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- W4315694680 abstract "Most economically significant ore deposits exist because of the advective transport of solutes and heat by flowing groundwater. Mobilization, transport, and deposition of chemical species are all linked to fluid flow. The thermal effects of flowing groundwater can explain the emplacement of some relatively high-temperature ore deposits at anomalously shallow depths. Although many ore deposits are associated with magmatic– hydrothermal systems, in this chapter we focus on the important subset of ore deposits formed in sedimentary basins with no associated igneous rocks. In particular, we will emphasize Mississippi Valley type (MVT) lead–zinc deposits, other stratiformbase-metal deposits, and both tabular and unconformity-type uranium deposits. Each type of deposit is economically significant, was apparently controlled by regional patterns of groundwater flow, and has been the subject of “paleohydrologic” reconstructions over the past several decades. They are thus of particular interest to hydrogeologists.We will then consider two examples of economic mineralization caused by essentially in situ diagenetic processes: supergene enrichment of copper porphyry deposits and Colombian emeralds. The specific material in this chapter is complemented by the generalized discussions of chemical and heat transport in Chapters 3 and 4 and, more directly, by the discussion of basin-scale flow and transport in Chapter 5. Ore deposits associated with magmatic–hydrothermal systems are considered briefly in Section 8.8 and in considerable detail elsewhere (e.g., Barnes, 1979, 1997; Sillitoe and Hedenquist, 2003)." @default.
- W4315694680 created "2023-01-12" @default.
- W4315694680 date "2006-05-04" @default.
- W4315694680 modified "2023-09-27" @default.
- W4315694680 title "Ore deposits" @default.
- W4315694680 doi "https://doi.org/10.1017/9780511807855.007" @default.
- W4315694680 hasPublicationYear "2006" @default.
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