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Lattice deformation of blue halite from Zechstein evaporite basin : Kłodawa Salt Mine, Central Poland

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Lattice deformation of blue halite from Zechstein evaporite basin : Kłodawa Salt Mine, Central Poland

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dc.contributor.author Zelek, Sylwia pl
dc.contributor.author Stadnicka, Katarzyna [SAP11004149] pl
dc.contributor.author Toboła, Tomasz pl
dc.contributor.author Natkaniec-Nowak, Lucyna pl
dc.date.accessioned 2015-06-09T12:18:23Z
dc.date.available 2015-06-09T12:18:23Z
dc.date.issued 2014 pl
dc.identifier.issn 0930-0708 pl
dc.identifier.uri http://ruj.uj.edu.pl/xmlui/handle/item/9142
dc.language eng pl
dc.rights Udzielam licencji. Uznanie autorstwa 4.0 Międzynarodowa *
dc.rights.uri http://creativecommons.org/licenses/by/4.0/pl/legalcode *
dc.title Lattice deformation of blue halite from Zechstein evaporite basin : Kłodawa Salt Mine, Central Poland pl
dc.type JournalArticle pl
dc.description.physical 619-631 pl
dc.identifier.weblink https://link.springer.com/content/pdf/10.1007%2Fs00710-014-0323-9.pdf pl
dc.abstract.en Outcrops of natural blue and purple halite crystals have been found in K ł odawa (Poland) salt deposit originating from the Permian (Zechstein) salt formation within tectonic zones. Field works carried out on various levels of K ł odawa Salt Mine indicated differencesbothinintensity ofthe hue and in the size of the outcrops. Their occurrence was connected with the presence of epigenetic sediments rich in potassium. For the samples of blue ha lite, an optical anisotropy (birefringence) was observed for both standard mineralogical thin sections and thick plates, indicating a deviation from cubic symmetry. The blue colouration of the halites, described by ultraviolet – visible spectroscopy, is due to the presence of colour centres. The colour centres have been recently identi- fied as: F, R 1 (F 3 ), R 2 (F 3 ), M and plasmons (Wese ł ucha- Birczy ń ska et al., Vib Spectrosc 60:124 – 128, 2012 ). The trace amount of impurities detected in the blue halites by means of scanning electron microscopy – energy dispersive X-ray spec- troscopy and micro-X-ray fluorescence techniques were con- nected mainly with solid inclusions such as K x Na (1 − x ) Cl, KMgCl 3 ·6H 2 O, KCl, orthorhombic sulphur, quartz and some other phases like pyrite. Crystallographic data obtained by X- ray diffraction experiments for the single crystals of the halite from K ł odawa with different saturation of blue or purple colours, as well as for natural colourless halite, revealed lowering of space-group symmetry to monoclinic, orthorhom- bic, trigonal, tetragonal or even triclinic systems while the space group typical for pure NaCl is Fm -3 m. pl
dc.description.volume 108 pl
dc.description.number 5 pl
dc.identifier.doi 10.1007/s00710-014-0323-9 pl
dc.identifier.eissn 1438-1168 pl
dc.title.journal Mineralogy and Petrology pl
dc.language.container eng pl
dc.date.accession 2019-02-14 pl
dc.affiliation Wydział Chemii : Zakład Krystalochemii i Krystalofizyki pl
dc.subtype Article pl
dc.rights.original CC-BY; inne; ostateczna wersja wydawcy; w momencie opublikowania; 0 pl
dc.identifier.project ROD UJ / P pl
.pointsMNiSW [2014 A]: 25


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Udzielam licencji. Uznanie autorstwa 4.0 Międzynarodowa Except where otherwise noted, this item's license is described as Udzielam licencji. Uznanie autorstwa 4.0 Międzynarodowa