FIELD: geophysical means of the Earth exploration.
SUBSTANCE: horizontal components of the electromagnetic field are measured at the Earth's surface, in the frequency range sufficient for the field penetration to the required depths at the points located nearby all existing boreholes where temperature is known or can be measured. For each frequency, the effective electrical conductivity is measured and one-dimensional inversion is performed. Mathematical processing is carried out with the help of artificial neuron networks.
EFFECT: providing possibility of Earth crust temperature forecast updating.
2 cl, 1 tbl
| Title | Year | Author | Number |
|---|---|---|---|
| METHOD OF TEMPERATURE PREDICTION AT DEPTH BELOW WELL BOTTOM | 2019 |
|
RU2717685C1 |
| OPEN POROSITY PREDICTION METHOD IN THE SPACE BETWEEN WELLS | 2019 |
|
RU2717740C1 |
| METHOD FOR MARINE ELECTRICAL EXPLORATION | 2017 |
|
RU2642492C1 |
| METHOD OF PREDICTING OPEN POROSITY AT DEPTH BELOW BOTTOMHOLE | 2018 |
|
RU2696669C1 |
| UNDERWATER OBSERVATORY | 2013 |
|
RU2546784C2 |
| METHOD FOR THREE-DIMENSIONAL SEISMIC ZONING OF THE LITHOSPHERE | 2019 |
|
RU2730419C1 |
| METHOD OF FORECAST OF CAPACITIVE PARAMETERS AND TYPE OF FLUID SATURATION OF RESERVOIRS | 2013 |
|
RU2540216C1 |
| UNDERWATER OBSERVATORY | 2011 |
|
RU2468395C1 |
| METHOD OF PREDICTING GEODYNAMIC PROCESSES FROM ANOMALIES OF VARIATION OF EARTH'S GEOMAGNETIC FIELD | 2012 |
|
RU2544261C2 |
| METHOD DESIGNED TO MONITOR LOCAL IRREGULARITIES AND GEODYNAMIC ZONES OF GEOLOGICAL SECTION TOP PART (GST) | 2008 |
|
RU2363965C1 |
