嶺古 的英文怎麼說

中文拼音 [lǐnggǔ]
嶺古 英文
mineko
  • 嶺 : 名1. （頂上有路可通行的山） mountain; ridge 2. （高大的山脈） mountain range 3. （專指大庾嶺等五嶺） the five ridges
  • 古 : Ⅰ名詞1 （古代） antiquity; ancientry 2 （先哲的遺典、道統） books or orthodoxies of ancient sages...
  1. On the basis of analogic methodology, the deep gas resources of the basin is evaluated as 1116. 144 billion cubic meters, which is mainly distributed in the zones of xujiaweizi, miaotaizi, changling, yingshan, and gulong

    根據松遼盆地深層天然氣區帶地質評價參數取值標準，進行區帶地質評價，並通過與刻度區類比，得出深層天然氣資源量為11161 . 44 10 ^ 8立方公尺，主要分佈在徐家圍子、廟臺子、長嶺、鶯山、古龍等區帶中。
  2. 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
  3. From the middle devonian to the early carboniferous, the spores of the shishuyuan trough in the northern part of eqm and those of the nanwan trough in the southern part of eqm belonged to the south china province, and the late devonian corals, brachiopods, plants, and the early carboniferous fusulinids of the xichuan shelf were from the south china province

    在中泥盆世至早石炭世，東秦嶺北部柿樹園海槽與東秦嶺南部南灣海槽的孢子及浙川陸棚的晚泥盆世珊瑚、腕足類和古植物及早石炭世（蟲? ）屬華南生物省。
  4. 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洋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洋溝弧盆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。
  5. However, this railway is climb from siliguli of the above sea level of 121 meters to darjeeling of the above sea level of 2, 044 meters

    海拔119米的西里古里站至海拔2 ， 044米的大吉嶺站的全長82 . 1公里，是世界中有名的高原鐵路之一。
  6. The main stratums contain gold element are yanlinggou team of qinling group and huoshengmiao team of erlangping group in sub - paleozoic, the lithologise that are the best related with gold mineralization are graphite marble and dolomite marble in yanlinggou team and splite marble in huoshenmiao team

    主要賦礦地層中元古界秦嶺群雁嶺溝組及下古生界二郎坪群火神廟組，與金礦化關系最為密切的巖性分別為雁嶺溝組石墨大理巖、白雲石大理巖及火神廟組細碧巖等。
  7. The nutrients content, the number of microorganism and activity of edaphon in soil of gutongling 4 - year - old, 10 - year - old and 16 - year - old organic tea garden were measured

    摘要對湖南湘陰縣蘭嶺茶廠古桐嶺不同種植年限的4年生、 10年生、 16年生有機茶園，分別進行了土壤養分含量、微生物類群數量及活性測定。
  8. You will drive past the great divide watershed of the american continent to arrive at mammoth hot springs to view the multi - colored lava flow from extinct volcanoes, examine fossilized trees, and catch the glimmer of beautiful lakes in the secluded woods

    穿越美國大陸的分水嶺，到達公園最北的mammoth hot springs ，五顏六色的梯田，溫泉及滾燙的熔巖，石化的古木，碳化的火山口，林間的小湖，泛上裊裊的輕煙，宛如神話世界。
  9. There are eight large deserts and four large sandlots in china. the area of keerqin sandlot is biggest of the four sandlots. and it lies in the west part of northeast china, the transition zone of inner mongolia plateau and northeast plain, and is the transition areas of daxingan mountain knap zone and west liao river plain, the interleaving section of agriculture and pasture in east china

    我國有八大沙漠和四大沙地，科爾沁沙地在四大沙地中面積最大，它位於我國東北地區西部，地處內蒙古高原向東北平原的過渡帶，是大興安嶺西南丘陵區向西遼河平原過渡區和我國東部的農牧交錯區。
  10. ( 3 ) jianchaling ultrabasic intrusion belongs to magnesian ultrabasic simple rock - body, close related with yangzi block in space, which formed in the interim of proterozoic active tectonic zone to phanerozoic orgenic belt

    （ 3 ）證實煎茶嶺超基性巖體為含鐵的鎂質超基性單式巖體，空間上與揚子地塊關系密切，形成於新元古代由元古宙活動帶向顯生宙造山帶過渡時期。
  11. The western architecture always provide popular styles from europe, such as neoclassicism, eclectic, and romanticism styles among others. on the chinese architecture field, there were always the " ling - nan " architecture style in macau city

    當時西式建築都是沿用歐洲流行的風格建造，有新古典主義、折衷主義及浪漫主義等風格；中式則沿用一貫的嶺南風格建築。
  12. The number of species in the southern slope of qinling mountain was most abundant because of distribution of some palaearctic species to the top of qinling mountain, especially species of oedipodidae, another reason may b. e the large number of endemic species in this area

    秦嶺南坡種類最多，主要是有部分古北界的種類滲透分佈在中、高山地帶，特別是斑翅蝗科的種類，另外還有部分特有種。
  13. The article makes parallel research on the archaeological culture of the yun - gui plateau and the south of the five ridges from the era of paleolith to the xi han dynasty, and discusses the intercommunication and interaction of the early culture between these 2 aspects

    摘要本文通過對舊石器時代至西漢時期雲貴高原與嶺南考古學文化的對比研究，探討二者之間早期文化的相互交流與影響。
  14. At the same time, it is proved again that jianchaling rock - body intruded in new proterozoic

    並佐證了煎茶嶺巖體確為新元古代形成的超基性巖體。
  15. As far as the relationship between gmnr flora and other flora outside of guangdong province, the analysis shows that gmnr is more similar to jianfengling than to lushan mountain an jiulong mountain. so, the author thinks gmnr is floristically a transitional zone from the tropic to subtropic, and it should be a part of east - asia region, belonging to the " paleotropic kingdom "

    同時，與省外地區植物區系的比較結果表明，古兜山等廣東地區與與熱帶區系海南尖峰嶺植物區系的聯系比與中亞熱帶植物區系的廬山、九龍山植物區系的聯系要密切些（甚至強于與車八嶺植物區系的聯系） ，進一步證明了本植物區系熱帶向亞熱帶過渡的性質，為華南省植物區系的組成部分，隸屬于古熱帶植物區。
  16. On the basis of the types of sand stone, light and heavy mineral associations, planimetric map of sedimentary facies and directions of palaeoflow, it is considered that detrital material of terrigenous deposit of chang6 - 8 oil - beds in this area come from southwest provenance, northeast provenance, west provenance and south provenance, respectively, which are the denudation area of huating - longxian county in southwestern, yinshan ancient land in the northern, the denudation area of yantong mountain and tongxin to the west of yangjiajuzi - yinjiacheng county and qinling ancient land in the southern

    根據砂巖類型、輕、重礦物組合、沉積相帶平面展布及古水流方向等特徵的分析，認為研究區延長組長6 ? 8油層組陸源碎屑物質來自西南、東北、西部和南部四大物源區，分別為西南華亭?隴縣一帶剝蝕區，北部陰山古陸，西部的楊家咀子、殷家城以西的煙筒山、同心地區剝蝕區和南部秦嶺古陸。
  17. In kurseong town dec. 1978 kurseong is the biggest town of midway

    Kurseong是從西里古里至大吉嶺段半路最大的街市。
  18. 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。
  19. On the basis of the analyses of peripheral ancient land, types of sand stone, light and heavy mineral associations and directions of palaeoflow, it is considered that detrital material of terrigenous origin of the upper palaeozoic in this area come from south provenance and north provenance, respectively, yinshan ancient land in the northern and east qinling ancient land in the southeastern

    根據盆地周緣古陸、砂巖類型、輕、重礦物組合及古水流方向等特徵的分析，認為研究區上古生界陸源碎屑物質來自南、北兩大物源區，即北部的陰山古陸和東南部的東秦嶺古陸。
  20. Paleozoic paleobiogeographic provinces and paleogeographic changes in the eastern qinling

    東秦嶺古生代古生物區與古地理變遷
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