火山地區 的英文怎麼說

中文拼音 [huǒshānde]
火山地區 英文
volcanic region
  • : fire
  • : 名詞1 (地面形成的高聳的部分) hill; mountain 2 (形狀像山的東西) anything resembling a mountain...
  • : 區名詞(姓氏) a surname
  • 火山 : [地質學] volcano; burning mountain
  1. Nine days before the most recent silent earthquake on kilauea, a torrential rainstorm dropped nearly a meter of water on the volcano in less than 36 hours

    就在奇勞亞最近一次發生無聲震的九天前,一陣猛烈的暴風雨在36小時之內讓火山地區累積了將近一公尺的雨量。
  2. Geothermal power stations tap aquifers heated by contact with hot rocks in volcanic regions ? or, in hot but dry spots, they pump water past such rocks to heat it up

    熱發電廠利用火山地區? ?或者溫高且乾燥的點? ?的乾熱巖體傳導熱能給含水層畜熱,然後將水注入含水層利用熱巖體對其加熱並使之汽化。
  3. The age values are close to crystallizing age of the quartz. combined with other geochronological data and the geological features, it is concluded that the indo - chinese epoch may be the principle mineralization period for gold deposits in the southwestern tianshan mountains. 3

    金屬硫化物的~ ( 34 ) s = - 3 . 4 + 2 . 6 ,西南天下古生界層中廣泛存在各類巖可能是該礦床的主要硫源,部分可能有深部物質的參與。
  4. 4. the relative fertile lithospheric characters of yanshan area, unique plate tectonic situation and developed deep faults can explain reasons of the volcanism and tectonic events in yanshan area throughout the mesozoic

    4燕特有的相對「易熔」的巖石圈性質,所處的特殊的構造位置及發育的深大斷裂,可以較好的解釋該發生貫穿整個中生代的活動和構造變形的可能性。
  5. These islands are the most isolated land surrounded by ample ocean surface for the great storms of the pacific to generate giant, perfect waves that pulse from deep water into the shallow reefs and lava rock of the hawaiian island chain

    夏威夷群島是一個個最為孤立的、四周被巨大的海洋表面圍繞著的方,太平洋上強烈的風暴產生巨大而完美的波濤就會從深水處湧出,並進入淺礁以及夏威夷一系列的
  6. They are free of turbidity, except in some limestone areas and volcanic areas with high secondary permeability where large underground rivers occur.

    它們不至於渾濁、只是在灰巖火山地區具有高的次生滲透性並存在大下河時除外。
  7. Lee, c. s., tsai, c. f., chung, s. l. and spot member, 1998, active interaction of submarine volcanoes and ocean current in the southernmost part of okinawa trough. agu fall meeting

    李昭興、蔡慶輝、鍾孫霖, 1998 ,海底震和洋流的交互作用: spot。中國球物理年會, 487 - 496頁。
  8. Lee, c. s., chung, s. l. and spot members, 1998, southernmost part of the okinawa trough ( spot ) : an active extension / collision / subduction area, agu western pacific geophysical meeting

    李昭興、蔡慶輝、鐘孫霖, 1998 ,海底震和洋流的交互作用: spot。中國球物理年會, 487 - 496頁。
  9. Here we used wavelet and spectral analysis to different kind seismic waves in volcanic area, in order to pick up their spectral character and determine the type of these earthquakes

    本文對不同種類的震波形運用小波分析和頻譜分析的方法,希望能提取不同類型震的一些頻譜特徵,確定震的類型。
  10. Numerical simulation of gravity variation in volcanic region

    火山地區重力場變化的數值模擬
  11. During my master " degree investigation, i mainly focused on the coarse - grain stratigraphy within mesozoic basins in chengde and pingquan districts, the eastern yanshan, and did systemic provenance analysis and paleo - current direction measurement and studied the relationship among basin evolution, volcanism and tectonism. then i summarized the mesozoic basin development and the coupling characters of basin and mountain. the evolution of basin and mountain in this area can be divided into several stages : the stage of compression uplift and flexural basin during the triassic through the early jurassic, the stage of structural compression - volcanism and foreland basin during the middle and late jurassic and the stage of rift basin in the cretaceous

    在野外典型路線調查的基礎上,對燕東段承德、平泉的中生代盆中發育的粗碎屑沉積層,進行了系統的物源分析與古流測定,並在此基礎上重點剖析了盆的發育、活動、構造變動三者之間的關系,總結了本中生代盆發育規律及盆耦合特徵,並將盆演化劃分為:三疊紀?早侏羅紀的構造擠壓隆升與撓曲盆發育階段階段,中晚侏羅紀的構造擠壓?活動與類前陸盆發育階段,早白堊世的拉張斷陷盆發育階段。
  12. Many of the procedures we tried had never been used before on an active explosive volcano.

    我們採用的許多試驗方法,過去還從未在一次活噴發火山地區用過。
  13. The mission also included geological experiments in the area around the volcano and testing a two - wheeled vehicle called " marvin, " which may be used in future mars missions

    原計劃還包括在該火山地區進行址勘測,以及測試一種名叫" marvin "的兩輪運輸車,這種車是為日後在星進行勘測時使用而設計的。
  14. Based on the several year data of permafrost in the region of fenghuoshan mountain, this paper not only studied the transformation of upper limit of permafrost in natural ground and roadbed but also the thawing of permafrost, and analysed quantitatively the status of heat which have entered permafrost

    摘要基於對多年來風火山地區的多年凍土資料,研究了天然和路基下的凍土上限變化情況以及多年凍土的融化狀態,並定量分析了進入多年凍土內的熱狀況。
  15. The results demonstrate that the upper limit of permafrost in this area had declined from 1970s to the middle phase of 1990, and permafrost has appeared degenerate tendecy, but since middle 1990s, permafrost have a stable state ; ground temperature of roadbed near the earth surface is higher than that of the natural ground, thawing time of roadbed near the earth surface is longer than that of the natural ground, the heat income within the permafrost is greater than the heat release from the permafrost during anannual period, the heat accumulation within the permafrost is temporarily appeared as temperature rising, but with the heat accumulation within permafrost growing up year by year, permafrost temperature will become higher gradually, and strong thawing of permafrost could be happened in the region

    結果表明:風火山地區從20世紀70年代到90年代中期凍土上限下降,凍土出現退化現象,從90年代至今凍土趨于穩定;路基近溫明顯高於對應天然表下的溫,路基近表經歷的融化期長于對應天然表,進入多年凍土的熱收支也呈現出吸熱明顯大於放熱的周期性變化,進入多年凍土的熱積累暫時以增高溫耗熱為主,但隨著凍土吸熱量的逐年積累、凍土溫度的不斷升高,本凍土可能發生強烈融化。
  16. There are 11 display areas inside the museum, covering subjects such as the formation of various types of hot spring, the history of peitou s development as a spa, local industries such as peitou porcelain and lincao rush weaving, the volcanic geology of the area, hot springs around the world, and most particularly, the mineral known as hokutolite or " peitou stone.

    館內分十一個展示,有關溫泉的種類來源,北投溫泉相關的發展歷史及圖像,北投燒陶瓷和藺草等特殊產業,和北投的形世界溫泉介紹等,其中最特殊的是北投石。
  17. On the basis of study on petrology, volcanic geology, geochemistry, isotopic chronology, antitheses of the regional strata and 4 suits of volcanic rock stratum of the yanshan - liaoning area, the rhythm of yanshanian volcanic activity is divided into 1 gigantic - cycle, 4 cycles, 11 micro - cycles, 24 sub - cycles and many rhythms. in addition, the temporal and spatial evolution and regional contrast of every - level rhythms are discussed. 3. based on the study on classifications of rhythm of volcanic activity and regional contrast, the petrology, mineralogy, geochemistry, and isotopic characteristics of every - level rhythms are discussed

    2 、通過對燕遼期發育的四套巖的巖石學、質學、球化學、同位素年代學的綜合研究,通過運用綜合方法進行層對比和分析噴發盆層特徵的基礎上,將本活動節律,劃分為1個二級節律(大旋迴) 、 4個三級節律(旋迴) 、 11個亞三級節律(小旋迴) 、 24個四級節律(亞旋迴)和多個五級節律(韻律)等,論述了各級活動節律特徵及其時空演化和域對比。
  18. The mantle source for the mesozoic mafic volcanic rocks in yanshan area exhibit transition character in space and time : the mantle source components vary from subduction - related metasomatic components and emi components through dominant emi components and slight subduction - related metasomatic components to emi components ; spatially, mantle source of the volcanic rocks show a regular variation trend from an enriched lithospheric mantle with emi - like signatures in the western shandong province through emi and / or subduction - related metasomatic components in yanshan area to subduction - related metasomatic lithospheric mantle in the hinggan - mongolian orogen

    中酸性巖則來源於殼,與玄武質巖漿底侵作用關系密切。 3燕巖源組分在時空上具有一定的演化規律:在時間上,從早期俯沖交代幔及emi的參與,經中期以emi佔主導及極少量俯沖交代組分的階段,演變到晚期以emi為主,可能有少量軟流圈貢獻的組分,再到晚白堊世以軟流圈為主。
  19. 2. early jurassic mafic volcanic rocks in yanshan area were derived from decompression melting of an ancient continental lithospheric mantle, which had been previously metasomatized by subducted slabs during the closure of paleo - asian ocean ; the mantle source of late jurassic mafic volcanic rocks were contributed by dominant emi and insignificant subducted metasomatic components ; early cretaceous mafic volcanic rocks were derived from decompression melting of an ancient continental lithospheric mantle ( emi ). with regard to the basaltic lavas, the felsic rocks resulted from partial melting of continental crust, which closely related to basaltic underplating

    2燕早侏羅世中基性巖來自於早期俯沖交代的古老巖石圈幔部分熔融作用,俯沖交代作用可能與早期古亞洲洋閉合事件有關;晚侏羅世中基性巖更多來自於類似於emi型幔源的部分熔融作用,俯沖交代成分貢獻很弱;早白堊世基性巖則來自於emi型幔源的部分熔融作用。
  20. Two types of volcanoes exist in the three sisters region and each poses distinct hazards to people and property

    三姐妹有兩種形式的,都對人和財產構成威脅。
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