south china basin 中文意思是什麼

south china basin 解釋
南中國海盆
  • south : n 索斯〈姓氏〉。n 1 南；南方。2 南國居民。3 〈詩〉南風。4 〈the S 〉（一國或一地區的）南方，南部...
  • china : n. 中國。n. 瓷器；瓷料，白瓷土，瓷質黏土。 a piece of china一件瓷器。
  • basin : n 1 臉盆；水盆。2 滿盆，（一）盆。3 盆地，流域。4 水坑，地塘；（港灣）深度；內灣，小灣；【造船】...
  1. The primary representations of the vulnerabilities of water resource in hengyang basin where is a typical hilly region with red and purple soils in south china are analyzed : the precipitation re source varies greatly in spatial and temporal distribution ; the soils and rock property are not in favor of water and soil conserving ; the structure of crops needs a high water consumption ; and the farm irrigation works are timeworn and frangible

    摘要以中國南方典型的紅壤和紫色土丘陵區衡陽盆地為例，分析論述了衡陽盆地地表水資源脆弱性主要表現在：降水資源時空分佈不均勻；不利於水土保持的地表物質組成和植被覆蓋；耗水量大的農業種植結構以及調蓄水功能弱的農田水利工程體系等方面。
  2. The modified zndx in comparison with others is well indicative of the severity and extent of flood / drought event and of more objective classification of them, which is therefore quite applicable to a extended area. ( 3 ) the main anomaly structures of grades of drought / food in summer over northwest china present pluvial pattern and dry pattern in all the areas, and spatial changes are opposite pattern from the noth to the south and the west to the east. the first four rotated loading vector fields represent four principal precipitation anomaly areas : the weishui river basin, east of the qinghai - xizang plateau

    但修訂過的zndx指數根據氣溫、土壤濕度及前期氣候濕潤度等因子能夠客觀的反映出西北地區的旱澇特徵。 （ 3 ）西北地區季與年區域旱澇等級表明：西北地區的乾旱雨澇有顯著的階段性和年際變化特徵。 1980 』 s到1990 』 s中期，氣候較濕潤，土壤濕度增墑較明顯； 1990 』 s中期以後是40年乾旱最異常的時段； 1960 』 s旱澇交替發生，旱澇趨勢接近常年； 1970 』 s氣候雖乾旱，但沒有1990 』 s中後期顯著。
  3. In east china sea shelf basin, the mesozoic relict sediments are distributed in some central - south areas, such as fuzhou sag, minjiang sag and yushan lower uplift

    摘要東海陸架盆地中生界主要分佈於盆地中南部的福州凹陷、閩江凹陷和漁山低隆起地區。
  4. The topography and the physiognomy of the south china sea are very complex such as continental slop, continental shelves, seamounts, sea basin, etc. the south china sea lies between qingzang plateau, which is as the main driver of the variety of climate, and the western part of the pacific, which is called warm pool, and is influenced by some current systems, such as coastal current, kuroshi, etc. the south sea has considerable species

    南海具有陸坡、陸架、海溝、海盆等復雜的地形、地貌；南海位於作為地球氣候變化的主要驅動力的青藏高原和西太平洋暖池之間；南海受到沿岸流、南海暖流水、黑潮入侵水等流系的影響；南海具有豐富的物種分佈；上述因素共同影響南海生源要素的分佈、輸送和遷移。
  5. Study on hydrocarbon sources of lower triassic jialingjiang formation in south of sichuan basin, china

    四川盆地南部嘉陵江組烴源研究
  6. All the turn - point year is around 1974. another feature of interdecadal variability of interannual relationship between winter sea - ice extent of davis strait and summer, july and august rainfall of 160 stations is that the interannual correlation pattern have changed from east - west pattern to " + - + " north - south pattern around 1974. the interdecadal characteristics of correlation distribution pattern of interannual relationship between winter sea - ice extent of davis strait and summer, july 500hpa height of northern hemisphere are : " - + - " pattern from the beginning of novoya zemlya island, by way of balkhash lake to japan sea which is strongly negatively correlated with the rainfall of north china at the same period before 1974 and " + - " pattern from the beginning of ural mountains, by way of bujr lake to hetao basin which is badly correlated with the rainfall of north china at the same period after 1974

    冬季戴維斯海峽海冰面積與華北夏季及7 、 8月降水年際關系有明顯的年代際變化特徵：其與夏季總降水的年際關系由1974年前較好的負相關在1974年後變差，與7月降水的年際關系由1974年前較好的負相關在1974年後變弱，與8月降水的年際關系由1974年前較好的負相關在1974年後變差；另一方面，其與中國160站夏季及7 、 8月降水的年際關系在1974年前後發生變化的主要特徵是：與夏季總降水、 7月、 8月降水的年際關系由1974年前的相關系數分佈呈「東西型」變為1974年後相關系數分佈呈「 - + - 」的「南北型」 。
  7. Delegations of countries of south asia organized by icimod, investigated seabuckthorn planting and processing in loess plateau, yellow river basin, china

    和一些國際組織簽署了在中國北京建立國際沙棘研究培訓中心的「北京宣言」 。
  8. Based on an analysis of causes and basic characteristics of drought in north and south areas of china, it is pointed out that drought in north areas, such as the yellow river basin and the huaihe river basin, was characterized by the severe systematic demand - supply contradiction resulted from the shortage of water resources, and successive drought disasters intensified by hot and dry weather, and that drought in south areas was characterized by the occurrence or successive occurrence of dry years due to hot and dry weather and the seasonal water shortage induced by their geographic and climatic features and insufficient water supply capacity

    摘要以區域乾旱特徵分析以及乾旱災害應對策略研究為目的，闡述我國南、北方兩種不同地域類型的區域乾旱成因和基本特徵，指出黃淮海區域的乾旱特徵主要表現在天然水資源短缺引發的系統性深度供需矛盾，以及晴熱少雨氣候加劇這種矛盾而產生的持續乾旱災害；南方地區的乾旱特徵主要表現在晴熱少雨氣候導致枯水年或連續枯水年出現，以及地理氣候特徵和供水工程容量不足等因素產生的年內季節性乾旱缺水。
  9. Study of the gravity anomalyand construction evolution in ? the south china sea basin

    南海海盆重力異常場特徵及構造演化
  10. Distribution characters and exploration potential of mesozoic sea facies sedimentary strata in the south china sea basin

    南海盆地中生代海相沉積地層分佈特徵及勘探潛力分析
  11. According to the topography and geomorphology, the abnormality of gravitation and magnetic field, characteristics of crust structure and the environment of lithospheric dynamics in the northwestern of the south china sea, the seismic profiles were explained across the yinggehai basin and xisha trough

    摘要本文根據南海西北部殼體的地形地貌、重磁場異常和地殼結構特徵和巖石圈動力學環境，對穿過鶯歌海盆地和西沙海槽的地震剖面進行解釋。
  12. The central - southern songliao basin and its adjacent area are located in the south of inner mongolian - northeastern china neotectonic region of the circum - pacific neotectonic domain

    摘要松遼盆地中南部及其鄰區位於濱太平洋新構造域的內蒙一東北新構造區南部。
  13. The nature of the rucheng basin in southeastern hunan and its significance to the tectonic setting of south china during the early yanshanian

    湘東南汝城盆地性質及其對華南燕山早期構造環境的啟示
  14. Abstract : in the light of sequence stratigraphic research work on permain coal - accumulating basins in south china and jurassic ordos coal - accumulating basin in north china, the sequence stratigraphic model and coal - accumulating model of passive continental margin and continental down warping basin were established, the comparison between both settings was also briefly conducted

    文摘:運用層序地層學原理，對華南二疊紀含煤盆地和侏羅紀鄂爾多斯含煤盆地進行研究，建立了被動大陸邊緣盆地和陸相坳陷盆地的地層層序沉積模式和層序聚煤模式，並對兩者聚煤作用作了簡要對比。
  15. There are 6 dominant spatial patterns : same distribution allover the country ; the seesaw between the regions of south of the yangtze river and mid - lower reaches of the yellow river ; the seesaw between the regions over the yangtze river and the yellow river and the south part of south china ; coherent variations over the yangtze - huaihe river basin and north - east china and opposite variations in the regions of north china and north - west china and south - east part of china ; the seesaw between the east part and the west part of china ; coherent variations over mid - lower reaches of the yellow river and south china and opposite variations in the yangtze river basin

    近44年來我國逐旬降水量年變化特徵主要存在六種空間分佈型：全國大范圍地區年變化特徵一致的分佈；長江以南地區和黃河中下游地區降水量分佈相反；長江、黃河流域和華南沿海降水量分佈相反；長江、淮河流域和東北地區與華北、西北和東南沿海降水量分佈相反；我國東西部地區降水量分佈相反；長江流域與黃河中下游和華南降水量分佈相反。
  16. In drought or flood years over the yangtze river basin, the features of the establishment, progression and decrease of moisture transport is significantly different, meanwhile the differences of the moisture transport by the monsoon circulation between mid and low latitudes in the northern hemisphere, and by the subtropical high are obvious, so are their convergence, especially over south china sea, the tropical west pacific, the yangtze river basin, north china and north - east in china

    （ 4 ）長江流域旱澇年亞澳季風區夏季風水汽輸送的建立、推進、減弱的階段性特徵顯著不同，對應的中低緯季風環流、副高環流等季風系統水汽輸送、匯合也有顯著差別，尤其是在南海、熱帶西太平洋、長江流域、華北和東北等地區。
  17. In the droughts or floods over the yangtze river basin, between june and the second dekad in july, the moisture transport from the southern boundary, originating from south china sea and south china, is the most important influence factor, but between the last dekad in july and august, the one flowing out from northern boundary is the most important influence factor

    長江流域旱澇年， 6 - 7月中旬來源於南海、華南地區的南邊界水汽輸入是主要影響因子， 7月下旬一8月北邊界的水汽輸出是主要影響因子。長江流域旱（澇）年夏季風水汽輸送的北界偏北（南） ，副高南側的東南風水汽輸送偏北（南） 。
  18. The grade, tonnage and distribution of sandstone all show fractal structure features. the fractal dimension is 1. 13, 1. 15 and 2. 67 for average grade, tonnage and grade vs tonnage of sandstone copper deposits in the world respectively, and 0. 911 for the distribution of cu - bearing basins in south china, and 0. 932 for the distribution of sandstone copper deposits in kangdian region. the prospective reserve of sandstone copper deposits in main cu - bearing basins is predicted using a fractal model, which shows good prospects of ore potentiality in the central yunnan basin, the western yunnan basin, the huili basin, sichuang, the hengyang basin and the yuanma basin, hunan. 6figs., 1tab., 4refs

    砂巖銅礦床的品位、噸位及空間分佈具有分形分佈的特徵.世界主要砂巖銅礦床的平均品位、噸位和品位與噸位關系的分維值分別為1 . 13 、 1 . 15和2 . 67 ；我國南方含銅盆地和康滇地區砂巖銅礦空間分佈的分維值分別為0 . 911和0 . 932 .利用礦床的分形模式對主要含銅盆地的砂巖銅礦遠景進行了預測，結果表明滇中、滇西、會理、衡陽和沅麻等盆地還有較大的找礦前景.圖6 ，表1 ，參4
  19. Abstract : the grade, tonnage and distribution of sandstone all show fractal structure features. the fractal dimension is 1. 13, 1. 15 and 2. 67 for average grade, tonnage and grade vs tonnage of sandstone copper deposits in the world respectively, and 0. 911 for the distribution of cu - bearing basins in south china, and 0. 932 for the distribution of sandstone copper deposits in kangdian region. the prospective reserve of sandstone copper deposits in main cu - bearing basins is predicted using a fractal model, which shows good prospects of ore potentiality in the central yunnan basin, the western yunnan basin, the huili basin, sichuang, the hengyang basin and the yuanma basin, hunan. 6figs., 1tab., 4refs

    文摘:砂巖銅礦床的品位、噸位及空間分佈具有分形分佈的特徵.世界主要砂巖銅礦床的平均品位、噸位和品位與噸位關系的分維值分別為1 . 13 、 1 . 15和2 . 67 ；我國南方含銅盆地和康滇地區砂巖銅礦空間分佈的分維值分別為0 . 911和0 . 932 .利用礦床的分形模式對主要含銅盆地的砂巖銅礦遠景進行了預測，結果表明滇中、滇西、會理、衡陽和沅麻等盆地還有較大的找礦前景.圖6 ，表1 ，參4
  20. ( 2 ) around mid - 1970s ", precipitation of east china has also a great change : precipitation of north and south china decreases, rainfall of basin of yangtze river and north - east china increases, the distinct areas are drainage of yangtze river, huanghuai and west south china. before or after 1976, the year and the next year while el nino or la nina happens, the distribution of rainfall anomaly shows opposite characters in most area of east china

    （ 2 ）對海溫轉變前後我國東部降水的分析表明， 70年代中期我國東部降水特徵也發生了明顯的轉變：從大范圍多雨轉為大范圍少雨，其中華北、華南由多雨轉為少雨，黃淮和華南西部地區降水減少，而長江中下游及其南部和東北由少雨轉為多雨； 76年前後厄爾尼諾發生當年和次年及拉尼娜發生當年和次年，我國東部相當大的范圍內降水異常出現反相的特徵。
分享友人
分享到 Line

分享到臉書