磁測深 的英文怎麼說

中文拼音 [cícèshēn]
磁測深 英文
magnetic sounding
  • 磁 : 名詞1. [物理學] （磁性; 能吸引鐵、鎳等的性質） magnetism 2. （瓷） porcelain; china
  • 測 : 動詞1. （測量） survey; fathom; measure 2. （測度; 推測） conjecture; infer
  • 深 : Ⅰ形容詞1 （從上到下或從外到里的距離大） deep 2 （深奧） difficult; profound 3 （深刻; 深入） thor...
  1. Based on an integrated correlation and study of regional and deep geophysical data such as 12 magnetotelluric sounding profiles, 5 seismic profiles, tomographic imaging velocity structural data and gravity and magnetic field, the authors have formulated the 3d deep tectonic framework of the middle and lower yangtze valley and its neighborring areas in relation to the distribution of auriferous skarn deposits and copper ( associated with gold ) skarn deposits

    作者藉助12條大地電磁測深剖面、 5條地震剖面、層析成像速度結構資料、重磁場等區域的和深部的地球物理資料進行綜合對比研究，給出長江中下游及其鄰區的三維深部構造格架及其與含金夕卡巖礦床和銅伴生金夕卡巖礦床的分佈關系。
  2. The inversion results of synthetic magnetotelluric sounding data are ideal, which indicates that the algorithm possesses advantages of expediting convergence, avoiding earliness and improving precision, and can be used in mt data analysis

    對各種類型的大地電磁測深理論曲線進行計算，結果表明：採用實數編碼混合遺傳演算法進行反演具有收斂速度快、解的精度高和避免出現早熟等優點，可用於大地電磁資料解釋。
  3. The research of large igneous rock province - ermei basalt extrusion - mantle plume shows that songpan - ganzi folded belt is a hopeful target for breakthrough of petroleum exploration, and the key issue is how to make well a coupling and optimization among its faults, structures, traps and reservoirs

    根據地震測深、重、磁、電等的探查，發現該褶皺帶深部有一低速高導層，而對大火成巖省峨眉玄武巖噴溢地幔柱的認識深化均表明，四川松潘甘孜褶皺帶是可望獲得油氣勘探突破的靶區，重要的是斷裂構造、圈閉、儲集層的耦合與優化。
  4. They not only have the quality of slow decay, but also narrow beam and focused energy, which are widely used in military and communication

    慢衰減電磁波的衰減比一般電磁波慢，可以實現較大的探測深度；由於它的頻率高，可以實現較高的解析度。
  5. In this paper, by explored geo - physico - chemical prospecting method for looking for oil in prior prospect, the authors summarize a suit of prospective technique and program, which is valid to oil - geology trait of zhidan area and composed of ; oil gas geo - chemical prospect ( acid degradation of hydrocarbon, absorbed - fluorescent spectrum, ultraviolet radiation spectrum, methane carbon - isotope ) non seismic detection in favorable explorative area which confirmed by chemical prospect ( matural potential, gamma energy spectrum. accurately magnetic analysis ) resistively prospecting in anomalous area which confirmed by physicalprospect successful general evaluation of geo - physicochemical prospect

    通過勘探早期地質物化探綜合找油方法實驗，筆者總結了一套適合志丹探區石油地質特點的勘探方法組合和勘探程序：油氣地球化學勘探（酸解烴、吸附烴、熒光光譜、紫外光譜、甲烷碳同位素、蝕變碳酸巖）化探圈定的有利勘探區進行非地震物探（自然電位、伽瑪能譜、高精度磁測、土壤測氧）物探圈定的異常區進行電阻率測深勘探地質物化探成果綜合評價。
  6. Based on an integrated analysis of the surface geological, aeromagnetic, gravity, mt and seismic data from the area of mangnai to serteng mountains in the western qaidam basin, the authors think that the qaidam basin is sandwiched between the north kunlun block and serteng tectonic belt, including two first - order tectonic units the qaidam block and the southern margin of the qilian block and four second - order tectonic units the northern margin of the north kunlun block, qaidam basin, serteng tectonic belt and suhai lake basin in the south of the qilian block

    摘要通過柴達木盆地西部茫崖賽什騰山地表地質、航磁、重力、大地電磁測深和地震資料的綜合分析，認為柴達木盆地夾持在昆北地塊與賽什騰構造帶之間，其中包括柴達木地塊與祁連地塊南緣2個一級構造單元和昆北地體北緣，柴達木盆地，賽什騰構造帶和祁連地塊南部的蘇干湖盆地等4個二級構造單元。
  7. Through analysis on skin depth and calculation of the responses of a theoretical model, the mt response curves for 40 number and 80 number frequencies are obtained

    通過對趨膚深度分析以及對理論模型響應的計算，得到了80個頻率點與40個頻率點的大地電磁測深響應曲線。
  8. On the basis of analyzing previous scientists ' work, aeromagnetic data from north china wee reprocessed with 3 - d magnetosphere inversion method and program quantitative buried depth of curie temperature interface was obtained ; seismogenesis and its re1atnhip with curie temperature interface were discussed in the light of results from deep seismic sounding and deep fluid

    摘要在前人工作的基礎上，運用三維磁性層反演方法和程序，對華北地區航磁資料進行了再處理，得出了研究區內居里溫度面的定量埋深，結合人工地震測深和深部流體對地震成因及其與居裏面的關系進行了討論。
  9. Operation and maintenance for magnetotelluric instruments

    大地電磁測深儀使用與維護
  10. Digital magnetic telluro sounding instrument

    數字大地電磁測深儀
  11. Double power earth electric magnetic depth measuring and application

    雙源大地電磁測深及其應用
  12. Application and development on the inversion technique of the magnetotelluric sounding

    大地電磁測深資料常規反演方法的應用現狀及進展
  13. In the process of mt depth measurement, frequencies with 40 numbers are basically used at present

    摘要在大地電磁測深中，目前基本上使用40個頻率點的數據。
  14. The result of measurement with 40 number frequency is compared with that of 80 number frequency

    對比分析了採用80個頻率點與採用40個頻率點的大地電磁測深結果。
  15. Based on the examples of controlled source audio - frequency magnetotellurics application, the paper discuses the problems of electromagnetic sounding in deep geothermal investigation

    摘要以可控源音頻大地電磁測深應用實例，討論電磁測深方法在深部地熱資源調查中的應用問題。
  16. The inverse problem of mt for 1 - d was studied by using a real coded hybrid genetic algorithm, which was based on the combination of simplex method and genetic algorithm

    摘要設計了一種求解一維大地電磁測深反演問題的實數編碼混合遺傳演算法，它是通過單純形搜索與遺傳演算法結合而成。
  17. Although the magnetotelluric sounding method applied to land is mature, many technical problems arise when they are transplanted into the seafloor environment, one of which is how to put magnetic field sensors down to the seafloor to complete measurements

    摘要大地電磁測深在陸地上的方法技術成熟，但將其移植到海洋中卻遇到了較多的技術問題。
  18. Exemplified by the application of controlled source audio - frequency magnetotelluric sounding, this paper discusses the deep and periphery prospecting work with the resistivity sounding technique in the bajiazi lead and zinc mine of liaoning province

    摘要以可控源音頻大地電磁測深方法應用為例，討論遼寧省八家子鉛鋅礦深部及外圍電阻率測深找礦問題。
  19. Because limited by the sampling channel of transient electromagnetic measuring depth fieldwork curve ( generally 20 ~ 40 channels ), the smoothing degree of fieldwork curve is not very good, it make against the differential imaging treatment. in order to hold the continuous change characters of the curve and seek the voltage exactly, we use the thrice spline insert number function to reconstruct the fieldwork data ; 4

    ） t ； 3 .由於受瞬變電磁測深實測曲線取樣道的限制（一般為20 ~ 40道） ，實測曲線光滑程度較差，不利於微分成像處理，為了更好的把握曲線連續變化的特徵及準確求導，採用了三次樣條插值對實測數據進行重構;續
  20. It can reach the purpose of improving precise. this thesis study the theory of tem measuring depth method, wavelet analysis and differential conductance imaging principle of tem measuring depth data, then the thesis brings forward the tem fast imaging technology based on the wavelet analysis

    本文在詳細論述了瞬變電磁測深法的基本理論、小波分析的基本理論以及瞬變電磁測深數據的微分電導成像原理的基礎上，提出了基於小波分析的tem快速成像技術。
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