Arid
DOI10.1127/ejm/2015/0027-2420
Mayenite supergroup, part III: Fluormayenite, Ca12Al14O32 [square F-4(2)], and fluorkyuygenite, Ca12Al14O32[(H2O)(4)F-2], two new minerals from pyrometamorphic rocks of the Hatrurim Complex, South Levant
Galuskin, Evgeny V.1; Gfeller, Frank2; Armbruster, Thomas2; Galuskina, Irina O.1; Vapnik, Yevgeny3; Dulski, Mateusz4,5; Murashko, Mikhail6; Dzierzanowski, Piotr7; Sharygin, Viktor V.8,9; Krivovichev, Sergey V.10; Wirth, Richard11
通讯作者Galuskin, Evgeny V.
来源期刊EUROPEAN JOURNAL OF MINERALOGY
ISSN0935-1221
EISSN1617-4011
出版年2015
卷号27期号:1页码:123-136
英文摘要

Two new mineral species of the mayenite group, fluormayenite Ca12Al14O32[square F-4(2)] (I (4) over bar 3d, a = 11.9894(2) angstrom, v = 1723.42(5) angstrom(3), Z =-- 2) and fluorkyuygenite Ca12Al14O32[(H2O)(4)F-2] (I (4) over bar 3d, a = 11.966(2) angstrom, V = 1713.4(1) angstrom(3), Z = 2), are major constituents of larnite pyrometamorphic rocks of the Hatrurim Complex (Mottled Zone) distributed along the Dead Sea rift on the territory of Israel, Palestinian Autonomy and Jordan. Holotype specimens of fluormayenite and fluorkyuygenite were collected at the Jabel Harmun, Judean Mts., Palestinian Autonomy and in the Hatrurim Basin, Negev Desert, Israel, respectively. Mineral associations of holotype fluormayenite and fluorkyuygenite are similar and include larnite, shulamitite, Cr-containing spinel-magnesioferrite series, ye’ elimite, fluorapatite-fluorellestadite, periclase, brownmillerite, oldhamite as well as the retrograde phases portlandite, hematite, hillebrandite, afwillite, foshagite, ettringite, katoite and hydrocalurnite. Fluormayenite and fluorkyuygenite crystals, usually < 20 mu m in size, are colourless, in places with greenish or yellowish tint, the streak is white. Both minerals are transparent with a vitreous lustre; they do not show fluorescence. Fluormayenite and fluorkyuygenite are isotropic and have similar refractive indices: n = 1.612(3) and n = 1.610(3) (589 nm), respectively. The hardness of fluormayenite and fluorkyuygenite is H (Mohs) 51/2-6; VIM load 50 g, 771(38) kg mm(-2); and 5-51/2; VHN load 50 g, 712(83) kg m(-2), respectively. Both minerals have the microporous tetrahedral framework structure characteristic of the mayenite supergroup. In fluormayenite 1/3 of the structural cages are occupied by fluorine. In fluorkyuygenite, in addition to fluorine and negligible amounts of OH, H2O molecules occupy about 2/3 of the cages. The holotype fluormayenite from Jabel Harmun has the crystal chemical formula (Ca11.951Na0.037)(Sigma 11.987)(Al-13.675 Fe0.2703+Mg0.040Si0.009P0.005S0.0136+)(Sigma 14.013) O-31.503(OH)(1.492){square 4.581F1.375Cl0.044](Sigma 6), fluorkyuygenite from the Hatrurim Basin has the composition Ca-12.034(Al13.344Fe0.3983+ Si-0224)Sigma O-13.966(32)[(H2O)(3.810)F-1.894 (OH)(0.296)](Sigma 6). Raman spectra of fluormayenite and fluorkyuygenite in the spectral region 200-1000 cm(-1) are similar and are characterized by the four strong main bands at about 320 (nu(2) AlO4), 520 (nu(4) AlO4), 700, 770 (nu(1) AlO4) cm(-1). In the O-H vibration region fluorkyuygenite shows a


英文关键词fluorkyuygenite fluormayenite new mineral mayenite supergroup crystal structure Raman pyrometamorphic rocks Hatrurim Complex Israel
类型Article
语种英语
国家Poland ; Switzerland ; Israel ; Russia ; Germany
收录类别SCI-E
WOS记录号WOS:000350837400011
WOS关键词PALESTINIAN AUTONOMY ; MOTTLED ZONE ; JABEL HARMUN ; VOLCANO ; SYSTEM
WOS类目Mineralogy
WOS研究方向Mineralogy
来源机构Ben-Gurion University of the Negev
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/187212
作者单位1.Univ Silesia, Fac Earth Sci, Dept Geochem Mineral & Petrog, PL-41200 Sosnowiec, Poland;
2.Univ Bern, Inst Geol Sci, Mineral Crystallog, CH-3012 Bern, Switzerland;
3.Ben Gurion Univ Negev, Dept Geol & Environm Sci, IL-84105 Beer Sheva, Israel;
4.Univ Silesia, Inst Phys, PL-40007 Katowice, Poland;
5.Poland & Silesian Ctr Educ & Interdisciplinary Re, PL-41500 Chorzow, Poland;
6.Systemat Mineral, St Petersburg 199178, Russia;
7.Warsaw Univ, Inst Geochem Mineral & Petrol, PL-02089 Warsaw, Poland;
8.RAS, Siberian Branch, VS Sobolev Inst Geol & Mineral, Novosibirsk 630090, Russia;
9.Novosibirsk State Univ, Russia & Dept Geol & Geophys, Novosibirsk 630090, Russia;
10.St Petersburg State Univ, Geol Fac, Dept Crystallog, St Petersburg 199034, Russia;
11.GFZ German Res Ctr Geosci, Helmholtz Ctr Potsdam, D-14473 Potsdam, Germany
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Galuskin, Evgeny V.,Gfeller, Frank,Armbruster, Thomas,et al. Mayenite supergroup, part III: Fluormayenite, Ca12Al14O32 [square F-4(2)], and fluorkyuygenite, Ca12Al14O32[(H2O)(4)F-2], two new minerals from pyrometamorphic rocks of the Hatrurim Complex, South Levant[J]. Ben-Gurion University of the Negev,2015,27(1):123-136.
APA Galuskin, Evgeny V..,Gfeller, Frank.,Armbruster, Thomas.,Galuskina, Irina O..,Vapnik, Yevgeny.,...&Wirth, Richard.(2015).Mayenite supergroup, part III: Fluormayenite, Ca12Al14O32 [square F-4(2)], and fluorkyuygenite, Ca12Al14O32[(H2O)(4)F-2], two new minerals from pyrometamorphic rocks of the Hatrurim Complex, South Levant.EUROPEAN JOURNAL OF MINERALOGY,27(1),123-136.
MLA Galuskin, Evgeny V.,et al."Mayenite supergroup, part III: Fluormayenite, Ca12Al14O32 [square F-4(2)], and fluorkyuygenite, Ca12Al14O32[(H2O)(4)F-2], two new minerals from pyrometamorphic rocks of the Hatrurim Complex, South Levant".EUROPEAN JOURNAL OF MINERALOGY 27.1(2015):123-136.
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