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Several minerals from zeolite group have been found in Rębiszów basaltoid deposits: gobbinsite, natrolite, gismondine, garronite, thomsonite and phillipsite. For the first time gobbinsite has been recognized in basaltoids from Lower Silesia. Moreover, a new phase has been distinguished on the basis of some determined parameters (such as calculation of chemical formulae and X-ray diffraction patterns), belonging to zeolite group and occurring together with other zeolites. Origin of the whole assemblage of zeolite minerals can be related to hydrothermal activity of post-magmatic solutions within thermal contraction cracks of congealing basaltoid lava.
Czasopismo
Rocznik
Tom
Strony
23--32
Opis fizyczny
Bibliogr. 15 poz., rys., tab., wykr.
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autor
- Institute of Applied Geology, Silesian University of Technology, ul. Akademicka 2, 44-100 Gliwice, Poland, zadamczy@zeus.polsl.gliwice.pl
Bibliografia
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BPZ2-0018-0053