Tm. Williams et al., Regional geochemical reconnaissance of the Cordillera Occidental of Ecuador: economic and environmental applications, APPL GEOCH, 15(4), 2000, pp. 531-550
A regional geochemical reconnaissance survey of the Cordillera Occidental o
f Ecuador was initiated in 1995 as a sub-component of a wider Mining Develo
pment and Environmental Control Technical Assistance Project (PRODEMINCA) i
n Ecuador. The 36,000 km(2) survey area encompasses oceanic and continental
-margin volcanosedimentary terranes with known occurrences of porphyry-styl
e Cu-Mo, exhalative massive sulphide, epithermal Au and mesothermal polymet
allic mineralisation. A survey sample medium of < 177 mu m stream sediments
was selected following an orientation study in the vicinity of known porph
yry Cu mineralisation. In the 2-4 degrees S sector of the Cordillera Occide
ntal for which data are presented, 4850 drainage samples were collected at
an average density of 1 per 2.57 km2. All were analysed for 36 major and tr
ace elements (Au, Ag, Cu, Pb, Zn, Mo, Ni, Co, Cd, Bi, As, Sb, Fe, Hg, Mn, T
e, Pa, Cr V, Sn, W, La, Al, Mg, Ca, Na, K, Sr, Y, Ga, Li, Nb, Sc, Ta, Ti, Z
r). A stringent quality-control procedure included the systematic analysis
of certified reference samples, field duplicates and replicates, data for w
hich were used to calculate analytical precision, temporal drift and practi
cal detection limits. Results for this part of the cordillera highlight the
contrasting lithogeochemical signatures of the ocean-floor basalt terrane
(Pallatanga Unit), the island-arc terrane of the Macuchi Unit, the continen
tal volcanics of the Saraguro Group and the acid and intermediate lavas ext
ruded from the Late Miocene to the Quaternary. Regional geochemical images
for Au and associated pathfinder elements are dominated by anomalies relati
ng to known mines and prospects. New exploration targets, often inconspicuo
us at the regional scale, have however been identified through the normalis
ation of data for individual lithological units against their respective ge
ochemical backgrounds. In addition to mineral exploration, the drainage geo
chemical dataset for the Cordillera Occidental provides an unparalleled env
ironmental baseline against which the impacts of future anthropogenic activ
ities (including mining) may be assessed. A basis for the formulation of pr
agmatic sediment quality criteria and for the identification of natural geo
chemical hazards is also provided. (C) 2000 Elsevier Science Ltd. All right
s reserved.