物探与化探
物探與化探
물탐여화탐
GEOPHYSICAL AND GEOCHEMICAL EXPLORATION
2014年
6期
1241-1245
,共5页
倾斜地层%电各向异性%大地电磁测深%电磁响应%正演计算
傾斜地層%電各嚮異性%大地電磁測深%電磁響應%正縯計算
경사지층%전각향이성%대지전자측심%전자향응%정연계산
tilted strata%electric anisotropy%magnetotelluric sounding%electromagnetic response%forward calculation
研究地层电各向异性性质能够圈定沉积地层中的油气储层和与地球动力学过程、地震预报有关的深部线性构造。通过得到的N层倾斜电各向异性介质大地电磁响应公式,在不同的电各向异性系数、地层倾角、倾斜层厚度参数下,对电各向异性倾斜地层模型进行了正演计算。结果表明:当电各向异性系数、地层倾角、地层厚度三者中任一变量改变时,视电阻率曲线的形态基本保持不变,但视电阻率曲线振幅值变化较大;视电阻率曲线对地层倾角参数的变化反应最为敏感;电各向异性系数的增加,能突显薄层电阻率异常。这有助于以后的电各向异性介质大地电磁反演和应用研究。
研究地層電各嚮異性性質能夠圈定沉積地層中的油氣儲層和與地毬動力學過程、地震預報有關的深部線性構造。通過得到的N層傾斜電各嚮異性介質大地電磁響應公式,在不同的電各嚮異性繫數、地層傾角、傾斜層厚度參數下,對電各嚮異性傾斜地層模型進行瞭正縯計算。結果錶明:噹電各嚮異性繫數、地層傾角、地層厚度三者中任一變量改變時,視電阻率麯線的形態基本保持不變,但視電阻率麯線振幅值變化較大;視電阻率麯線對地層傾角參數的變化反應最為敏感;電各嚮異性繫數的增加,能突顯薄層電阻率異常。這有助于以後的電各嚮異性介質大地電磁反縯和應用研究。
연구지층전각향이성성질능구권정침적지층중적유기저층화여지구동역학과정、지진예보유관적심부선성구조。통과득도적N층경사전각향이성개질대지전자향응공식,재불동적전각향이성계수、지층경각、경사층후도삼수하,대전각향이성경사지층모형진행료정연계산。결과표명:당전각향이성계수、지층경각、지층후도삼자중임일변량개변시,시전조솔곡선적형태기본보지불변,단시전조솔곡선진폭치변화교대;시전조솔곡선대지층경각삼수적변화반응최위민감;전각향이성계수적증가,능돌현박층전조솔이상。저유조우이후적전각향이성개질대지전자반연화응용연구。
The study of the electric anisotropy properties of strata can delineate oil and gas reservoirs in the strata and the deep linear structure related to geodynamic process and earthquake prediction. On the basis of magnetotelluric response formula in N-layer tilted e?lectric anisotropic media obtained by the authors and under the condition of different electric anisotropy coefficients, dip angles of strata and thicknesses of tilted beds, the authors conducted forward calculation of the model for electric anisotropic tilted strata. The results show that, when any one of the three variables ( electrical anisotropy coefficient, dip angle of strata, and depth of strata) is changed, the shape of the apparent resistivity curve remains basically unchanged, but the amplitude value of the apparent resistivity curve varies considerably, that the apparent resistivity curve is most sensitive to the change of the dip angle parameter of strata, and that the in?crease of the electric anisotropy coefficient can clearly demonstrate the resistivity anomaly of the thin layer. The results achieved by the authors will be helpful to electric anisotropic media magnetotelluric inversion and applied research in future.