БАРИЕВЫЙ БИОТИТ ИЗ ИЛЬМЕН

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dc.contributor.author Кориневский В.Г.
dc.contributor.author Кориневский Е.В.
dc.contributor.author Кориневская Г.Г.
dc.date.accessioned 2022-12-02T04:36:07Z
dc.date.available 2022-12-02T04:36:07Z
dc.date.issued 2005
dc.identifier https://www.elibrary.ru/item.asp?id=9136360
dc.identifier.citation Записки Российского минералогического общества, 2005, 134, 2, 75-83
dc.identifier.issn 0869-6055
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/40580
dc.description.abstract The reported find of barium biotites at the Aspen cape of the Bolshoy Ishkul lake is the first one at the Urals. These minerals occur in labrador and bytownite biotite-amphibole gabbro forming non-metamorphosed inclusi-ons in blocks of serpentinite melange among metamorphic rocks of Ilmenogorsky complex. There ate two varie-ties of barium biotites: first - with a moderate Ba content (BaO 1.37 wt%), and second - the Ba-rich one (BaO 8.52 wt%). Their crystal-chermical formulas, calculated on 7 cations, are, respectively: I - (K0,98 Ba0.04)1.02 (Mg1.40 Fe2+0.81 Fe3+0.37 Ti0.25 AlVI0.14 Mn0.03 V0.03)3.01 (Si2.74 AIVI1.26O10) (OH)1.37; II - (K0.73 Ba0.27)1.00(Mg1.63 Fe2+0.54 Fe3+0.43 AlVI0.19 Ti0.19 Mn0.02)3.00 (Si2.50 AlVI1.50O10) (OH1.72 C10.04)1.76- Previously, the barium biotites with similar com-positions have been described in Coldwell alkaline complex (Ontario, Canada). It is probable that those bioti-te-amphibole and fassaite gabbro, with such specific biotites, may represent the rocks from bottom levels of the earth's crust, which were lifted up to surface by the serpentinite protrusions.
dc.title БАРИЕВЫЙ БИОТИТ ИЗ ИЛЬМЕН
dc.type Статья
dc.subject.udc 549.0(234.853)


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