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Evaporites pp 1469–1589Cite as

Lower Temperature Metals in an Evaporitic Framework

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Abstract

Most subsurface evaporites ultimately dissolve and, through their ongoing dissolution and alteration, can create conditions suitable for metal enrichment and entrapment in subsurface settings ranging from the burial diagenetic through to the metamorphic and igneous realms. Within this framework, this chapter explores relationships between evaporites and lower temperature ore deposits, where ore is defined as a mineral, or an aggregate of minerals, from which a valuable constituent, especially a metal, can be profitably mined or extracted. The next chapter explores the significance of dissolving and altering evaporites in ore deposits formed in the higher temperature igneous and metamorphic realms.

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Notes

  1. 1.

    Compact sphalerite and wurtzite masses of a pale brown colour, occurring in concentric layers with reniform surfaces, which also may contain pyrite and galena.

  2. 2.

    Pinolitic describes crystal splay textures made up of elongate lenticular crystals of ferroan to magnesian carbonate (siderite, ankerite, brun-nerite, magnesite) with outlines in two dimensions that resemble the patterning along the outside of a closed or partially closed pine-cone (Pinus pinea).

  3. 3.

    The coxco features were correctly interpreted as marine aragonite splay pseudomorphs Brown et al. (1978), then misidentified as pseudomorphs after radiating gypsum splay in subsequent studies; e.g. Walker et al. 1977; Jackson et al. 1987)

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  1. Department of Geology, Chulalongkorn University, Bangkok, Thailand

    John K. Warren

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Warren, J.K. (2016). Lower Temperature Metals in an Evaporitic Framework. In: Evaporites. Springer, Cham. https://doi.org/10.1007/978-3-319-13512-0_15

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