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Colimaite : ウィキペディア英語版
Colimaite

Colimaite, the naturally occurring analog of synthetic K3VS4, is a sulfide mineral discovered in southwestern Mexico. The potassium-vanadium sulfide was collected from the crater of the Colima volcano. The mineral colimaite is named after the locality of this volcano 〔Ostrooumov, M., Taran, Y., Arellano-Jimenez, M., Ponse, A., and Reyes-Gasga, J. (2009) Colimaite, K3VS4 – anew potassium-vanadium sulfide mineral from the Colima volcano, State of Colima (Mexico) Revista Mexicana de Ciencias Geológicas, 26(3), 600-608〕 and has been approved in 2007, along with its mineral name, by the Commission on New Minerals, Nomenclature and Classification (CNMNC). It has been given the International Mineralogical Association number of IMA 2007-045.〔
==Composition==
The chemical formula of colimaite is K3VS4. The enrichment of vanadium in Colima’s volcanic gases make it unique.〔 The study of sulfur content in the fumaroles is also important, in order to know how an eruption could affect global climate due to SO2 emissions.〔Jugo, P.J. (2009), Sulfur content at sulfide saturation in oxidized magmas. Geology, 37(5), 415-418〕

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