| 摘要 |
FIELD: geology. SUBSTANCE: method makes it possible to enhance geological efficiency and includes measurement of gravity force, transformation of fields of total norm gradient and generation of coordinates x, z of sources of anomalies in section. It is based on establishment of parameters of observation network, on determination of optimum parameters of transformation of fields of function of total norm gradient, on transformation of fields of chosen type with parameters close to optimal ones, on identification of axes of phase coincidence of anomalous zones, on establishment of character of source of anomalies and on determination of their coordinates. Result of given method lies in preparation of diagram of positioning of dense inhomogeneities of section (subhorizontal boundaries of section, subvertical contacts) without usage of a prior geological-geophysical information. EFFECT: enhanced geological efficiency of method. |
