U N I V E R S I D A D D E C O N C E P C I Ó N DEPARTAMENTO DE CIENCIAS DE LA TIERRA 10° CONGRESO GEOLÓGICO CHILENO 2003 THE CHUQUICAMATA INTRUSIVE COMPLEX: ITS RELATION TO THE FORTUNA INTRUSIVE COMPLEX, AND THE ROLE OF THE BANCO PORPHYRY IN THE POTASSIC ALTERATION ZONE ARNOTT, A. M. and ZENTILLI, M. Department of Earth Sciences, Dalhousie University, Halifax, NS, B3H 3J5, Canada (
[email protected];
[email protected]) INTRODUCCION The geology of Chuquicamata, Chile, recently reviewed by Ossandón et al. (2001) is relatively well understood. However, there are some major questions that remain controversial, a few of which are addressed in this extended abstract, reflecting some of the results of a doctoral thesis recently completed by Arnott (2003), the latest of a series of student theses supervised by M. Zentilli at Dalhousie University (e.g. Maksaev, 1990; Lewis, 1996; Lindsay et al., 1996; Pemberton, 1997; Lindsay, 1998). The Chuquicamata Intrusive Complex (CIC), developed during the Eocene-Oligocene (e.g. Zentilli et al., 1994; 1995; Reynolds et al. 1998; Mathur et al., 2000; Ballard et al., 2001) is composed of the heavily mineralized and hydrothermally altered Este, Oeste and Banco porphyries, and truncated by the West Fault. Juxtaposed across the West Fault lies the unaltered and unmineralized Fortuna Intrusive Complex (FIC) (Figure 1). The initial objective of this study was to unravel the evolution of hydrothermal alteration and its relation to the intrusion of the various igneous phases. At the same time it was intended to answer some fundamental questions with practical implications, such as: 1) Is the FIC genetically related to the CIC or an extraneous body? 2) Does the potassic alteration zone reflect an overprint by an intrusion younger than the Este Porphyry (i.e.