Mm. Konstantinov et Sf. Strujkov, APPLICATION OF INDICATOR HALOS (SIGNS OF ORE REMOBILIZATION) IN EXPLORATION FOR BLIND GOLD AND SILVER DEPOSITS, Journal of geochemical exploration, 54(1), 1995, pp. 1-17
The indicator method is a new, effective exploration method for blind
ore. This method is based on the partial redeposition of ore and vein
matter in the overlying rocks as a result of the magmatic, hydrotherma
l, and tectonic processes. Studies of ''standard'' deposits with blind
ore show that geochemical and mineral halos of redeposited matter fro
m blind ore bodies (indicator halos) occur in post-ore geological bodi
es termed ''lifts'' - faults, dikes, and quartz veins within the overl
ying rock. The indicator method uses special sampling of the past-ore
lift structures. The proposed technique can be used to search for blin
d ore mineralization in different geological environments. The post-or
e dikes are sampled across the strike of the prospective blind ore str
uctures. Dike material is analyzed for Au, Ag, Sn, Pb, Zn, Cu, CO2, an
d SO4. Experiments completed in the well-studied Ducat mining field su
ggest that this method is applicable over a vertical range of more tha
n 200 m. The ''resolution'' identifies individual blind ore bodies as
well as groups of orebodies. The post-ore fault method includes sampli
ng of the sand-size fraction of cataclastic material from these fault
zones, extraction of the paramagnetic fraction, and semi-quantitative
analysis of this fraction for the content of indicator elements. Our s
tudy has shown this method to be effective in exploration for blind or
e at 1 : 10 000 scale. The vertical range of this method is more than
300 m. The possibility of predicting the composition and average gold
and silver grades within the blind ore is also shown. Post-ore quartz
veins are sampled and rapidly checked for selected indicator elements
using a portable X-ray fluorescence (XRF) instrument. The testing of t
his method has identified several new orebodies. With the aim of impro
ving the sampling methods, the sample preparation methods and the anal
ysis of the samples for the indicator halos in the post-ore faults, st
udies of the following modifications to the indicator method were carr
ied out: (1) sampling of the fine (rock dust) fraction from fault zone
s; (2) sampling of the sand-size fraction by the rapid XRF method; and
(3) sampling of mosses in the post-ore fault zones (the bryogeochemic
al method). The proposed modifications suggest that these methods can
be used in a wide range of geographical landscapes.