溝川 的英文怎麼說

中文拼音 [gōuchuān]
溝川 英文
mizogawa
  • 溝 : 名詞1 （挖掘的水道或工事） channel; ditch; gutter; trench 2 （淺槽;似溝的窪處） groove; rut; furr...
  • 川 : 名詞1 （河流） river; stream 2 （平地; 平野） plain: 800里平川 a vast eight hundred li plain; 米...
  1. Comprehensive study indicates the dark, 50 - 300 m thick upper permian series, which is rich in the organic material ( om ) and biota, is beneficial to formation and protection of petroleum and natural gas. moreover the stratigraphy possess with better reservoir ability. the reservoir distributed in shallow glacis along beichuan tongkou - guangyuan changjianggou, he 12 well - she 1 well - jiange - cangxi yongningpu - long 4 well - bian 1 well in wujiaping stage and in platform edge beach along beichuan tongkou - jiangyou shuigentou - jiange - cangxi yongningpu - nanjiang

    綜合以上，本文認為研究區上二疊統地層厚50 ? 300m ，顏色較深、生物含量多、富含有機質，並且該套地層自形成后，大多直接進入埋藏成巖環境，是一套十分有利於油氣的形成與保存的地層；同時該套地層的局部層段具有一定的儲集性能，在吳家坪期儲層主要分佈在北川通口?廣元長江溝、河12井?射1井?劍閣?蒼溪永寧鋪?龍4井?扁1井一帶，在長興期儲層主要分佈在北川通口?江油水根頭?劍閣?蒼溪永寧鋪?南江一線。
  2. Chengdu to the kalong ditch 310 kilometers, the kalong ditch to amounts to the ancient glacier 112 kilometers

    成都至卡龍溝310公里，卡龍溝至達古冰川112公里。
  3. And reaches the ancient glacier state of roads from chengdu to the kalong ditch scenic are a extremely to be all good, to scenic are a in for pitch / cement road surface

    從成都至卡龍溝景區及達古冰川路況都非常好，到景區內均為柏油/水泥路面。
  4. Do not walk onto glaciers or large snowfields without the proper equipment and experience ; there is a real danger of falling into hidden crevasses

    想徒步冰川到四川海螺溝就可以了，至少發生意外救援都容易和快捷得多。
  5. At the surface of the pollen grains there are three types of aperturates, including three porates type, three colpates type and three porate - colpates type ; and four types of sculpture, namely, reticulate, striate, striate - reticulate and verrucate. the upper epidermal cells of the leaves of 12 species plants are detected with hpias - 1000 image analytic system through the treatment of binarization, and the experimental methods are proved stable. the results indicated that the waviness of the anticlinal walls ( sfc ) and the ratio of the feret ' s diameter ( slf ) of the epidermal cells of the middle lamina in the third node of leaves starting from the lowerest part of the stem have a relative constant range and could distinguish from each other. oieanolic acid, l, 5, 8 - trihydroxy - 3 - methoxyxanthone and swertiamarin are separately detected on the tlc, and the different chromatogram of various plants can be considered as characters of identification. the contents of oleanolic acid in 12 species of plants are determinated by hplc, but among the different plants and botanical organs their contents are different, and the highest content in flowers

    本文對川鄂產獐牙菜屬藥用植物資源進行了野外調查、標本採集和鑒定，對12種乾燥藥材的性狀進行了描述，提供了可以鑒別的特徵。通過掃描電子顯微鏡觀察的12種本屬藥用植物的花粉粒均為單粒花粉，萌發孔有3孔型， 3溝型和3孔溝型三種類型；表面紋飾包括網狀紋，條狀?網狀紋，條狀紋和瘤狀紋四種類型。用hpias ? 1000高清晰度彩色病理圖文分析系統對葉片上表皮細胞作圖像分析，並進行方法學研究，結果表明，同種植物莖上第3節葉片中段主脈和第1側脈之間葉上表皮細胞垂周壁彎曲程度sfc值和細胞縱、橫向直徑的比值slf值，種間有顯著差異，每種都有相對恆定范圍值。
  6. The author presume the original physiognomy of jiuzhai valley, and acknowledged changhai valley was a surface - water with uniform waterpower, the rize valley was a branch of it but the inequality rise of lithosphere, the deposit of earthquake landslides debris flows and falling or glacier blocked the river - way, furthermore, the flow water with high content of ca ( hco3 ) 2, so tufa dyke formed and evolvement the present dyke of lakes the present physiognomy formed on the base of those 2

    由於地震、滑坡、泥石流引起的堆積物和冰川作用形成的冰磧物堵塞河道，再加上構造運動造成地殼的不均勻抬升，九寨溝的這種獨特的地質環境以及高含ca （ hco _ 3 ） _ 2的巖溶水流作用下，為caco _ 3沉積創造條件，沉積的caco _ 3加高、連接最終形成灰華堤壩，使湖泊的形成成為可能。
  7. Lie of the mountain precipitous vigorous and rough, strange mountain different peak, glacier and cliffside spring in the gully, size high mountain lake and wide one forest, meadow, various kinds of exotic flowers and rare herbs, rare birds and animals, form scene, mountain region of plateau, that show unique characteristics

    四姑娘山山勢陡峭蒼勁粗獷，山溝內奇山異峰冰川飛泉，大小高山湖和廣闊的森林草地，各種奇花異草珍禽異獸，構成了獨具特色的高原山地風光。
  8. The value of containing soil and water is only 5. 1 percent and 0. 7 percent in total ecosystem value respectively in ansai county and wuchuan county, however in zhifanggou valley the ration gets to 60. 3 percent. so some measures of increasing the vegetation and strengthening the service function should be taken continuingly

    但是，區域的水土保持服務功能還很低下，安塞縣、武川縣水土保持價值占總服務價值的比例分別為5 . 1 、 0 . 7 ，紙坊溝流域則達到60 . 3 。
  9. There are parallel grooves or scratches produced when the glacier moved with its load of embedded rock on the lower side.

    冰川帶著低處嵌著的巖石活動時，形成了這些一條條平行的溝槽或擦痕。
  10. On the guanyin top, we look down around. northwest part was shayu valley. the rivers, villages, fruit trees and terraced fields were buddhism guanyins skirts

    登臨觀音頂，俯瞰四野，西北面沙峪溝河川村舍果林梯田，依偎腳邊，是觀世音菩薩的裙裾。
  11. The outcome shows that naixiong crude drugs is little iightcoioured, has a protruding terminal bud, has little fragrance ; the bodily form of shanchuanxiong is emacicated and small sized, has a dry and decayed gully in the middle part, has a strong fragrance the wooden degreen of naixiong " s fibre is at a lower stage, and thas small oil drops ; but chuanxiong and shanchuanxiong ' s are at a higher stage, and they has oil drops in abundance

    對奶芎、山川芎與川芎進行了生藥學研究：奶芎藥材顏色較淺，頂端有一突起的頂芽，氣微香；而山川芎體形枯瘦，個體較小，中心常有枯朽狀溝槽，氣香。奶芎組織中纖維木化程度低，油滴較少；而川芎、山川芎纖維木化程度高，油滴較多。
  12. Based on arcgis, discovery and gocad software platform, we built a 3d geological model of the yanjinggou anticline using 3d seismic data in the area

    文中基於arcgis 、 discovery以及gocad等三維軟體平臺，對川西鹽井溝地區地震資料進行精細的解析，得出鹽井溝背料是一個典型的三剪斷層傳播褶皺，並建立了它的三維模型。
  13. Because the structural interpretation of the 3d model only is of non - uniqueness and uncertainty due to geometric constraint, the finite strain analysis was also applied in the structural interpretation. 184 oriented samples have been drilled at 18 sampling sites in yanjinggou, western sichuan

    在川西鹽井溝地區18個采樣點鉆取了184塊定向巖心樣品，通過磁組構的分析結果發現，鹽井溝地區的磁組構基本上都是弱應變的初始變形組構，褶皺前翼應變強度比后翼略強。
  14. 1 the results of minshan mountains black bear population viability analysis : minshan mountains situate in the border of sichuan and ganshu province, north is from min county of ganshu, south to dujiangyan of sichuan, west is from shongpan langmu temple and maoergai, east to yanchang and wudu of ganshu with qinchuan of sichuan, the administrative area includes wen county, kang county, cheng county and liangdang of ganshu

    行政區劃包括甘肅的文縣、康縣、成縣、兩當；四川的平武、青川、北川、安縣、什邡、綿竹的全部，以及甘肅的武都和四川的九寨溝兩縣南部，四川松潘、茂汶兩縣東部，汶川縣、都江堰市、彭州市和北部地區。
  15. Mt. haizi is well - grown due to glacier process in the a quarterary period age of man. a vast of longstanding glacier remains stretch in the distance with steep valley wall and flat valley bed. the valley is typically formed " u " shape

    海子山第四世紀冰川作為極為發達，古冰川遺跡分佈廣泛，在夏塞峰德南坡幾條溝均為古冰川穀，谷壁陡立，谷底平坦，為典型的「 u 」型冰川。
  16. Abstract : the authors discuss roundly source of loose earth fo r impact - deposit debris flow to develop taking pingchuan debris flow, one of the quite typical impact - deposit debris flows in southwest sichuan province ， as an example in this paper. on the basis of detailed investigations in - situ, geotechn ial testing in lab and theory analysis, all results indicate obviously that moder ate and bulky loose earth in giant debris flow situating in southwest sichuan mo untainous area are main institute, whose tribulation are consistent with landform s. loose earth locating in mid - forepart catchment are quite unstable, so often be comes main source of loose earth of debris flow. formation of loose earth is cont rolled principally by geologic and geotechnical environment while human actions is the secondary factor for loose earth to form. in many times, human actions prov ide loose earth through loose earth stability

    文摘:本文以極具典型的平川泥石流為例比較全面的分析了沖淤變動型泥石流的物源問題.根據現場調研及室內巖土分析進行的研究成果顯示，川西南高山深谷地區的大型泥石流溝中的鬆散土體以中、粗粒段為主，其分佈與地形密切相關；位於泥石流溝中、前部位的鬆散土體的穩定性最差，是補給泥石流的重要物源；鬆散土體的發育主要受控于地質及巖土環境，人類活動只能影響鬆散土體的穩定性
  17. There is a evolutional phenomenon to have been recognized in shaanbei loess plateau from south to north. that is luochuan district with the loess yuan ( platform land ) in south. yan ' an - an ' sai district with the loess liang ( ridges ) mainly in middle and shunde - mizhi district with the loess mao ( rounded knolls ) mainly in north. this frame and tendency is got and thought to coincide with the styles of their bedrock traditionalh ? called conformability

    在長期的研究和調查過程中，發現陜北黃土高原在南北縱向上存在明顯的黃土地貌分異現象，即由南向北，大致依次為洛川黃土塬（廣義）地貌、延安?安塞黃土梁狀（為主）丘陵溝壑地貌、綏德?子洲黃土峁狀（為主）溝壑地貌。
  18. In the light of tectonic evolution stage and metallogenesis, these metallogenic system ( assemblage ) could be classified as follows : ( 1 ) the pre - divergent metallogenic system in the southwest margin of north china paleocontinent in the archean - meso proterozoic : dongdashan iron, jinchuan nickel - copper. ( 2 ) the divergent metallogenic system in the northern margin of the qaidam paleoplate in the middle - late proterozoic : huashugou - liugouxia iron. ( 3 ) the metallogenic system in the active margin in the early paleozoic : the metallogenic assemblage in the island arc - rift in the early stage ( baiyinchang - qingshuigou copper - polymetallic ) ; the metallogenic assemblage in island arc in the middle - late stage ( honggou - jiaolongzhang copper - polymetallic ) ; the back - arc extensional basin ( zhuzhuiyaba - jiugequan - shijuli copper ) ; the metallogenic assemblage in connection with subduction and magmatic - hydatogenesis ( taergou - xiaoliugou wolfram ; huashugou - liugouxia copper ; dadonggou - diaodaban lead - zinc ) ; the metallogenic assemblage is related to the oceanic crustal shards ( dadaoerji chromite ; yushigou chromite ). ( 4 ) the metallogenic system has something to do with collision - type orogeny : the metallogenic assemblage in foreland basin ( tianlu copper ) ; the metallogenic assemblage with the intracontinental orogeny and ductile shear ( hanshan - yingzhuishan gold )

    根據構造發展階段和成礦作用特點，確定本區成礦系統及組合如下： （ 1 ）華北板塊西南邊緣太古宙中元古代裂解期前成礦系統：東大山鐵成礦組合，金川鎳銅成礦組合； （ 2 ）柴達木板塊北緣中、新元古代裂解成礦系統：樺樹溝柳溝峽鐵成礦組合； （ 3 ）加里東期活動大陸邊緣成礦系統：早期島弧裂谷成礦組合（白銀廠清水溝銅及多金屬成礦組合） ，中、晚期島弧成礦組合（紅溝蛟龍掌銅及多金屬成礦組合） ，弧后擴張盆地成礦組合（豬咀啞巴九個泉石居里銅及多金屬成礦組合） ，與俯沖作用有關的巖漿熱液成礦組合（塔爾溝小柳溝鎢成礦組合，樺樹溝柳溝峽銅成礦組合，大東溝吊大坂鉛鋅成礦組合） ，洋殼殘片成礦組合（大道爾吉鉻成礦組合，玉石溝鉻成礦組合） ； （ 4 ）碰撞造山成礦系統：前陸盆地成礦組合（天鹿銅成礦組合） ，陸內造山韌性剪切成礦組合（寒山鷹咀山金成礦組合） 。
  19. At the same soil layer, the sic contents on the tops of the hills were higher than those in the gullies, however, the soc contents on the tops of the hills were lower than those in the valleys. the possible factors of influence on the distribution of soil carbon were soil water content and human activities

    Kriging插值結果顯示，在同一土壤層次的不同地貌部位，土壤碳含量存在明顯差異，土壤無機碳含量是梁峁地高、溝川地低，土壤有機碳含量是溝川地高、梁峁地低。
  20. On the contrary, the valley soils had the minimum change for the profile sic content and the maximum change for the profile soc content the diversity of the soil profile carbon content change were related to their sources, movements and inversions in the soils

    在不同地貌部位的不同層次之間，無機碳含量在地勢高的梁峁地的土壤剖面上變化幅度大，有機碳含量在地勢低的溝川地的土壤剖面上變化幅度大，二者的差異主要由各自的來源、在土壤中的遷移、轉化等的不同所引起。
分享友人
分享到 Line

分享到臉書