水下熱泉 的英文怎麼說

中文拼音 [shuǐxiàquán]
水下熱泉 英文
submerged hot spring
  • : 名詞1 (由兩個氫原子和一個氧原子結合而成的液體) water 2 (河流) river 3 (指江、河、湖、海、洋...
  • : 下動詞1. (用在動詞后,表示由高處到低處) 2. (用在動詞后, 表示有空間, 能容納) 3. (用在動詞后, 表示動作的完成或結果)
  • : 名詞1 (泉水) spring 2 (泉眼)the mouth of a spring; spring3 (錢幣的古稱) an ancient term for...
  1. The pattern is not unlike what one sees in some geysers, which slowly heat up, boil off their supply of groundwater in a spectacular display, refill, and repeat the cycle, day in and day out, year after year

    這樣的模式類似於某些間歇,緩慢的加,然後在一次壯觀的噴發中排出所有蓄積的沸騰地,然後再重新蓄,重復上述循環;日復一日,年復一年。
  2. Based on analysis of geologic foundation record about pingzhuang basin, a lot of sino - foreign geothermal geology record and investigation of field geology, measuring of ground temperature in person and geo - chemical analysis of ascension spring, gushing water of fault, the fact that the anomaly of geothermal gradient of pingzhuang basin, which is in region of low geothermal gradient, is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out. after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys, the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed. the sound condition of transmissibility fault and feeding water source, which are imperative in formation of the low - medium temperature geothermal system of convective type, is possessed in pingzhuang basin

    通過對平莊盆地基礎地質資料、國內外大量地地質資料的分析和野外地質調查、礦井實測地溫以及上升、斷層涌的地球化學分析等工作基礎上,指出地處低地溫梯度背景區的平莊盆地地溫梯度異常是由於盆地基底隆起和坳陷引起傳導型大地流再分配所致;運用州sys數值模擬了大地流向地表傳導背景的盆地地溫場,從而揭示了盆地基底(義縣組)頂界面地溫分佈特徵;闡明了盆地具有形成中低溫對流型地系統所必需的導斷裂、補給源等的良好條件,中低溫對流型地系統是地勘查的主要對象;圈定了平莊盆地北部朝陽溝?駱駝營子地勘查遠景區。
  3. Around the shade around, emeishan from the spring down on the stone, such as color sure, it may emerald pearl inlay, water jump pentium, acoustic jubilant singing, and the hospitality of the people of the emeishan welcome to the guests all over

    四周綠蔭環繞,峨眉山從石上流,色如白練,似明珠鑲翡翠,花跳躍奔騰,聲歡快歌唱,代表著情好客的峨眉山人歡迎著來五湖四海的賓客。
  4. Finite element numerical simulation of the geothermal water system in the hot spring area in fuzhou

    福州溫區地有限元數值模擬研究
  5. Whether or no, the mender of roads ran, on the sultry morning, as if for his life, down the hill, knee - high in dust, and never stopped till he got to the fountain

    總之,在那個炎的早晨他像逃命一樣向山奔跑,跑得灰塵揚起有膝蓋高,直跑到邊才停止。
  6. The results are of great practical significance on the efficient development of geothermal water and the control of land subsidence in practice. the models can also be applied to the areas with homologous hydrogeological condition

    研究成果對于進一步揭示福州溫區地動態特徵,對于福州地區地資源合理開發利用,有效控制地面沉降具有重要的實際意義。
  7. In the ensuing excitement, researchers advanced many theories to explain them : leaking aquifers ( which would be inexplicably perched high on crater rims ) ; pressurized geysers of water ; high - pressure outbursts of carbon dioxide gas ; volcanic heat sources at depth

    在接來的一陣狂中,研究者提出許多的理論來解釋: ?漏的含層(在隕石坑外緣必須被抬升至非常高的高度) 、受壓的間歇、高壓噴出的二氧化碳氣體、深層的火山源等。
  8. 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: ( 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(豬咀啞巴九個石居里銅及多金屬成礦組合) ,與俯沖作用有關的巖漿液成礦組合(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) 。
  9. Using the theory of environment isotope and deuterium excess ( d - excess ) parameter, we found the cause of formation of spring ground water in mianzhu area, including the water origin and transportation process and recharge and discharge relationship of various water bodies and hydrogeologic units ; 2. the type of terrestrial heat system is low - medium temperature system of convective type ; 3. this paper valued the si well ( including the scale of geothermal water, exploitation potential and evaluation of medical treatment mineral water ) ; 4

    論文以同位素地球化學和文地球化學的理論、技術為基礎,結合綿竹三箭s _ 1井及其鄰區溫形成的區域地質構造背景、地層巖石組合特徵及主要文地質條件,剖析了研究區內可能存在地的「儲、蓋、通、源」基本條件,對該區各體的氫、氧同位素、氘過量參數、氚含量以及化學分析資料進行了系統地研究,取得了以成果。
  10. On the basis of the analysis of the topography, geomorphology, geological structure of geothermal area and surroundings in fuzhou city, and the survey of hydrogeological condition, and the distribution of geothermal drilling, and the geothermal water exploitation, and the groundwater regime, and the scale and distribution of land subsidence, the relationship between land subsidence and geothermal water regime was discussed. the result showed that land subsidence of geothermal area in fuzhou city was mainly induced by the excessive extraction of geothermal water in the thesis

    在分析研究福州市溫區及周圍的地形地貌、地質構造、文地質條件的基礎上,對地井分佈、流量、位、地開採的歷史與現狀以及對地面沉降的表現、規模、分佈規律進行了深入的調查;分析了地歷年位、量動態變化特徵,並探討地與地面沉降的相關關系,結果表明過量開采地是導致福州市溫區地面沉降的主要原因。
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