Articles | Volume 11, issue 1
https://doi.org/10.5194/se-11-1-2020
https://doi.org/10.5194/se-11-1-2020
Research article
 | 
07 Jan 2020
Research article |  | 07 Jan 2020

Magmatic sulfides in high-potassium calc-alkaline to shoshonitic and alkaline rocks

Ariadni A. Georgatou and Massimo Chiaradia

Related subject area

Subject area: Tectonic plate interactions, magma genesis, and lithosphere deformation at all scales | Editorial team: Geochemistry, mineralogy, petrology, and volcanology | Discipline: Petrology
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Cited articles

Agangi, A. and Reddy, S. M.: Open-system behaviour of magmatic fluid phase and transport of copper in arc magmas at Krakatau and Batur volcanoes, Indonesia, J. Volcanol. Geoth. Res., 327, 669–686, https://doi.org/10.1016/j.jvolgeores.2016.10.006, 2016. 
Agostini, S., Doglioni, C., Innocenti, F., Manetti, P., Tonarini, S., and Savaşçin, M. Y.: The transition from subduction-related to intraplate Neogene magmatism in the Western Anatolia and Aegean area, Geol. S. Am. S., 418, 1–15, https://doi.org/10.1130/2007.2418(01), 2007. 
Aldanmaz, E.: Mantle source characteristics of alkali basalts and basanites in an extensional intracontinental plate setting, western Anatolia, Turkey: implications for multi-stage melting, Int. Geol. Rev., 44, 440–457, https://doi.org/10.2747/0020-6814.44.5.440, 2002. 
Aldanmaz, E., Pickard, Μ., Meisel, T., Altunkaynak, Ş., Sayıt, K., Şen, P., Hanan, B. B., and Furman, T.: Source components and magmatic processes in the genesis of Miocene to Quaternary lavas in western Turkey: Constraints from HSE distribution and Hf-Pb-Os isotopes, Contrib. Mineral. Petrol., 170, 1–20, https://doi.org/10.1007/s00410-015-1176-x, 2015. 
Alici, P., Temel, A., and Gourgaud, A.: Pb–Nd–Sr isotope and trace element geochemistry of Quaternary extension-related alkaline volcanism: a case study of Kula region (Western Anatolia, Turkey), J. Volcanol. Geoth. Res., 115, 487–510, https://doi.org/10.1016/S0377-0273(01)00328-6, 2002. 
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Short summary
We study the petrographical and geochemical occurrence of magmatic sulfide minerals in volcanic rocks for areas characterised by different geodynamic settings, some of which are associated with porphyry (Cu and/or Au) and Au epithermal mineralisation. The aim is to investigate the role of magmatic sulfide saturation processes in depth for ore generation in the surface.