FIELD: geology. SUBSTANCE: method involves mounting at least one seismic emitter and regional group of seismic receivers, application of pulse to each seismic emitter, using delays if two ore more seismic receivers are mounted, in order to provide focusing of total sounding beam for each requested point of region under investigation. Then method involves measuring signals which are emitted by each requested point and comparison of their power, and detecting non- homogeneity after processing of received data. EFFECT: increased resolution and reliability of detection of objects in region under investigation.
Title | Year | Author | Number |
---|---|---|---|
METHOD OF SEISMIC PROSPECTING | 1997 |
|
RU2136018C1 |
METHOD FOR SEISMIC PROSPECTING | 1997 |
|
RU2145097C1 |
PROCESS OF SEISMIC MICROZONING | 1996 |
|
RU2105997C1 |
METHOD OF SEISMIC MICROZONING | 1996 |
|
RU2105996C1 |
PROCESS OF SEISMIC MICROZONING | 1996 |
|
RU2105998C1 |
PROCESS OF SEISMIC MICROZONING | 1996 |
|
RU2105995C1 |
METHOD OF SEISMIC PROSPECTING | 0 |
|
SU1000962A1 |
METHOD OF RAPID PREDICTION OF EARTHQUAKES, TECTONIC AND TECHNOGENEOUS SHIFTS | 1996 |
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RU2106001C1 |
PROCESS OF SEISMIC MICROZONING | 1996 |
|
RU2099751C1 |
METHOD FOR DETECTION OF NON-COMPENSATED ELECTRIC CHARGE OF MATERIAL BODIES | 1998 |
|
RU2145103C1 |
Authors
Dates
1999-04-27—Published
1997-08-18—Filed