Abstract
All authors which were concerned with Monte Valerio supported pyrometasomatic or pneumatolytic-hydrothermal genetic processes, linked to the Mio-Pliocene acidic magmatic activity. The present authors, on the basis of factual observations directly achieved and/or reported in the existing literature, suggest synsedimentary tin deposition, followed by partial supergene remobilization, and assign a very limited role (if any) to the Mio-Pliocene magmatism and metamorphism on tin distribution.
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© 1982 Springer-Verlag Berlin Heidelberg
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Venerandi-Pirri, I., Zuffardi, P. (1982). The Tin Deposit of Monte Valerio (Tuscany, Italy): Pneumatolytic-Hydrothermal or Sedimentary-Remobilization Processes?. In: Amstutz, G.C., et al. Ore Genesis. Special Publication of the Society for Geology Applied to Mineral Deposits, vol 2. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-68344-2_6
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DOI: https://doi.org/10.1007/978-3-642-68344-2_6
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