Abstract: The disclosure is directed to an improved method and apparatus for subsurface electromagnetic logging in a borehole wherein means are provided to detect transverse magnetic mode components and to either correct for these spurious components in the processing of the received signals or to generate suitable cancelling signals.

Abstract: The disclosure is directed to an improved method and apparatus for subsurface electromagnetic logging in a borehole wherein means are provided to detect transverse magnetic mode components and to either correct for these spurious components in the processing of the received signals or to generate suitable cancelling signals.

Abstract: The disclosure is directed to a technique used for determining the mudcake-corrected water-filled porosity of formations surrounding a borehole, and which can also be used for determining the thickness of the mudcake formed on the borehole. Microwave electromagnetic energy is transmitted into the formations. Near and far receiving antennas are employed for receiving microwave electromagnetic energy from the formations. Means responsive to the outputs of the receiving antennas are provided for obtaining a travel-time-dependent differential measurement. Further means, responsive to the output of one of the antennas, are provided for obtaining a travel-time-dependent direct measurement. Finally, means are provided for determining the mudcake-corrected water-filled porosity of the formations from the differential and direct measurements. The mudcake thickness may also be determined from the differential and direct measurements.

Abstract: The disclosure is directed to an apparatus and method for determining dielectric constant and/or conductivity of earth formations surrounding a borehole. Electromagnetic energy is generated at a first location in the borehole. The relative attenuation of the electromagnetic energy is detected at a second location in the borehole. The detection is preferably performed using a first or "close" differential receiver arrangement. The relative phase of the electromagnetic energy is detected at a third location in the borehole, the third location being spaced farther from the first location than is the second location; in other words, the second location is between the first and third locations. The relative phase shift of the electromagnetic energy is measured by a second or "far" differential receiver arrangement located at the third location in the borehole.

Abstract: The disclosure is directed to an apparatus and method for determining dielectric constant and/or conductivity of earth formations surrounding a borehole. Electromagnetic energy is generated at a first location in the borehole. The relative attenuation of the electromagnetic energy is detected at a second location in the borehole. The detection is preferably performed using a first or "close" differential receiver arrangement. The relative phase of the electromagnetic energy is detected at a third location in the borehole, the third location being spaced farther from the first location than is the second location; in other words, the second location is between the first and third locations. The relative phase shift of the electromagnetic energy is measured by a second or "far" differential receiver arrangement located at the third location in the borehole.