Kumdykolite from the ultrahigh-pressure granulite of the
Bohemian Massif

J 2014

Kumdykolite from the ultrahigh-pressure granulite of the Bohemian Massif

KOTKOVÁ, Jana; Radek ŠKODA a Vladimír MACHOVIČ

Základní údaje

Originální název

Kumdykolite from the ultrahigh-pressure granulite of the Bohemian Massif

Autoři

KOTKOVÁ, Jana (203 Česká republika, garant, domácí); Radek ŠKODA (203 Česká republika, domácí) a Vladimír MACHOVIČ (203 Česká republika)

Vydání

American Mineralogist, CHANTILLY, Mineralogical Society of America, 2014, 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: 1.964

Kód RIV

RIV/00216224:14310/14:00074428

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.2138/am.2014.4889

UT WoS

000340580500029

EID Scopus

2-s2.0-84907004543

Klíčová slova anglicky

High-temperature studies; kumdykolite; micro-Raman; micro-Raman mapping; BSE; WDX; high-temperature; ultrahigh-pressure; granulite; microdiamond

Štítky

AKR, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 9. 4. 2015 15:15, Ing. Andrea Mikešková

Anotace

V originále

We report the first occurrence of kumdykolite, a high-temperature analog of albite, in the European Variscan belt. It was discovered in an ultrahigh-pressure, diamond-bearing quartzofeldspathic granulite from the northern Bohemian Massif. It is associated with phlogopite and quartz in a multiphase solid inclusion within garnet, considered to represent a trapped fluid or melt phase. Micro-Raman analysis and mapping along with BSE revealed the presence of a sub-equant, elongated grain of kumdykolite reaching 20 mu m in length. WDX analysis has shown that kumdykolite contains 2 wt% CaO, probably indicating significant miscibility with the Ca-end-member svyatoslavite. Similar to the case of microdiamond inclusions, the kumdykolite-bearing multiphase inclusion is located in the Ca- and Mg-rich central part of the garnet and thus must have been trapped at P > 4 GPa. The inclusion minerals, however, crystallized upon decompression and cooling during the exhumation. Kumdykolite preservation thus provides independent evidence for high temperature of the original trapped fluid, or melt, crystallization, and rapid cooling of the rocks. Our results imply that kumdykolite and other feldspar modifications stable at elevated pressures and temperatures may be common phases in quartzofeldspathic granulites and need to be searched for.

Návaznosti

GA13-21450S, projekt VaV

Název: Severočeské granulity obsahující diamant a coesit: studium médií vzniku diamantu v hluboké subdukční zóně a důsledky pro geodynamické modely

Investor: Grantová agentura ČR, Severočeské granulity obsahující diamant a coesit: studium médií vzniku diamantu v hluboké subdukční zóně a důsledky pro geodynamické modely

Citovat

KOTKOVÁ, Jana; Radek ŠKODA a Vladimír MACHOVIČ. Kumdykolite from the ultrahigh-pressure granulite of the Bohemian Massif. American Mineralogist. CHANTILLY: Mineralogical Society of America, 2014, roč. 99, 8-9, s. 1798-1801. ISSN 0003-004X. Dostupné z: https://dx.doi.org/10.2138/am.2014.4889.

@article{1228840,
   author = {Kotková, Jana and Škoda, Radek and Machovič, Vladimír},
   article_location = {CHANTILLY},
   article_number = {8-9},
   doi = {http://dx.doi.org/10.2138/am.2014.4889},
   keywords = {High-temperature studies; kumdykolite; micro-Raman; micro-Raman mapping; BSE; WDX; high-temperature; ultrahigh-pressure; granulite; microdiamond},
   language = {eng},
   issn = {0003-004X},
   journal = {American Mineralogist},
   title = {Kumdykolite from the ultrahigh-pressure granulite of the Bohemian Massif},
   volume = {99},
   year = {2014}
}

TY  - JOUR
ID  - 1228840
AU  - Kotková, Jana - Škoda, Radek - Machovič, Vladimír
PY  - 2014
TI  - Kumdykolite from the ultrahigh-pressure granulite of the Bohemian Massif
JF  - American Mineralogist
VL  - 99
IS  - 8-9
SP  - 1798-1801
EP  - 1798-1801
PB  - Mineralogical Society of America
SN  - 0003004X
KW  - High-temperature studies
KW  - kumdykolite
KW  - micro-Raman
KW  - micro-Raman mapping
KW  - BSE
KW  - WDX
KW  - high-temperature
KW  - ultrahigh-pressure
KW  - granulite
KW  - microdiamond
N2  - We report the first occurrence of kumdykolite, a high-temperature analog of albite, in the European Variscan belt. It was discovered in an ultrahigh-pressure, diamond-bearing quartzofeldspathic granulite from the northern Bohemian Massif. It is associated with phlogopite and quartz in a multiphase solid inclusion within garnet, considered to represent a trapped fluid or melt phase. Micro-Raman analysis and mapping along with BSE revealed the presence of a sub-equant, elongated grain of kumdykolite reaching 20 mu m in length. WDX analysis has shown that kumdykolite contains 2 wt% CaO, probably indicating significant miscibility with the Ca-end-member svyatoslavite. Similar to the case of microdiamond inclusions, the kumdykolite-bearing multiphase inclusion is located in the Ca- and Mg-rich central part of the garnet and thus must have been trapped at P > 4 GPa. The inclusion minerals, however, crystallized upon decompression and cooling during the exhumation. Kumdykolite preservation thus provides independent evidence for high temperature of the original trapped fluid, or melt, crystallization, and rapid cooling of the rocks. Our results imply that kumdykolite and other feldspar modifications stable at elevated pressures and temperatures may be common phases in quartzofeldspathic granulites and need to be searched for.
ER  -

KOTKOVÁ, Jana; Radek ŠKODA a Vladimír MACHOVIČ. Kumdykolite from the ultrahigh-pressure granulite of the Bohemian Massif. \textit{American Mineralogist}. CHANTILLY: Mineralogical Society of America, 2014, roč.~99, 8-9, s.~1798-1801. ISSN~0003-004X. Dostupné z: https://dx.doi.org/10.2138/am.2014.4889.

Přehled o publikaci