Occurrence of a new sulphate mineral: Ca7Na3K(SO4)9 in the Emet borate deposits, western Anatolia (Turkey)

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RECERCAT Home > Universitat de Barcelona > Mineralogia, Petrologia i Geologia Aplicada > Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada) > View document

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dc.contributor	Universitat de Barcelona
dc.contributor.author	García-Veigas, Francisco Javier
dc.contributor.author	Ortí Cabo, Federico
dc.contributor.author	Rosell, Laura (Rosell i Ortiz)
dc.contributor.author	Gündogan, Ibrahim
dc.contributor.author	Helvaci, Cahit
dc.date	2014-03-26T10:03:52Z
dc.date	2014-03-26T10:03:52Z
dc.date	2010
dc.date	2014-03-25T15:52:24Z
dc.identifier.citation	1641-7291
dc.identifier.citation	586126
dc.identifier.uri	http://hdl.handle.net/2445/52988
dc.format	8 p.
dc.format	application/pdf
dc.language.iso	eng
dc.publisher	Polish Geological Institute-National Research Institute
dc.relation	Geological Quarterly, 2010, vol. 54, num. 4, p. 431-438
dc.rights	(c) Polish Geological Institute-National Research Institute, 2010
dc.rights	info:eu-repo/semantics/openAccess
dc.subject	Miocè
dc.subject	Evaporites
dc.subject	Miocene
dc.subject	Evaporites
dc.title	Occurrence of a new sulphate mineral: Ca7Na3K(SO4)9 in the Emet borate deposits, western Anatolia (Turkey)
dc.type	info:eu-repo/semantics/article
dc.type	info:eu-repo/semantics/publishedVersion
dc.description.abstract	This paper is a preliminary report on the petrographic and geochemical characteristics of a new sulphate mineral associated with lacustrine glauberite layers. This mineral is present in two boreholes recently drilled in the Emet borate district (Mio-cene; western Anatolia , Turkey). The evaporitic succession in these boreholes is mainly formed of a glauber ite-probertiteal-ternation. We suggest the name"emetite", after the town of Emet, for the new sulphate mineral, although the fine crystal size hinders the appropriate chemical and crystallographic characterization required to propose it as a new mineral to the International Mineralogical Association. .

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