焉耆 的英文怎麼說

中文拼音 [yānqí]
焉耆 英文
karasahr
  • 焉 : [書面語]Ⅰ代詞1 （跟介詞「于」加代詞「是」相當） here; herein 2 （哪裡; 怎麼） how; why Ⅱ副詞（乃;...
  • 耆 : Ⅰ形容詞1 （年老的） very old; elderly2 （強橫） tyrannicalⅡ名詞1 （六十歲以上的人） over sixty ye...
  1. Yanqi basin is stituated between tarim basin and tarpan - harmi basin. its petrolenm system underwent the formation and destruction during jurassic - cretaceous, the activation and reconstruction during tertiary - quaternary

    焉耆盆地位於塔里木盆地和吐哈盆地之間，其含油氣系統經歷了侏羅紀-白堊紀的形成與破壞階段和第三紀-第四紀的活化與再建階段。
  2. 4. combined with the analysis of the hydrocarbon - generation history, hydrocarbon maturity, fluid inclusions, authigenic illites isotopes chronology and trap forming history, it affirms that jurassic reservoirs formed in three phases : the first in the late jurassic, which was the primary pool - forming phase, the second in the telophase of jurassic to cretaceous, which was the adjusting - destroying phase, the third in tertiary, which was the secondary phase

    4 、採用烴源巖生烴史、油氣成熟度、流體包裹體、儲層自生伊利石同位素年代學和圈閉演化史綜合方法，確認焉耆盆地侏羅系油氣藏具有三期成藏的特點，第一期發生在侏羅紀晚期，是盆地的主要成藏期，第二期為侏羅紀末至白堊紀的油氣藏破壞、調整和再分配期，第三期發生在第三紀，是盆地的次要成藏期。
  3. If a thorough research on the remainders of tocharian a and b as well as a great many of references in chinese are made, the situation of budduist belief in agni and kuci from the establishment of tang dynasty ( in 618 ad ) to the third year of dachong chiangfu in song dynasty ( in 1010 ad ) will be fully understood

    摘要人們如果運用大量的吐火羅文a 、 b殘卷的資料和漢文相關材料進行詳盡考察，就會知道從唐朝建立到宋大中祥符三年（ 1010年） 400年前焉耆與龜茲的佛教信仰情況。
  4. Yanqi basin, located in the northern wing of the " v - type " thrust - fold belt, is related to the reversion of the kuluketage aulacogen

    因此庫魯克塔格裂陷槽的構造反轉是焉耆盆地構造變形的主要力學來源。 2 、描述了盆地內的構造樣式。
  5. Yanqi basin is an intermont basin of tian shan, there is a nww trending right lateral strike slip active fault in southwestern basin, its maximum slip distance is 210m, and slip rate is about 10mm / yr, moreover, there is a west - east trending active anticline along northern basin

    焉耆盆地是一個天山山間盆地，盆地西南緣發育一條走向北西西的右行走滑活動斷層，最大走滑距離為210m ，走滑速率約10mm / yr ，盆地西北緣發育走向近東西的活動褶皺。
  6. The tectonic framework and border faults of the basin were related to the basement configuration. 3. based on the regional tectonic setting and sedimentary sequence evolution, the structural physics modeling and balance profile reversion are first carried out

    焉耆盆地前中生代基底硬塊的形態及內部結構對中新生代盆地的形成及形變具有重要的控製作用，現今盆地的構造格局和重要的邊界斷層都與基底的結構有關。
  7. The phase of reservoir formation can be the period when the basin is the subsidence such as the reservoir of shixi 2 well, shi 002 well, shi nan 4 well, cai san 2 well in zhungeer basin, tuo 76 well ; the phase of being reservoir can be the period when the basin is the uplift such as the reservoir of songliao basin, miyang basin, dongpusag, eerduosi basin, yaqi basin

    油氣的成藏期可以在盆地沉降期，如準噶爾盆地石西2井、石002井、石南4井、彩叄2井的油氣藏；也可以在抬升剝蝕期，如松遼盆地、泌陽盆地、東濮凹陷、鄂爾多斯盆地、焉耆盆地的部分油氣藏。
  8. Ideas on the petroleum geology conditions of yanji basin

    對焉耆盆地油氣地質條件的認識
  9. The time in yanqi

    焉耆的時間
  10. Relations between jurassic inclusions and oil amp; gas migration amp; accumulation in yanqi basin

    焉耆盆地侏羅系包裹體與油氣運聚期次的關系
  11. Yanqi basin is a typical reformed residual basin where several oil and gas fields with commercial value and some product energy have been found in recent years

    焉耆盆地是一典型的改造殘留盆地，在其中已發現多個有商業價值和一定規模產能的油氣田。
  12. Interpreting the remote sensing images and verifying the facts in south tian shan, we studied active tectonics of yanqi basin, aheqi fault and kuche depression

    通過遙感圖像和野外實際驗證相結合的研究方法，對南天山焉耆盆地、阿合奇斷裂和庫車坳陷的活動構造進行了研究。
  13. Aiming at the abnormal phenomenon that water content of some production wells with decline along with the time in the yanqi basin, this paper puts forward an argument that low water - cut oil layers exist in the low permeability formation

    摘要針對焉耆盆地部分生產井，在投產過程中存在隨時間的延長含水率下降的反常現象，提出了低滲地層存在低含水油層的觀點。
  14. Beginning form relation of basin - mountain, the tectonic evolution and the petroleum system and pool - forming process have been studied with the integration of structural physics modeling, balance profile reversion and other new testing technology. the main innovative achievements of the dissertation can be summarized as following : 1. on the basis of comprehensive analysis of yanqi basin relationship to tianshan orogenic belts, it was suggested that kuluketage faulted - upheaval was an aulacogen in early paleozoic, which undergone multiple opening - closing along with tianshan orogenic belts, and suffered extensively compressing in late hercyhian cycle and formed a " v - type " thrust - fold belt

    論文總的指導思想是以現代石油地質理論為基礎，以整體、動態、系統、綜合分析為原則，以成盆?成烴?成藏研究為主線，運用正、反演相結合的殘留盆地油氣成藏系統評價思路，採用構造物理模擬、平衡剖面復原和多種測試新技術，從盆山耦合關系切入，研究含油氣系統成藏要素及其相互作用過程，探討油氣成藏主控因素和油氣分佈的有序性，取得如下創新性成果和認識： 1 、系統分析了焉耆盆地形成演化與天山構造帶的關系，提出盆地南側的庫魯克塔斷隆在早古生代為一大型裂陷槽，之後隨著天山構造帶的演化，經歷了多次開合運動。
  15. From late - mesozoic to eogene, northern edge of mesozoic tarim basin became uplift gradually and the sedimentary range migrate to south. present u ' erdusi basin, yanqi basin, kumishi basin became uplift one by one and experienced strong deformation, denudation and reformation and some strata are denuded

    中生代晚期到早第三紀，塔里木中生代盆地北緣逐步隆升，沉積范圍向南遷移，今尤爾都斯、焉耆和庫米什盆地范圍先後隆升，缺失沉積，並造較強烈變形、剝蝕等改造。
  16. By the integrated research on sedimentary - tectonic evolution and reformation of yanqi basin and the comparison of die evolution of northern tarim basin and tianshan belt, the result shows that yanqi basin experiences five evolution stages include forland basin ( t2 - 3 ), extensional basin ( j ), compression and denudation stage ( k ), regional depression stage ( e ), and broken intracontinental forland basin ( n + q ). at mesozoic, kuche basin and yanqi basin belonged to a unity

    對焉耆盆地沉積-構造演化及改造綜合研究，並與塔里木盆地北部及天山構造帶演化對比表明，今焉耆盆地先後經歷了周緣前陸盆地（ t2 - 3 ） 、伸展盆地（ j ） 、擠壓剝蝕階段（ k ） 、區域沉降（ e ）和破裂陸內前陸盆地（ n + q ）五大演化階段。
  17. The research on the lithologjcal and mineral parameters and the sedimentary fades of different periods of mesozoic strata shows that the northern boundary of yanqi basin is almost the same, but great differences existed in the southwestern yanqi basin, that is, the sedimentary range of mesozoic original basin is more bigger than present basin

    中生代地層各種巖礦參數和各時代沉積相研究表明，今焉耆盆地北部與原始沉積邊界較為相近；西南和南部的邊界今古差異較大，即在中生代原始盆地沉積范圍要比今盆地范圍要廣。
  18. Its results approve the yanqi basin is a mesozoic - cenozoic compressive basin ( revival foreland basin ) in the tianshan composite orogenic belts. the tectonic evolution in mesozoic - cenozoic can be divided into three stages : the weakly compressive stage in the early to middle jurassic, intensively compressive stage in the late yanshan cycle, and face to face compressive stage in the himalaya cycle

    根據構造變形及盆地沉積特徵，論述了焉耆盆地中、新代構造演化的三個階段，即早、中侏羅世弱擠壓階段、燕山晚期強烈擠壓階段和喜山期對沖構造發育階段。
  19. By the comparison of the residual strata, sedimentary evolution and source rocks among kuche depression, kumishi basin, u ' erdusi basin and yanqi basin, die result shows that mesozoic sedimentary environment of these basins has tightly relationship which all belongs to tarim basin

    通過將塔里木盆地北部庫車坳陷地層、沉積演化和烴源巖以及庫米什盆地、尤爾都斯盆地殘留中生代地層與焉耆盆地的對比研究認為，庫車、焉耆、尤爾都斯及庫米什盆地在中生代沉積環境彼此相關，均屬大型塔里木中生代盆地的有機組成部分。
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