Formation of pretulite (ScPO4) by recrystallization of Sc-rich
precursors in Dolni Bory pegmatite: Evidence for different
mobility of Sc, Y, REE and Zr in hydrothermal conditions

J 2017

Formation of pretulite (ScPO4) by recrystallization of Sc-rich precursors in Dolni Bory pegmatite: Evidence for different mobility of Sc, Y, REE and Zr in hydrothermal conditions

VÝRAVSKÝ, Jakub, Milan NOVÁK a Radek ŠKODA

Základní údaje

Originální název

Formation of pretulite (ScPO4) by recrystallization of Sc-rich precursors in Dolni Bory pegmatite: Evidence for different mobility of Sc, Y, REE and Zr in hydrothermal conditions

Autoři

VÝRAVSKÝ, Jakub (203 Česká republika, garant, domácí), Milan NOVÁK (203 Česká republika, domácí) a Radek ŠKODA (203 Česká republika, domácí)

Vydání

Chemical Geology, Amsterdam, Elsevier Science BV, 2017, 0009-2541

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10504 Mineralogy

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 3.570

Kód RIV

RIV/00216224:14310/17:00096296

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1016/j.chemgeo.2016.11.031

UT WoS

000393001800003

Klíčová slova anglicky

Pretulite; Zircon; Scandium; Hydrothermal alteration; Mobilization of scandium; Granitic pegmatite

Štítky

NZ, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 4. 4. 2018 08:49, Ing. Nicole Zrilić

Anotace

V originále

Three distinct types (A, B and C) of secondary pretulite (ScPO4) were found in a single andalusite-diaspore nodule from the quartz core of the pegmatite dyke No. 3, Dolni Bory, Czech Republic. Primary crystallization of the nodule containing pretulite precursors - Sc, Y, U, P-rich zircon and Sc,W-rich ixiolite- proceeded at T <= 410 degrees C and P <= 2 kbar. Subsequent subsolidus hydrothermal alteration at T approximate to 350-300 degrees C transformed part of the andalusite to pyrophyllite, and triggered complete dissolution of Sc, Y, U, P-rich zircon I. In-situ reprecipitation produced Y, U-depleted zircon II with common inclusions of xenotime II and pretulite A (0.88-0.92 apfu Sc, 0.04-0.07 apfu Zr, <0.03 apfuY). During the same process recrystallization of Sc, W-rich ixiolite produced heterogeneous pretulite B (0.21-0.89 apfu Sc, 0.09-0.78 apfu Zr, <= 0.07 apfu Y). The origin of pretulite C (almost ideal ScPO4) closely associated with pyrophyllite replacing andalusite and distant from the potential Sc-precursors is explained by the separation of Sc from other HFSE present in the original precursors, which were immobile probably due to absence of suitable strong ligands in the fluids. Saturation of any Sc-dominant mineral (except thortveitite, Sc2Si2O7) is almost never achieved during primary magmatic crystallization due to the extremely high compatibility of Sc; consequently, the processes of hydrothermal alteration of Sc-enriched precursors and the selective mobilization and fractionation of Sc from other HFSE are important for the formation of scandium minerals. (C) 2016 Elsevier B.V. All rights reserved.

Návaznosti

MUNI/A/1316/2015, interní kód MU

Název: Geologické, geodynamické a environmentální procesy východního okraje Českého masívu (Akronym: Geodyn)

Investor: Masarykova univerzita, Geologické, geodynamické a environmentální procesy východního okraje Českého masívu, DO R. 2020_Kategorie A - Specifický výzkum - Studentské výzkumné projekty

Citovat

VÝRAVSKÝ, Jakub, Milan NOVÁK a Radek ŠKODA. Formation of pretulite (ScPO4) by recrystallization of Sc-rich precursors in Dolni Bory pegmatite: Evidence for different mobility of Sc, Y, REE and Zr in hydrothermal conditions. Chemical Geology. Amsterdam: Elsevier Science BV, 2017, roč. 449, January, s. 30-40. ISSN 0009-2541. Dostupné z: https://dx.doi.org/10.1016/j.chemgeo.2016.11.031.

@article{1375598,
   author = {Výravský, Jakub and Novák, Milan and Škoda, Radek},
   article_location = {Amsterdam},
   article_number = {January},
   doi = {http://dx.doi.org/10.1016/j.chemgeo.2016.11.031},
   keywords = {Pretulite; Zircon; Scandium; Hydrothermal alteration; Mobilization of scandium; Granitic pegmatite},
   language = {eng},
   issn = {0009-2541},
   journal = {Chemical Geology},
   title = {Formation of pretulite (ScPO4) by recrystallization of Sc-rich precursors in Dolni Bory pegmatite: Evidence for different mobility of Sc, Y, REE and Zr in hydrothermal conditions},
   volume = {449},
   year = {2017}
}

TY  - JOUR
ID  - 1375598
AU  - Výravský, Jakub - Novák, Milan - Škoda, Radek
PY  - 2017
TI  - Formation of pretulite (ScPO4) by recrystallization of Sc-rich precursors in Dolni Bory pegmatite: Evidence for different mobility of Sc, Y, REE and Zr in hydrothermal conditions
JF  - Chemical Geology
VL  - 449
IS  - January
SP  - 30-40
EP  - 30-40
PB  - Elsevier Science BV
SN  - 00092541
KW  - Pretulite
KW  - Zircon
KW  - Scandium
KW  - Hydrothermal alteration
KW  - Mobilization of scandium
KW  - Granitic pegmatite
N2  - Three distinct types (A, B and C) of secondary pretulite (ScPO4) were found in a single andalusite-diaspore nodule from the quartz core of the pegmatite dyke No. 3, Dolni Bory, Czech Republic. Primary crystallization of the nodule containing pretulite precursors - Sc, Y, U, P-rich zircon and Sc,W-rich ixiolite- proceeded at T <= 410 degrees C and P <= 2 kbar. Subsequent subsolidus hydrothermal alteration at T approximate to 350-300 degrees C transformed part of the andalusite to pyrophyllite, and triggered complete dissolution of Sc, Y, U, P-rich zircon I. In-situ reprecipitation produced Y, U-depleted zircon II with common inclusions of xenotime II and pretulite A (0.88-0.92 apfu Sc, 0.04-0.07 apfu Zr, <0.03 apfuY). During the same process recrystallization of Sc, W-rich ixiolite produced heterogeneous pretulite B (0.21-0.89 apfu Sc, 0.09-0.78 apfu Zr, <= 0.07 apfu Y). The origin of pretulite C (almost ideal ScPO4) closely associated with pyrophyllite replacing andalusite and distant from the potential Sc-precursors is explained by the separation of Sc from other HFSE present in the original precursors, which were immobile probably due to absence of suitable strong ligands in the fluids. Saturation of any Sc-dominant mineral (except thortveitite, Sc2Si2O7) is almost never achieved during primary magmatic crystallization due to the extremely high compatibility of Sc; consequently, the processes of hydrothermal alteration of Sc-enriched precursors and the selective mobilization and fractionation of Sc from other HFSE are important for the formation of scandium minerals. (C) 2016 Elsevier B.V. All rights reserved.
ER  -

VÝRAVSKÝ, Jakub, Milan NOVÁK a Radek ŠKODA. Formation of pretulite (ScPO4) by recrystallization of Sc-rich precursors in Dolni Bory pegmatite: Evidence for different mobility of Sc, Y, REE and Zr in hydrothermal conditions. \textit{Chemical Geology}. Amsterdam: Elsevier Science BV, 2017, roč.~449, January, s.~30-40. ISSN~0009-2541. Dostupné z: https://dx.doi.org/10.1016/j.chemgeo.2016.11.031.

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