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• W2152717032 abstract "Sir: The El Teniente Cu-Mo deposit in central Chile is an extraordinary accumulation of Cu-Mo ore (Fig. 1⇓), and we welcome the opportunity provided by Skewes and Stern (2007) to discuss and clarify several important issues regarding its classification and interpretation, and to address several incorrect assertions that they make regarding our manuscript (Cannell et al., 2005). We have interpreted El Teniente to be a typical porphyry deposit, in terms of its alteration assemblages, vein and breccia styles, and spatial and temporal relationships between Cu-Mo mineralization and felsic porphyries. Skewes and Stern (2007) dispute our claims that mineralization occurred primarily in veins and was related to felsic intrusive activity. They also take issue with our interpretations of the various geochronological datasets from El Teniente and our classification of El Teniente as a porphyry Cu-Mo deposit. We address each of these in turn below.In order to facilitate the following discussion, Table 1⇓ correlates the geologic nomenclature of Skewes and Stern (2007) with that of Cannell et al. (2005). Figures 1⇓ and 2⇓ illustrate the location of the main geologic units on underground mine level 6 at El Teniente. Also shown on Figure 1⇓ are the approximate locations of the hypogene sulfide mineral zones. Figure 2⇓ shows the block model of Mo grades in the mine. For more details of geologic relationships at El Teniente, refer to figure 4 of Cannell et al. (2005) and figures 4 and 5 of Skewes et al. (2002). Although the dacite porphyry dike is shown as a single unit on Figure 1⇓, note that Rojas (2002, 2003) mapped multiple phases within this composite intrusive body.Skewes and Stern (2007) criticized our use of what they assert to be an “outdated map of hypogene mineralization” …" @default.
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• W2152717032 date "2005-08-01" @default.
• W2152717032 modified "2023-10-17" @default.
• W2152717032 title "Geology, Mineralization, Alteration, and Structural Evolution of the El Teniente Porphyry Cu-Mo Deposit" @default.
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• W2152717032 doi "https://doi.org/10.2113/gsecongeo.100.5.979" @default.
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