3-DIMENSIONAL MISE-A-LA-MASSE MODELING APPLIED TO MAPPING FRACTURE-ZONES

被引:47
作者
BEASLEY, CW [1 ]
WARD, SH [1 ]
机构
[1] UNIV UTAH,RES INST,EARTH SCI LAB,SALT LAKE CITY,UT 84108
关键词
GEOPHYSICS - MATHEMATICAL TECHNIQUES - Integral Equations;
D O I
10.1190/1.1442044
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A numerical scheme applying the method of volume integral equations has been developed for borehole-to-borehole and borehole-to-surface modeling of the apparent resistivity response of a thin conductive body in a half-space; the inhomogeneity simulates a fracture zone in a geothermal system. The algorithm is applicable for the direct-current case when the buried electrode is either inside (mise-a-la-masse) or outside (near-miss) the body. In implementing the scheme, the integral equation is transformed into a matrix equation as a result of discretizing the inhomogeneity into rectangular cells.
引用
收藏
页码:98 / 113
页数:16
相关论文
共 15 条
[1]   A METHOD FOR CALCULATING MISE-A-LA-MASSE ANOMALIES IN THE CASE OF HIGH CONDUCTIVITY CONTRAST BY THE INTEGRAL-EQUATION TECHNIQUE [J].
ELORANTA, E .
GEOEXPLORATION, 1984, 22 (02) :77-88
[2]   3-DIMENSIONAL INDUCED POLARIZATION AND ELECTROMAGNETIC MODELING [J].
HOHMANN, GW .
GEOPHYSICS, 1975, 40 (02) :309-324
[3]  
KAUAHIKAUA J, 1980, GEOTHERM RES COUNC T, V4, P65
[4]  
MWENIFUMBO CJ, 1980, THESIS U W ONTARIO L
[5]  
NEWKIRK DJ, 1982, DOEID1207947 U UT DE
[6]   3-DIMENSIONAL TERRAIN CORRECTIONS FOR MISE-A-LA-MASSE AND MAGNETOMETRIC RESISTIVITY SURVEYS [J].
OPPLIGER, GL .
GEOPHYSICS, 1984, 49 (10) :1718-1729
[7]  
ROSS HP, 1984, DOESF121962 U UT RES
[8]  
Schlumberger C., 1920, ETUDE PROSPECTION EL
[9]  
SILL WR, 1978, 778 U UT DEP GEOL GE
[10]  
SILL WR, 1983, DOEID12079104 U UT R