Hydrothermal replacement of garnet by tourmaline in elbaite
subtype LCT pegmatites

k 2015

Hydrothermal replacement of garnet by tourmaline in elbaite subtype LCT pegmatites

BUŘIVAL, Zbyněk a Milan NOVÁK

Základní údaje

Originální název

Hydrothermal replacement of garnet by tourmaline in elbaite subtype LCT pegmatites

Autoři

BUŘIVAL, Zbyněk (203 Česká republika, garant, domácí) a Milan NOVÁK (203 Česká republika, domácí)

Vydání

PEG 2015: 7th International Symposium on Granitic Pegmatites, 2015

Další údaje

Jazyk

angličtina

Typ výsledku

Prezentace na konferencích

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Polsko

Utajení

není předmětem státního či obchodního tajemství

Kód RIV

RIV/00216224:14310/15:00083335

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova česky

LCT pegmatit; elbaitový subtyp; subsolidus; alterace; zatlačování; granát; turmalín

Klíčová slova anglicky

LCT pegmatite; elbaite subtype; subsolidus; alteration; replacement; garnet; tourmaline

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 8. 7. 2015 15:23, Mgr. Zbyněk Buřival, Ph.D.

Anotace

V originále

Replacement mineral assemblages (tourmalines, micas) after primary garnet are indicator of composition of residual fluids. Mineral assemblages of tourmaline replacing garnet from elbaite-subtype pegmatites cutting marble and calc-silicate rock (Tsarafara Nord and Tamponilapa, Madagascar) and enclosed in gneiss and amphibolite (Ctidružice, Czech Republic) were examined. Primary mineral assemblages in all three pegmatites include spessartine-dominant garnet (Sps42-96) and black schorl to Mg-rich schorl, albite and quartz. Garnet replacement reactions were observed only in the vicinity of the Li-enriched albite unit. The replacement takes place mainly on the direct contact of garnet and albite. The total volume of this replacement process related to the whole pegmatite volume is negligible. Secondary assemblages replacing garnet and albite consist of mostly dark blue Fe-rich fluor-elbaite to very rare fluor-liddicoatite and quartz. Secondary tourmaline differs from primary ones in low to negligible contents of Mg, Ti, and mostly also Fe, and apparently elevated contents of Al, Mn, Li and F. However, behavior of Ca and Na is distinct in tourmalines from the individual localities. The schorl – fluor-elbaite – liddicoatite is present mainly at Tsarafara, whereas at Tamponilapa, most compositions represent schorl – elbaite – rossmanite solid solution, with rare schorl-uvite trend. Textural relations showing replacement of garnet and albite by tourmaline and quartz suggest the simplified reaction: 23 NaAlSi3O8 + 3 (Mn2Fe1)Al2Si3O12 + 12 H3BO3 + 3 LiF + HF = 4 (Na0.75)(Al1.25Fe0.75Li0.75Mn0.25)Al6 (Si6O18)(BO3)3(OH)3F + 44 SiO2 + 10 Na2SiO3 + 5 MnO + 12 H2O + OH-

Citovat

BUŘIVAL, Zbyněk a Milan NOVÁK. Hydrothermal replacement of garnet by tourmaline in elbaite subtype LCT pegmatites. In PEG 2015: 7th International Symposium on Granitic Pegmatites. 2015.

@proceedings{1305844,
   author = {Buřival, Zbyněk and Novák, Milan},
   booktitle = {PEG 2015: 7th International Symposium on Granitic Pegmatites},
   keywords = {LCT pegmatite; elbaite subtype; subsolidus; alteration; replacement; garnet; tourmaline},
   language = {eng},
   title = {Hydrothermal replacement of garnet by tourmaline in elbaite subtype LCT pegmatites},
   year = {2015}
}

TY  - CONF
ID  - 1305844
AU  - Buřival, Zbyněk - Novák, Milan
PY  - 2015
TI  - Hydrothermal replacement of garnet by tourmaline in elbaite subtype LCT pegmatites
KW  - LCT pegmatite
KW  - elbaite subtype
KW  - subsolidus
KW  - alteration
KW  - replacement
KW  - garnet
KW  - tourmaline
N2  - Replacement mineral assemblages (tourmalines, micas) after primary garnet are indicator of composition of residual fluids. Mineral assemblages of tourmaline replacing garnet from elbaite-subtype pegmatites cutting marble and calc-silicate rock (Tsarafara Nord and Tamponilapa, Madagascar) and enclosed in gneiss and amphibolite (Ctidružice, Czech Republic) were examined. Primary mineral assemblages in all three pegmatites include spessartine-dominant garnet (Sps42-96) and black schorl to Mg-rich schorl, albite and quartz. Garnet replacement reactions were observed only in the vicinity of the Li-enriched albite unit. The replacement takes place mainly on the direct contact of garnet and albite. The total volume of this replacement process related to the whole pegmatite volume is negligible. Secondary assemblages replacing garnet and albite consist of mostly dark blue Fe-rich fluor-elbaite to very rare fluor-liddicoatite and quartz. Secondary tourmaline differs from primary ones in low to negligible contents of Mg, Ti, and mostly also Fe, and apparently elevated contents of Al, Mn, Li and F. However, behavior of Ca and Na is distinct in tourmalines from the individual localities. The schorl – fluor-elbaite – liddicoatite is present mainly at Tsarafara, whereas at Tamponilapa, most compositions represent schorl – elbaite – rossmanite solid solution, with rare schorl-uvite trend. Textural relations showing replacement of garnet and albite by tourmaline and quartz suggest the simplified reaction: 23 NaAlSi3O8 + 3 (Mn2Fe1)Al2Si3O12 + 12 H3BO3 + 3 LiF + HF = 4 (Na0.75)(Al1.25Fe0.75Li0.75Mn0.25)Al6 (Si6O18)(BO3)3(OH)3F + 44 SiO2 + 10 Na2SiO3 + 5 MnO + 12 H2O + OH-
ER  -

BUŘIVAL, Zbyněk a Milan NOVÁK. Hydrothermal replacement of garnet by tourmaline in elbaite subtype LCT pegmatites. In \textit{PEG 2015: 7th International Symposium on Granitic Pegmatites}. 2015.

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