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combination entropy中文是什么意思

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  • By applying the theory and method of geological anomaly, it is focused on the analysis of the characters of major geological anomalies and their effect of mineralization in daye-jiurui region . the analysis result shows that the basement fault anomalies control a few major large hidden batholiths and their associated orefields; that the anomalies of cover structure confine most cu-au deposits and fe-cu deposits within their scope; that the geochemical anomalies and lithofacies-paleogeographical anomalies are major geological factors leading to trataboundness of some cu-au deposits; that the anomalies of rock operties provide the favorable chemical and physical conditions for the ore-forming process, including the seepage, circulation, convergence and deposit of ore-bearing hydrothermal solution; that the anomalous ctive stage of mesozoic magmatite is almost consistent with the major mineralization epoch of the fe, cu deposits, and the structure of multi-levels, and the zoning in magmatic system determine the spatial distribution of the mineralization system . then, based on the above analysis, a comprehensive variate, geological combination entropy, is brought forward for reflecting the complex degree of the combination of geological ore-controlling factors . after circumscribing the anomalies of geological combination entropy, the relations between the anomalies and ore deposits are determined
    從地質(zhì)異常的角度,重點(diǎn)分析了大冶九瑞地區(qū)主要地質(zhì)異常的特征及其對(duì)成礦的影響.由分析可知:基底斷裂異??刂屏吮緟^(qū)若干重要規(guī)模較大的隱伏巖基及伴生礦田,而蓋層構(gòu)造異??刂沏~金礦床和鐵銅礦床的空間位置;地層的地球化學(xué)異常和巖相古地理異常是造成一些銅金礦床層控性的主要地質(zhì)因素;蓋層的巖性異常為含礦熱液的滲流、循環(huán)、聚集和礦質(zhì)沉淀等一系列成礦作用提供了有利的物理和化學(xué)條件;中生代巖漿巖的異?;顒?dòng)期也是本區(qū)主要的鐵銅成礦期,巖漿巖系統(tǒng)的多層分枝和分帶性結(jié)構(gòu)控制了本區(qū)成礦系統(tǒng)的三維空間分布.在上述分析的基礎(chǔ)上,構(gòu)置了地質(zhì)組合熵作為反映控礦地質(zhì)因素組合系統(tǒng)結(jié)構(gòu)復(fù)雜程度的綜合變量,并圈定出組合熵異常,由此確定了綜合地質(zhì)異常與礦床的關(guān)系
  • By applying the theory and method of geological anomaly, it is focused on the analysis of the characters of major geological anomalies and their effect of mineralization in daye-jiurui region . the analysis result shows that the basement fault anomalies control a few major large hidden batholiths and their associated orefields; that the anomalies of cover structure confine most cu-au deposits and fe-cu deposits within their scope; that the geochemical anomalies and lithofacies-paleogeographical anomalies are major geological factors leading to trataboundness of some cu-au deposits; that the anomalies of rock operties provide the favorable chemical and physical conditions for the ore-forming process, including the seepage, circulation, convergence and deposit of ore-bearing hydrothermal solution; that the anomalous ctive stage of mesozoic magmatite is almost consistent with the major mineralization epoch of the fe, cu deposits, and the structure of multi-levels, and the zoning in magmatic system determine the spatial distribution of the mineralization system . then, based on the above analysis, a comprehensive variate, geological combination entropy, is brought forward for reflecting the complex degree of the combination of geological ore-controlling factors . after circumscribing the anomalies of geological combination entropy, the relations between the anomalies and ore deposits are determined
    從地質(zhì)異常的角度,重點(diǎn)分析了大冶九瑞地區(qū)主要地質(zhì)異常的特征及其對(duì)成礦的影響.由分析可知:基底斷裂異??刂屏吮緟^(qū)若干重要規(guī)模較大的隱伏巖基及伴生礦田,而蓋層構(gòu)造異??刂沏~金礦床和鐵銅礦床的空間位置;地層的地球化學(xué)異常和巖相古地理異常是造成一些銅金礦床層控性的主要地質(zhì)因素;蓋層的巖性異常為含礦熱液的滲流、循環(huán)、聚集和礦質(zhì)沉淀等一系列成礦作用提供了有利的物理和化學(xué)條件;中生代巖漿巖的異?;顒?dòng)期也是本區(qū)主要的鐵銅成礦期,巖漿巖系統(tǒng)的多層分枝和分帶性結(jié)構(gòu)控制了本區(qū)成礦系統(tǒng)的三維空間分布.在上述分析的基礎(chǔ)上,構(gòu)置了地質(zhì)組合熵作為反映控礦地質(zhì)因素組合系統(tǒng)結(jié)構(gòu)復(fù)雜程度的綜合變量,并圈定出組合熵異常,由此確定了綜合地質(zhì)異常與礦床的關(guān)系
  • On the basis of the calculating of complexity ( c value ) and combination entropy ( h value ) from the numerical method of geoanomaly analysis, logged signals data ( spontaneous potential, acoustic slowness, spontaneous gamma ray and electrical resistivity ) and seismic data ( amplitude, frequency, phase, etc . ) are processed after regularization of data obtained from linqing basin of shengli oil field . many types of geoanomalies obtained from the computation are analyzed so the spacial variation rules of them can be discovered . then the oil regions can be predicted by this method
    本文創(chuàng)新性地將地質(zhì)異常概念引入油氣勘探領(lǐng)域,以地質(zhì)異常理論為指導(dǎo),以勝利油田臨清坳陷油氣地質(zhì)異常預(yù)測研究為例,針對(duì)我國陸相含油氣盆地的常規(guī)測量、測試和解釋數(shù)據(jù),如與地震相關(guān)的數(shù)據(jù)(振幅、頻率、吸收系數(shù)、層速度等)、與測井相關(guān)的數(shù)據(jù)(自然電位、聲波、視電阻率、自然伽馬等)等,提取不同數(shù)據(jù)類型的地質(zhì)異常以及異常組合特征,通過對(duì)這些參數(shù)的綜合研究分析其空間變化規(guī)律,系統(tǒng)地建立有效預(yù)測油氣藏的新技術(shù)和新方法,進(jìn)而達(dá)到區(qū)域油氣資源預(yù)測的研究目的。
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