Factorial kriging has been used in geochemical exploration for the estimati
on and cartography of the spatial components of the variables, helping with
the identification and interpretation of geochemical anomalies. Those spat
ial components appear by the decomposition of the variables in its several
structural components, given by the variograms. In this paper a new form of
factorial kriging is introduced, by using the geologic information as an e
xternal drift. This was achieved considering as an external variable (exter
nal drift) sample co-ordinates on the first axis resultant from a principal
component analysis (PCA), interpreted as a lithological factor. With this
type of geostatistical technique each point appears in the resultant maps a
s a combination of geochemical and geological information, attending the ge
ographic localization of the samples. This technique was tested on a set of
2450 sediment samples collected on a 640 km(2) area, between the Tras-os-M
ontes e Bite Douro and the Beira Alta regions. From the 34 initial elements
analyzed (10 major elements P2O5, SiO2, Al2O3 Fe2O3, MgO, CaO, Na2O, K2O,
TiO2 and MnO expressed in oxide percentage and 24 elements expressed in ppm
As, Bi, Ag, Sb, W, B, Cu, Pb, Zn, Sn, Nb, Li, Be, Zr, Y, La, Ba, Cd, Mo, V
, Cr, Co, Ni and Sr) only the results obtained for 2 of them are presented
in this work. The first was Sn, which is associated with some mineralisatio
n in this region and the other one was Zn, which shows similar behavior in
the whole area, with the exception of a small region. (C) 2001 Elsevier Sci
ence Ltd. All rights reserved.