陸塊在rodinia中的位置提供重要的地質線索。
  19. Quantitative calculation of trace element content for the residue after partial melting suggests that intermediate - mafic granulites outcropped in the dabie orogen are not the residue of partial melting

    殘留相微量元素定量計算結果表明，大別山現今出露的中基性麻粒巖不是部分熔融后形成的殘留體。
  20. Geologists and geophysicists have carried out substantial work on petrology, geochemistry, chronology and geophysics, et al., which yields important reference material and constrains for explanations of questions, such as the delamination and exhumation mechanism for the lower crust, models of the rapid uplift of himalayan orogen and deep subduction of india - eurasia plate. while only a little has been done to study the eastern syntaxis at present

    地質學家和地球物理學家已經對西構造結進行了大量的巖石學、地球化學、年代學和地球物理學等方面的研究，為解釋下地殼的拆沉、折返機制，喜馬拉雅造山帶的快速隆升和印度-歐亞板塊的大陸深俯沖模式等提供了重要的參考信息和約束條件。
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