Method utilizing electromagnetic wave pulses for determining the locations of boundary surfaces of underground mineral deposits

A method of determining the location or locations of one or more compositional discontinuities in salt deposits by measuring the travel time of electromagnetic waves reflected off of boundary surfaces between underground bodies of differing mineralogical characteristics, the method comprising

• generating powerful pulses of electromagnetic waves such that the waves have a frequency between 1 and 500 MHz, the pulses formed by the electromagnetic waves having a pulse duration of 0.1 to 1 microsecond and a pulse-repetition frequency of 10 to 1000 Hz, and radiating the thusly generated pulses of electromagnetic waves into the solid body of a mountain or other geological structure from within the interior of an underground excavation,
• said generating and radiating of powerful pulses of electromagnetic waves comprising the following procedure:
• positioning a dipole antenna having a spark gap defined by its two antenna elements close to but not in contact with a wall of the underground excavation,
• building up a static charge on the two antenna elements of the dipole antenna by connecting the output of a high-voltage low-power D.C. generator across the two antenna elements via two high-resistance charging resistors each connected to a respective one of the two antenna elements of the dipole antenna, so that the high-voltage low-power D.C. generator furnishes energy at low power to the dipole antenna, the resulting increase of static energy on the antenna elements eventually reaching the ignition voltage of the antenna's spark gap, whereupon the static charge on the two antenna elements is rapidly dissipated due to attenuation resulting from the antenna spark gap's electric arc spark resistance thereby producing from the energy previously supplied to the antenna by the lower-power D.C. generator a higher-power pulse of electromagnetic waves, and then recommencing the build-up of static charge on the antenna from the low-power D.C. generator until another such pulse of electromagnetic waves is produced, and repeating this procedure to produce a series of such pulses,
• the radiation transmitted from the dipole antenna being reflected back from the one or more boundary surfaces with different respective travel times;
• and
• receiving the reflected-back radiation utilizing a receiving antenna positioned close to but not in contact with a wall of the underground excavation and making a recording thereof.