Abstract
Hot water is a very effective medium for the transport and enrichment of certain elements that are subsequently precipitated from the water. This can happen in very different places such as at a hot spring on the seabed, along a fault, in fine cracks above a granite pluton, in a cave, or in the pores of the rock. The space necessary for precipitation can even be created by simultaneously dissolving the surrounding rock in a process called replacement.
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Further Reading
Guilbert, J.M., and C.F. Park. 1986. The Geology of Ore Deposits. New York: WH Freeman.
Laznicka, P. 2010. Giant Metallic Deposits: Future Sources of Industrial Metals, 2nd ed. Heidelberg: Springer.
Misra, K.C. 2000. Understanding Mineral Deposits. Dordrecht, Niederlande: Kluwer Academic Publishers.
Neukirchen, F. 2012. Edelsteine: Brillante Zeugen für die Erforschung der Erde. Heidelberg: Springer Spektrum.
Okrusch, M., and S. Matthes. 2009. Mineralogie: Eine Einführung in die spezielle Mineralogie, Petrologie und Lagerstättenkunde, 8th ed. Heidelberg: Springer.
Pirajno, F. 2009. Hydrothermal Processes and Mineral Sytems. Heidelberg: Springer.
Pohl, W.L. 2011. Economic Geology. Chichester: Wiley-Blackwell.
Robb, L. 2005. Introduction to Ore-Forming Processes. Malden, MA: Blackwell Science.
Rothe, P. 2010. Schätze der Erde. Darmstadt: Primus Verlag.
Seidler, C. 2012. Deutschlands verborgene Rohstoffe: Kupfer. Hanser, München: Gold und seltene Erden.
Winter, J.D. 2001. Igneous and Metamorphic Petrology. New Jersey: Prentice Hall.
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Neukirchen, F., Ries, G. (2020). Hydrothermal Deposits. In: The World of Mineral Deposits. Springer, Cham. https://doi.org/10.1007/978-3-030-34346-0_4
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