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O'Keefe & Thiel 1991
O'Keefe, S.G. and Thiel, D.V. (1991). Electromagnetic emissions during rock blasting. Geophysical Research Letters 18: doi: 10.1029/91GL01076. issn: 0094-8276.

Radio emissions during quarry blasting have been recorded in the audio frequency band. Three distinct mechanisms are suggested to explain the observed results; rock fracture at the time of the explosion, charged rocks discharging on impact with the pit floor and micro-fracture of the remaining rock wall due to pressure adjustment of the bench behind the blast. The last mechanism was evident by a train of discrete impulses recorded for up to one minute after the blast. It is assumed that during this time the rock behind the blast was subjected to a significant change in pressure. This may be related to ELF observations during earthquakes. ¿American Geophysical Union 1991

BACKGROUND DATA FILES

Abstract

Keywords
Electromagnetics, Instrumentation and techniques, Physical Properties of Rocks, Fracture and flow, Radio Science, Electromagnetic noise and interference
Journal
Geophysical Research Letters
http://www.agu.org/journals/gl/
Publisher
American Geophysical Union
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