Vranaite, ideally Al16S4Si4O38, a new mineral related to
boralsilite, Al16B6Si2O37, from the Manjaka pegmatite, Sahatany
Valley, Madagascar

J 2016

Vranaite, ideally Al16S4Si4O38, a new mineral related to boralsilite, Al16B6Si2O37, from the Manjaka pegmatite, Sahatany Valley, Madagascar

CEMPÍREK, Jan, E.S. GREW, A.R. KAMPF, C. MA, Milan NOVÁK et. al.

Základní údaje

Originální název

Vranaite, ideally Al16S4Si4O38, a new mineral related to boralsilite, Al16B6Si2O37, from the Manjaka pegmatite, Sahatany Valley, Madagascar

Autoři

CEMPÍREK, Jan (203 Česká republika, garant, domácí), E.S. GREW (840 Spojené státy), A.R. KAMPF (840 Spojené státy), C. MA (840 Spojené státy), Milan NOVÁK (203 Česká republika, domácí), Petr GADAS (203 Česká republika, domácí), Radek ŠKODA (203 Česká republika, domácí), Michaela VAŠINOVÁ GALIOVÁ (203 Česká republika, domácí), F. PEZZOTTA (380 Itálie), L.A. GROAT (124 Kanada) a S.V. KRIVOVICHEV (643 Rusko)

Vydání

American Mineralogist, CHANTILLY, Mineralogical Society of America, 2016, 0003-004X

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Spojené státy

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 2.021

Kód RIV

RIV/00216224:14310/16:00088762

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.2138/am-2016-5686

UT WoS

000385605100018

Klíčová slova anglicky

Vranaite; boralsilite; Madagascar; pegmatite; new mineral; structural complexity; Ostwald step rule; borosilicate minerals

Štítky

AKR, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 16. 4. 2017 23:27, Ing. Andrea Mikešková

Anotace

V originále

The system B2O3-Al2O3-SiO2 (BAS) includes two ternary phases occurring naturally, boromullite, Al9BSi2O19, and boralsilite, Al46B6Si2O37, as well as synthetic compounds structurally related to mullite. The new mineral vranaite, a third naturally occurring anhydrous ternary BAS phase, is found with albite and K-feldspar as a breakdown product of spodumene in the elbaite-subtype Manjaka granitic pegmatite, Sahatany Valley, Madagascar. Boralsilite also occurs in this association, although separately from vrnnaite; both minerals form rare aggregates of subparallel prisms up to 100 p.m long. Vranaite is monoclinic, space group 121m, a= 10.3832(12), b= 5.6682(7), c= 10.8228(12) angstrom, beta = 90.106(11)degrees; V= 636.97(13) angstrom(3), Z= 1. In the structure [R-1, = 0.0416 for 550 F-o> 4 sigma F-o], chains of A106 octahedra run parallel to [010] and are cross-linked by Si207 disilicate groups, B03 triangles, and clusters of A104 and two A105 polyhedra. If all sites were filled (Al4 and Al5 to 50%), the formula becomes Al16B4Si4O38, close to Li1.08Be0.47Fe0.02Al14 65B3.89Si3.88O36.62 calculated from the analyses assuming cations sum to 24. The compatibility index based on the Gladstone-Dale relationship is 0.001 ("superior"). Assemblages with vranaite and boralsilite are inferred to represent initial reaction products of a residual liquid rich in Li, Be, Na, K, and B during a pressure and chemical quench, but at low H2O activities due to early melt contamination by carbonate in the host rocks. The two BAS phases are interpreted to have crystallized metastably in lieu of dumortierite in accordance with Ostwald Step Rule, possibly first as "boron mullite," then as monoclinic phases. The presence of such metastable phases is suggestive that pegmatites crystallize, at least partially, by disequilibrium processes, with significant undercooling, and at high viscosities, which limit diffusion rates.

Návaznosti

GA14-13347S, projekt VaV

Název: Variabilita lehkých prvků (Li, Be, B) ve vybraných horninotvorných a akcesorických minerálech z felsických magmatických a metamorfovaných hornin

Investor: Grantová agentura ČR, Variabilita lehkých prvků (Li, Be, B) ve vybraných horninotvorných a akcesorických minerálech z felsických magmatických a metamorfovaných hornin

Citovat

CEMPÍREK, Jan, E.S. GREW, A.R. KAMPF, C. MA, Milan NOVÁK, Petr GADAS, Radek ŠKODA, Michaela VAŠINOVÁ GALIOVÁ, F. PEZZOTTA, L.A. GROAT a S.V. KRIVOVICHEV. Vranaite, ideally Al16S4Si4O38, a new mineral related to boralsilite, Al16B6Si2O37, from the Manjaka pegmatite, Sahatany Valley, Madagascar. American Mineralogist. CHANTILLY: Mineralogical Society of America, 2016, roč. 101, 9-10, s. 2108-2117. ISSN 0003-004X. Dostupné z: https://dx.doi.org/10.2138/am-2016-5686.

@article{1375107,
   author = {Cempírek, Jan and Grew, E.S. and Kampf, A.R. and Ma, C. and Novák, Milan and Gadas, Petr and Škoda, Radek and Vašinová Galiová, Michaela and Pezzotta, F. and Groat, L.A. and Krivovichev, S.V.},
   article_location = {CHANTILLY},
   article_number = {9-10},
   doi = {http://dx.doi.org/10.2138/am-2016-5686},
   keywords = {Vranaite; boralsilite; Madagascar; pegmatite; new mineral; structural complexity; Ostwald step rule; borosilicate minerals},
   language = {eng},
   issn = {0003-004X},
   journal = {American Mineralogist},
   title = {Vranaite, ideally Al16S4Si4O38, a new mineral related to boralsilite, Al16B6Si2O37, from the Manjaka pegmatite, Sahatany Valley, Madagascar},
   volume = {101},
   year = {2016}
}

TY  - JOUR
ID  - 1375107
AU  - Cempírek, Jan - Grew, E.S. - Kampf, A.R. - Ma, C. - Novák, Milan - Gadas, Petr - Škoda, Radek - Vašinová Galiová, Michaela - Pezzotta, F. - Groat, L.A. - Krivovichev, S.V.
PY  - 2016
TI  - Vranaite, ideally Al16S4Si4O38, a new mineral related to boralsilite, Al16B6Si2O37, from the Manjaka pegmatite, Sahatany Valley, Madagascar
JF  - American Mineralogist
VL  - 101
IS  - 9-10
SP  - 2108-2117
EP  - 2108-2117
PB  - Mineralogical Society of America
SN  - 0003004X
KW  - Vranaite
KW  - boralsilite
KW  - Madagascar
KW  - pegmatite
KW  - new mineral
KW  - structural complexity
KW  - Ostwald step rule
KW  - borosilicate minerals
N2  - The system B2O3-Al2O3-SiO2 (BAS) includes two ternary phases occurring naturally, boromullite, Al9BSi2O19, and boralsilite, Al46B6Si2O37, as well as synthetic compounds structurally related to mullite. The new mineral vranaite, a third naturally occurring anhydrous ternary BAS phase, is found with albite and K-feldspar as a breakdown product of spodumene in the elbaite-subtype Manjaka granitic pegmatite, Sahatany Valley, Madagascar. Boralsilite also occurs in this association, although separately from vrnnaite; both minerals form rare aggregates of subparallel prisms up to 100 p.m long. Vranaite is monoclinic, space group 121m, a= 10.3832(12), b= 5.6682(7), c= 10.8228(12) angstrom, beta = 90.106(11)degrees; V= 636.97(13) angstrom(3), Z= 1. In the structure [R-1, = 0.0416 for 550 F-o> 4 sigma F-o], chains of A106 octahedra run parallel to [010] and are cross-linked by Si207 disilicate groups, B03 triangles, and clusters of A104 and two A105 polyhedra. If all sites were filled (Al4 and Al5 to 50%), the formula becomes Al16B4Si4O38, close to Li1.08Be0.47Fe0.02Al14 65B3.89Si3.88O36.62 calculated from the analyses assuming cations sum to 24. The compatibility index based on the Gladstone-Dale relationship is 0.001 ("superior"). Assemblages with vranaite and boralsilite are inferred to represent initial reaction products of a residual liquid rich in Li, Be, Na, K, and B during a pressure and chemical quench, but at low H2O activities due to early melt contamination by carbonate in the host rocks. The two BAS phases are interpreted to have crystallized metastably in lieu of dumortierite in accordance with Ostwald Step Rule, possibly first as "boron mullite," then as monoclinic phases. The presence of such metastable phases is suggestive that pegmatites crystallize, at least partially, by disequilibrium processes, with significant undercooling, and at high viscosities, which limit diffusion rates.
ER  -

CEMPÍREK, Jan, E.S. GREW, A.R. KAMPF, C. MA, Milan NOVÁK, Petr GADAS, Radek ŠKODA, Michaela VAŠINOVÁ GALIOVÁ, F. PEZZOTTA, L.A. GROAT a S.V. KRIVOVICHEV. Vranaite, ideally Al16S4Si4O38, a new mineral related to boralsilite, Al16B6Si2O37, from the Manjaka pegmatite, Sahatany Valley, Madagascar. \textit{American Mineralogist}. CHANTILLY: Mineralogical Society of America, 2016, roč.~101, 9-10, s.~2108-2117. ISSN~0003-004X. Dostupné z: https://dx.doi.org/10.2138/am-2016-5686.

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