側嶺 的英文怎麼說

中文拼音 [zhāilǐng]
側嶺 英文
celing
  • 側 : 側形容詞[方言] （傾斜; 不正） slant; sloping
  • 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
  1. From mangshan nature reserve to babaoshan, the central china species are clearly constantly reducing, but the central china species are clearly constantly increasing. this trend shows that the terrestrial mollusca fauna exists many differences in two areas

    從莽山到八寶山，陸生貝類體現出華中區成分明顯在減少，華南區成分明顯在增加的趨勢，這表明南嶺山脈南北兩側陸生貝類區系成分存在較大的差異。
  2. The hongqiling cu - ni ore deposit is located to the northern flank of a contacting zone ( the huifahe fault systems ) between the north china platform and the jilin - heilongjiang syncline system

    摘要紅旗嶺銅鎳礦床地處華北地臺與吉黑地槽系接觸帶輝發河斷裂北側。
  3. With the deuterium excess ( d - excess ) parameter, the conclusion that the tunnel location lies on the watershed between south and north geohydrology structures is validated

    利用氘過量參數，進而證實了隧道選址位於南北兩側水文地質單元的分水嶺之上的結論。
  4. The first phase involves the formation of thrusting and napping towards nww accompanied by extensive igneous activity and mineralization. the second phase corresponds to the development of asymmetrical small fold downwards north and south. the final phase the cenozoic is marked by strong brittle fractures activity resulting in the sharp heave of the landform of xiaoqinling aera

    太華群內的褶皺及南北兩側斷裂分析表明，小秦嶺燕山期至少經歷3期變形，第一期為sse nww向的褶皺變形作用；第2期為南北向正斷下滑剪切作用；第3期為脆性正斷作用。
  5. With blue - brick decorated walls, elaborating interior design, well - planned settings, elegant red - wood furniture, exquisite wood carvings, stained colorful glass, typical manzhou windows and barred windows, xiguan folk arts museum surely shows you the charms of southern china culture

    門口兩側則是水磨青磚墻，室內裝修陳設相當講究，名貴典雅的紅木傢具，精巧雅緻的木雕花飾，富有地方特色的滿洲窗和檻窗，裝嵌著書畫圖案的彩色玻璃，處處都散發著濃郁的嶺南韻味。
  6. Hole strategy ： avoid the bunker on the left of the green

    球洞攻略：要避開果嶺左側的沙坑。
  7. A good tee shot to the right of the bunkers will set you up for a short downhill second shot to the large green

    朝沙坑右側發個好球，會讓你再用一個下坡短桿就到達碩大的果嶺。
  8. Based on the theory of plate tectonics and the new knowledge of continental dynamics, this paper starts mostly with tectonic analysis and then makes a comprehensive view on the characteristic of stratum composition, gold mine mineralized, magmatic activity as well as ruptures activity to discuss the yanshanian tectonic evolution of the xiaoqinling area under the regional tectonic framework of qinling orogenic belt

    本文以板塊構造理論和大陸動力學研究的新認識為指導，採用以構造分析為主線，結合區內地層沉積、金礦成礦、巖漿活動以及南北兩側斷陷盆地形成演化等綜合分析，在秦嶺區域構造大框架下對小秦嶺燕山期的構造演化特徵進行探討。
  9. Pay special attention to 2nd shot if the front fairway is not in sight as there is a lake to the left of the fairway in front so the shot to the green must be exact

    第二桿如看不到前方球道情況要特別當心，前方球道左側有一湖泊，進攻果嶺要非常精準。
  10. Zijingguan fault zone is the main structure in taihang mountains that are located in the central part of 20 ~ 30 ne - striking daxing ' anling - taihan - wuling tectonic belt. it is composed of two diagonalized faults that are wulonggou - shanghuangqi fault located in the west and zijingguan - lishan fault in the east

    紫荊關斷裂帶是大興安嶺?太行山?武陵山構造帶中段太行山地區的主體構造，總體走向20 30 ，由西側的烏龍溝?上黃旗斷裂和東側的紫荊關?靈山斷裂左階斜列組成。
  11. From pattern of construct, we may know shanqian fault in north of xiaoqingling and luonan fault in south of xiaoqingling are delimitation faults, xunmadao fault is located in the middle of xiaoqingling, many great and middle ore deposits are distributed in both of xunmadao fault

    從構造格局上看，北緣的山前斷裂、南緣的洛南斷裂為小秦嶺的劃界斷裂，中部巡馬道斷裂的兩側分佈著許多大中型金礦床。陳耳金礦床位於巡馬道斷裂的北側，為石英脈型金礦床。
  12. May, 1997, weihai jinfeng real estate company of huaneng comprehensive industrial co. shandong branch began to fill out the sea and build the dam in barren beach and wild mountain range in the east of bathing beach, and fire the first battle of building golden bay hotel

    金海灣大事記1997年5月，華能綜合產業山東公司下屬威海金峰房地產公司在威海國際海水浴場東側荒灘野嶺之地上，開始填海築壩，打響了建設金海灣國際飯店的第一仗。
  13. Regional difference in lower - level temperature dv and pressure dv are greatly weakened and dv of llj is distinctly faint without the nanling ridge. this result show that nanling ridge acts as a critical role in the establishment of dv of the lower - level temperature and pressure, which give rise to the dv of llj in south china

    而當模式中僅僅去掉南嶺和武夷山山脈地形后，低層大氣溫度場日變化的區域性差異明顯變弱，梅雨低壓帶南側原南嶺山脈所在地的溫度日較差明顯減小，使得梅雨低壓槽與華南地區之間的南北向水平溫度梯度和水平氣壓梯度的日較差顯著變小，導致華南低空急流日變化的顯著減弱。
  14. Beijing longdi superior jade gallery. it is aside the ming tombs and badaling convenient for exit or entrance of jingchang highway

    北京龍地美玉館地處北京市昌平區西關環島東南側，毗鄰京昌高速公路出口，交通十分發達，是游覽明十三陵和八達嶺長城的必經之路。
  15. Situated at the foothills of wo king shan in ping che of ta kwu ling, cheung shan temple was built some two hundred years ago for worshipping the buddha

    位於打鼓嶺坪?禾徑山之山腳，長山之側，大約建於二百年前，為一座古樸的佛寺。
  16. Fish fauna and dividing of northern line of oriental region, at yali river upper reach of beijiang river

    南嶺南部北江源地魚類區系及東洋區北側界的劃分
  17. The jinan spring catchment is a complicated karst water system, the following major work had been done in order to discuss the proplem of spring protection and water supply. 1. having conduced exploration, experiment and comprehensive research, the southern boundary of the jinan spring catchment is determined to be the surface water divide ( changecheng mountain ), the source of yufu river and baedasha river ; the northern one is the carbonniferous and permian strata, together with the igneous rock mass in the north of jinan, and the eastern and the western ones are dongwu and mashan faults respectively, which are weakly permeable boundaries. the total area of the spring catchment is 1486 km2

    濟南泉域為一復雜的巖溶水系統，為了探討保泉供水問題，主要做了以下工作： （一）經過勘查、試驗和綜合研究確定濟南泉域邊界是：南邊界為玉符河、北大沙河源頭的地表水分水嶺（即長城嶺） ；北邊界為濟南北部的石炭、二迭系煤系地層和巖漿巖體；東、西兩側分別以弱透水的濟南東部的東塢斷裂和西部的馬山斷裂為邊界。
  18. The average altitude of mountain area is 4000 meters above sea level and 2900 - 3500 meters for valley area. the datong river passes south side the area

    之間，冷嶺與大坂山聳立於海北站的南北兩側，是世界海拔最高的草甸類型的實驗站，山地平均海拔
  19. These phenomena show that the fault has strongly activities at the same time. at that time tan - lu fault zone occurred a large - scale left - lateral displacement. the strike - slip movement on the tan - lu fault zone cau sed the zhangbaling uplifting which became source region and the hefei basin appeared strike - slip flexure at the west side of the fault

    說明了控盆斷裂?郯廬斷裂帶在該時期具有強烈活動，且以大規模走滑運動為主，郯廬斷裂帶的走滑使得東側張八嶺進一步快速隆升，仍構成沉積物源系統；在斷裂西側，合肥盆地因走滑而撓曲，形成沉積可容空間。
  20. Left side and in the direction of dongguan, guanchang east road, dalingshang town, dongguan

    東莞市大嶺山鎮莞長路向東路段往東莞方向左側
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