Application of geostatistics to identify gold-rich areas in the Finisterre-Fervenza region, NW Spain

Citation
R. Jimenez-espinosa et M. Chica-olmo, Application of geostatistics to identify gold-rich areas in the Finisterre-Fervenza region, NW Spain, APPL GEOCH, 14(1), 1999, pp. 133-145
Citations number
33
Categorie Soggetti
Earth Sciences
Journal title
APPLIED GEOCHEMISTRY
ISSN journal
08832927 → ACNP
Volume
14
Issue
1
Year of publication
1999
Pages
133 - 145
Database
ISI
SICI code
0883-2927(199901)14:1<133:AOGTIG>2.0.ZU;2-R
Abstract
Three univariate geostatistical methods of estimation are applied to a geoc hemical data set. The studied methods are: ordinary kriging (cross-validati on), factorial kriging, and indicator kriging. These techniques use the pro babilistic and spatial behaviour of geochemical variables, giving a tool fo r identifying potential anomalous areas to locate mineralization. Ordinary kriging is easy to apply and to interpret the results. It has the advantage of using the same experimental grid points for its estimates, and no addit ional grid points are needed. Factorial kriging decomposes the raw variable into as many components as there are identified structures in the variogra m. This, however, is a complex method and its application is more difficult than that of ordinary or indicator kriging. The main advantages of indicat or kriging are that data are used by their rank order, being more robust ab out outlier values, and that the presentation of results is simple. Neverth eless, indicator kriging is incapable of separating anomalous values and th e high values from the background, which have a behaviour different to the anomaly. In this work, the results of the application of these 3 kriging me thods to a;set of mineral exploration data obtained from a geochemical surv ey carried out in NW Spain are presented. This area is characterised by the presence of Au mineral occurrences. The kriging methods were applied to As , considered as a pathfinder of Au in this area. Numerical treatment of Au is not applicable, because it presents most values equal to the detection l imit, and a series of extreme values. The results of the application of ord inary kriging, factorial kriging and indicator kriging to As make possible the location of a series of rich values, sited along a N-S shear zone, cons idered a structure related to the presence of Au. (C) 1998 Elsevier Science Ltd. All rights reserved.