賀蘭山 的英文怎麼說
中文拼音 [hèlánshān]
賀蘭山
英文
helan shan-
Damocles faced the wall and meditated for ten years and got the buddhist allegory finally, i sit there for two hours and thirty six minutes, at 7 : 29 pm, i made a decision at last : i need to be a graduate student, after a full pack of smokes of helan mountains brand had been finished by me
達摩面壁十載終于悟得憚機，我在靜坐了兩小時三十六分七點九二秒、抽完了整整一盒賀蘭山牌香煙之後我終于做出了一個決定：我要考研！The phreatic groundwater in the diluvial fan in front of the helan mountain is mainly recharged by precipitation and the lateral flow from the helan mountain ; the phreatic groundwater both in the diluvial fan of the qingtongxia gorge and in the fluvial plain is mainly recharged by the influent seepage of irrigation water from the yellow river
賀蘭山洪積扇單一潛水主要接受山區側向徑流及大氣降水補給；青銅峽洪積扇單一潛水及沖湖積平原上覆潛水，主要接受黃河灌溉水的入滲補給。The main uplift age is in eocene and isochronous to that of the formation of yinchuan graben
賀蘭山的主隆升期始於始新世，與銀川地塹的形成同步。Abstract : according to the observation of the number concentration spectrum and the mass concentration of atmospheric aerosol, tsp and its particle size distribution, micrometeorology, and the solar spectroscopic radiation, even the neutron activation treatment of sand dust samples in helan mountainous area, the formation law of sandstrom, dust and sand blowing weather and the characteristics of climatic variation in this area and the influence of helan mountain are counted and analysed
文摘:利用賀蘭山地區沙塵暴歷史資料和綜合觀測資料，對大氣背景、浮塵、揚沙和沙塵暴發生期間的大氣氣溶膠數濃度譜、質量譜、大氣總懸浮顆粒（ tsp ）及粒徑分佈、微氣象、分光日射觀測以及沙塵樣品進行中子活化處理，分析了該地區浮塵、揚沙和沙塵暴形成規律，氣候變化特徵和賀蘭山的影響。According to the observation of the number concentration spectrum and the mass concentration of atmospheric aerosol, tsp and its particle size distribution, micrometeorology, and the solar spectroscopic radiation, even the neutron activation treatment of sand dust samples in helan mountainous area, the formation law of sandstrom, dust and sand blowing weather and the characteristics of climatic variation in this area and the influence of helan mountain are counted and analysed
利用賀蘭山地區沙塵暴歷史資料和綜合觀測資料，對大氣背景、浮塵、揚沙和沙塵暴發生期間的大氣氣溶膠數濃度譜、質量譜、大氣總懸浮顆粒（ tsp ）及粒徑分佈、微氣象、分光日射觀測以及沙塵樣品進行中子活化處理，分析了該地區浮塵、揚沙和沙塵暴形成規律，氣候變化特徵和賀蘭山的影響。Analysis on the 060714 rainstorm floodwater east foot of helan mountain in ningxia
寧夏賀蘭山東麓060714暴雨洪水分析A large amount of data of the latest regional geoglogy and the latest correlation data of layers and rock formation have been quoted, and a description of distribution of crystalline basement, formation, evolution as well as the distribution characteristic of the fracture belt of ordos basin have been made in this paper, and the paper also pointed out that the g - layer which lies between the base of the basin and tg reflector, is the extension of basinward of guandaokou of jixian system. the layer of changcheng system and jixian system, which had been divided before, can be correlated with the exposed huangqikou group and wangquankou group in helan mountain, and divided into qingbaikou system. so, the paper denied the viewpoint of the existence of aulacogen in hutuo period and middle proterozoic in this basin
文中引用了大量最新的區域地質資料和最新的地層、巖系劃分對比資料，對鄂爾多斯盆地結晶基底的巖系分佈、形成、演化以及斷裂的展布特徵進行了描繪，並指出盆地基底與tg反射層之間的g層是薊縣系官道口群向盆地的延伸，盆地中原劃分的長城系、薊縣系地層可以和賀蘭山出露的黃旗口組、王全口組對比，亦劃歸青白口系，從而否定了鄂爾多斯盆地存在滹沱期坳拉谷和盆地中有中元古坳拉谷發育階段的看法。The present thrust nappe structure formed in late jurassic according to comprehensive analysis of sedimentary, structure and fission track tesing result
據沉積、構造和裂變徑跡測試結果綜合分析認為，現今所見的賀蘭山逆沖推覆構造形成於晚侏羅世。The tholeiite with late trassic age has been found in helanshan area on the north part of western margin of ordos basin
在盆地西緣北部賀蘭山地區，發現典型拉張環境形成的拉斑玄武巖，測年時代為晚三疊世。Late triassic to mid jurassic strata in which owns the good coal of van ' an formation distributes widely with huge thickness in helan mountain
在賀蘭山的中生代地層中，晚三疊世-中侏羅世地層分佈廣泛、厚度巨大，中侏羅世延安組為賀蘭山的優質含煤層。Structure characteristics show that helan mountain was in extensional environment in late triassic and no obvious compressional evidence in early - mid jurassic
構造特徵分析表明，在晚三疊世賀蘭山地區處于拉張環境，早中侏羅世構造環境亦無明顯擠壓跡象。The study on the structural feature opened out by the non - seismic ( mt ) profile of xiaonangou in qinglong mountain on the west edge of ordos basin and the seismic profile across helan mountain shows that a series of thrust blocks - qinglong - luoshan - nioushou - helan mountain, were the thin - skin structure formed by the westward compression of ordos block and the dextral shear of alashan block
通過對盆地西緣青龍山南端小南溝的非地震mt剖面以及橫穿賀蘭山的地震剖面揭示的構造形態研究認為，盆地西緣一系列推覆體青龍山?羅山?牛首山以至賀蘭山是由於鄂爾多斯地塊向西推擠同時與阿拉善地塊的右行運動所產生的「薄皮構造」 。On the basis of theoretical studies and discussion, combining the construction of the forest resource investigation management information system of ningxia forest information platform, we selected suyukou manage station of ningxia helan mountain nature protect bureau as an example and realized the automatic and remote user authority management of forest resource second class investigation data
在理論研究和討論的基礎上，結合寧夏林業信息平臺項目森林資源調查管理信息系統建設，選擇寧夏賀蘭山自然保護局蘇峪口管理站為試點進行應用例證。實現了森林資源二類調查數據庫的動態管理以及遠程用戶權限管理。Helan shan is located in the northwest of china, 37. 0 - 3 9. 6 n. and 105. 3 - 106. 8 e. its altitude ranges from 1 600m to 3 556m. the cosmo politan genera and species of higher fungi from helan shan amount to 64. 1 % and 1 9. 8 % respectively. most of them are saprophytic taxa of broad physiological adap tability. the genera belonging to the boreal areal type make up 35. 9 %, and species 52. 7 %, which indicates that the higher fungi flora of the helan shan are dominan ted by boreal elements. no tropical genera and species have been found there. the elements of europe - asia add up to 11. 5 %, while the elements of east asia - north america amount to 9. 9 % which shows close relationship of fungi between the helan shan and the above two regions. the elements of china - japan amount to 3. 1 %, whic h reflects some relations of higher fungi between china and japan. few elements e ndemic to helan shan were found but with further investigation and study, it is p ossible to find some considering its isolated geographic location and varied top ography
賀蘭山高等真菌區系地理成分中，世界性分佈屬佔64 . 1 % 、種佔19 . 5 ，他們多為適應性強的腐生菌類;歐亞北美分佈屬佔35 . 9 % 、種佔52 . 7 % ，未發現熱帶分佈的屬或種，充分顯示出該地區真菌以北溫帶分佈成分為主的特點;歐亞分佈種佔11 . 5 % ，東亞北美分佈種佔9 . 9 % ，表明該地區真菌區系與歐洲、北美洲的密切聯系;中國&日本分佈種佔3 . 1 % ，可見本地區和日本在真菌區繫上也有著聯系;本地區特有成分較少，但從賀蘭山特殊的地理位置、相對孤立的山體和復雜的地形分析，隨研究工作的深入，很可能有一些山的分佈的特有成分被發現.賀蘭山真菌區系成分與鄰近的內蒙古大青山相比較，共有種多達57種，而與地處亞熱帶向熱帶過渡的湖南莽山相比較，共有種僅有12種，更進一步說明本地區深居北溫帶，真菌區系以泛北極成分為主的特色It has regular flights to beijing, shanghai, guangzhou, xian and chengdu. the main tourist attractions in yinchuan or nearby are haibao pagoda. mausoleums of the western xia emperors, the nanguan mosque and rolling bell pass in the helan mountains
銀川是寧夏回族自治區的首府，也是交通樞紐，自銀川至北京上海廣州西安成都有定期航班，銀川及其附近旅遊景觀有海寶塔西夏陵墓，獻花清真大寺，賀蘭山小滾鐘口等。000 groups of ancient rock paintings with more than 20, 000 single figures are distributed on several mountains from the helan ridge in the west of ningxia in the north to zhongwei in the south
在寧夏西部賀蘭山脈北起石嘴山，南至中衛的多個山口，分佈著1000多組，單個圖案超過2萬個的古代巖畫。The maowusu desert and the tengeli desert are important deserts in the north china
摘要毛烏素沙地與騰格里沙漠位於賀蘭山東西兩側，是中國北方重要的沙漠之一。According to the analysis of newly - compiled 1 : 2000000 gravity and magnetic data, there exist three ( eastern, central and western ) deep tectonic areas in northern china, which are hounded in the east by helan mountain - liupan mountain - longmen mountain line and in the west by xingxingxia - ruoqiang line
摘要根據新編制的1 : 200萬重磁資料分析，中國北部深層存在東、中、西3個構造區，其東界在賀蘭山六盤山龍門山一線，西界在星星峽若羌一線。The control tactics on the cucumber root - knot nematodes disease in greenhouses of helan mountain farm in ningxia
寧夏賀蘭山農牧場溫棚黃瓜根結線蟲病綜合防治對策The diversity and spatial distribution of plant communities in the helan mountains
賀蘭山植物群落類型多樣性及其空間分異分享友人