FIELD: deep probing in search for gas and oil fields. SUBSTANCE: parameters of inhomogeneity are brought out to light by results of advance studies. Area Qin of this inhomogeneity is calculated with its projection on day surface. Area size on which observations are conducted is calculated by formula Q=Qin+ h2/2,, where h is depth of bedding of inhomogeneity. Maximal and minimal distances between sources of field are calculated by equations ; , where α is measurement error. Geophones are arranged by system of profiles with spacing Dy between geophones. At least two sources of field are positioned in parallel to inhomogeneity on opposite sides of it. Electric current same in value and direction is passed. Derivative of vertical component of vector of magnetic induction and first horizontal components of electromagnetic field U
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Authors
Dates
1997-03-27—Published
1994-05-26—Filed