Successful application of ground‐penetrating radar in the exploration of gem tourmaline pegmatites of southern California

Application of ground-penetrating radar has been successful in delineating gem-bearing zones in the Himalaya pegmatite mine of the Mesa Grande district of southern California. The high frequency of the electromagnetic signal allows features as small as a few centimetres to be resolved within 1-2 m of the surface of a mine wall. Careful initial set-up consisted of: (i) selection of antennae with sufficiently high central frequencies; (ii) recording with a short time of scan to reduce end-of-scan noise levels; (iii) choosing appropriate colour schemes to highlight extreme amplitude variations. Operation during data collection consisted of pre-painting marking points on the mine face and air launching the signal to reduce false anomalies caused by rocking of the antenna on the rough surfaces. Data processing using the Hilbert transform provided images of the cavity geometry that were then used by the blasting captain for accurate placement of explosives. The instantaneous frequency plot was found to be effective in distinguishing air-filled from clay-filled pockets, and the instantaneous phase plot was helpful in selecting potential targets where the amplitude was less than the maximum range. When carefully used in conjunction with good knowledge of the geological conditions, the method promises to provide an important tool for mapping internal structures of pegmatites, thus assisting future mining activities.

[1]  Steven A. Arcone,et al.  Ground-penetrating radar reflection profiling of groundwater and bedrock in an area of discontinuous permafrost , 1998 .

[2]  Georadar anisotropy in the Gotthard Gneiss, Switzerland , 1997 .

[3]  George A. McMechan,et al.  GPR characterization of buried tanks and pipes , 1997 .

[4]  Dean Goodman,et al.  Ground-Penetrating Radar: An Introduction for Archaeologists , 1997 .

[5]  Mark Grasmueck,et al.  3-D ground‐penetrating radar applied to fracture imaging in gneiss , 1996 .

[6]  O. Olsson,et al.  BOREHOLE RADAR APPLIED TO THE CHARACTERIZATION OF HYDRAULICALLY CONDUCTIVE FRACTURE ZONES IN CRYSTALLINE ROCK1 , 1992 .

[7]  J. M. Glover Void Detection using Standing Wave Analysis , 1992 .

[8]  David C. Nobes,et al.  Preliminary evaluation of GPR for nickel laterite exploration , 2000, International Conference on Ground Penetrating Radar.

[9]  J. Cook RADAR TRANSPARENCIES OF MINE AND TUNNEL ROCKS , 1975 .

[10]  Peter F. Ulriksen,et al.  Application of impulse radar to civil engineering , 1982 .

[11]  Jesse Fisher,et al.  The Geology, Mineralogy, and History of the Himalaya Mine, Mesa Grande, San Diego County, California , 1998 .

[12]  Jeffrey J. Daniels,et al.  Locating caves, tunnels and mines , 1988 .

[13]  R. G. Gastil,et al.  K-Ar Apparent Ages, Peninsular Ranges Batholith, Southern California and Baja California , 1975 .

[14]  J. Deen,et al.  MEASURED UNDERWATER NEAR‐FIELD E‐PATTERNS OF A PULSED, HORIZONTAL DIPOLE ANTENNA IN AIR: COMPARISON WITH THE THEORY OF THE CONTINUOUS WAVE, INFINITESIMAL ELECTRIC DIPOLE1 , 1990 .

[15]  Declan Vogt,et al.  Application of borehole radar to South Africa's ultradeep gold mining environment , 2000, International Conference on Ground Penetrating Radar.

[16]  Gilles Grandjean,et al.  Frequency–wavenumber modelling and migration of 2D GPR data in moderately heterogeneous dispersive media , 1998 .

[17]  F. Cook Applications of Geophysics in Gemstone Exploration , 1997 .

[18]  L. T. Dolphin,et al.  Radar probing of Victorio Peak, New Mexico , 1978 .

[19]  D. Goodman Ground‐penetrating radar simulation in engineering and archaeology , 1994 .

[20]  I. D. Longstaff,et al.  Gated stepped-frequency ground penetrating radar , 2000 .

[21]  S. Tillard Radar experiments in isotropic and anisotropic geological formations (granite and schists)1 , 1994 .

[22]  M. Taner,et al.  Complex seismic trace analysis , 1979 .