Ce. Dunn et Ge. Ray, A COMPARISON OF LITHOGEOCHEMICAL AND BIOGEOCHEMICAL PATTERNS ASSOCIATED WITH GOLD MINERALIZATION IN MOUNTAINOUS TERRAIN OF SOUTHERN BRITISH-COLUMBIA, Economic geology and the bulletin of the Society of Economic Geologists, 90(8), 1995, pp. 2232-2243
Analyses of rock and tree tissue samples collected from an area surrou
nding gold mineralization at tile inactive Carolin mine show geochemic
al distribution patterns with some striking similarities and significa
nt differences. Lithogeochemical sampling outlines a zone, several hun
dred meters across, in which hydrothermally altered rocks are enriched
in Na and depleted in K and Ba. Within this zone lies a 40 m wide are
a where the rocks are enriched sporadically in Au and As. The Au, As,
and Na biogeochemical halos outlined by twigs and needles of the most
common tree in the survey area, Pacific silver fir (Abies amabilis), a
re significantly larger in areal extent than the respective lithogeoch
emical halos of these elements. This is a result of physical and chemi
cal downslope dispersion of these elements in tile colluvium and groun
d water. Differences in the biogeochemical and lithogeochemical patter
ns of Ba and Cr are attributed to the availability of these elements t
o the plant roots: in the hydrothermally altered rocks, Ba and Cr are
more readily released from the crystal structure of such minerals as s
ericite and fuchsite than in the nonaltered rocks where these elements
are roost likely contained in K feldspar and chromite. This comparati
ve study indicates that the biogeochemical method is a valuable approa
ch to gold exploration in the mountainous terrain of British Columbia,
because trees can integrate and amplify the geochemical signatures of
rocks, surficial deposits, and ground water and give rise to large an
d intense anomalies derived from narrow zones of mineralization. Sampl
ing and analysis of tree tissues is a cost-efficient method to identif
y areas of metal enrichment. At the Carolin mine, reconnaissance-levee
sampling at a density of a few trees per square kilometer would have
been sufficient to identify the area of anomalously high Au, As, and N
a concentrations. Reconnaissance biogeochemical surveys at this sample
density in rugged terrain may assist in identifying valleys hosting m
ineralization that subcrops beneath a veneer of surficial deposits, an
d thereby, provide a focus for followup prospecting by lithogeochemica
l or other methods of exploration.