Titlebook: Hydrothermal Processes and Mineral Systems; Franco Pirajno Book 2009 Springer Science+Business Media B.V. 2009 Hydrothermal processes.Hydr

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demonstrating an origin that lies outside of the paraphyletic ‘synziphosurines.’ Horseshoe crab body fossils are exceptionally rare and are found mostly in shallow coastal and marginal marine Konservat-Lagerstätten deposits. Their sporadic occurrences document a post-Cambrian history of low overall

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Water and Hydrothermal Fluids on Earth,othermal processes and systems. Given the context of this book, this introduction is perhaps somewhat elementary and by no means exhaustive, but for the reader who wants to further his/her knowledge I provide a list of a range of useful and/or essential published works. Water is an oxide of hydrogen

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Tectonic Settings, Geodynamics and Temporal Evolution of Hydrothermal Mineral Systems,1990). Condie (1997, 2005) examined the tectonics and crustal evolution of the Earth. Review papers on tectonic settings of mineral systems include Kerrich et al. (2005) and Groves and Bierlein (2007). For the first part of this chapter I draw from these works and discuss the tectonic environment of

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Intrusion-Related Hydrothermal Mineral Systems,rray of transitional conditions can lead to a large number of ore deposit types and mineralisation styles that effectively defy a rigorous classification. For this reason descriptions of hydrothermal mineral systems, by necessity, must be regarded as end members or parts of a continuum. This simplif

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Skarn Systems,eralisation and laterally to skarn deposits, where carbonate rocks are present (see Fig. 5.4). Skarns are rocks dominated by calc-silicate minerals formed by replacement of carbonate lithologies either during regional metamorphism or by contact metasomatic processes related to igneous intrusions. Th

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