煤田地质与勘探
煤田地質與勘探
매전지질여감탐
COAL GEOLOGY & EXPLORATION
2010年
2期
50-53,58
,共5页
游秀珍%吴小平%王威%余勇%鲁晶津
遊秀珍%吳小平%王威%餘勇%魯晶津
유수진%오소평%왕위%여용%로정진
电阻率%深部三维结构%二维反演%分辨能力
電阻率%深部三維結構%二維反縯%分辨能力
전조솔%심부삼유결구%이유반연%분변능력
resistivity%3D deep structures%2D resistivity inversion%resolution
利用三维有限差分方法进行深部三维结构的电阻率三维数值模拟,对计算得到的单极-单极和对称四极装置视电阻率剖面进行电阻率二维反演研究.结果显示:单极-单极装置在横向上只要三维异常体中心的水平间距不小于两者中心埋深之和,就可以基本将2个三维结构分辨出来;相同情况下,对称四极装置在横向上的分辨效果优于单极-单极装置;单极-单极装置在垂向上的分辨要优于对称四极装置.
利用三維有限差分方法進行深部三維結構的電阻率三維數值模擬,對計算得到的單極-單極和對稱四極裝置視電阻率剖麵進行電阻率二維反縯研究.結果顯示:單極-單極裝置在橫嚮上隻要三維異常體中心的水平間距不小于兩者中心埋深之和,就可以基本將2箇三維結構分辨齣來;相同情況下,對稱四極裝置在橫嚮上的分辨效果優于單極-單極裝置;單極-單極裝置在垂嚮上的分辨要優于對稱四極裝置.
이용삼유유한차분방법진행심부삼유결구적전조솔삼유수치모의,대계산득도적단겁-단겁화대칭사겁장치시전조솔부면진행전조솔이유반연연구.결과현시:단겁-단겁장치재횡향상지요삼유이상체중심적수평간거불소우량자중심매심지화,취가이기본장2개삼유결구분변출래;상동정황하,대칭사겁장치재횡향상적분변효과우우단겁-단겁장치;단겁-단겁장치재수향상적분변요우우대칭사겁장치.
Numerical simutation for 3D model with deep structures was carried out by using 3D finite difference resistivity modeling method. 2D inversion of calculated apparent resistivity profiles of pole-pole and symmetric four-pole sounding was studied. The result indicates that pole-pole system can resolve 3D structures if the horizontal interval of the center of 3D abnormal bodies is not less than the total depth of the center of the two structures.Under the same conditions, symmetric four-pole system has horizontal resolution better than pole-pole system, and pole-pole system has vertical resotution better than symmetric four-pole system.