Accessory priderite and burbankite in multiphase solid inclusions in the orogenic garnet peridotite from the Bohemian Massif, Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F15%3A00442927" target="_blank" >RIV/67985831:_____/15:00442927 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.2465/jmps.140613c" target="_blank" >http://dx.doi.org/10.2465/jmps.140613c</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.2465/jmps.140613c" target="_blank" >10.2465/jmps.140613c</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Accessory priderite and burbankite in multiphase solid inclusions in the orogenic garnet peridotite from the Bohemian Massif, Czech Republic

Popis výsledku v původním jazyce

This paper reports on priderite (potassium titanate) and burbankite (alkali Sr Ca REE Ba carbonate) from an orogenic garnet peridotite body enclosed in high pressure garnet-kyanite-bearing quartzo-feldspathic Gföhl granulite in the Bohemian Massif of theVariscan belt. The garnet peridotite contains ubiquitous phlogopite and was interpreted to be derived from the mantle wedge formed at the convergent plate margin. The earliest generation of chromian spinel, surrounded by kelyphitized garnet, ubiquitously contains multiphase solid in-clusions (MSIs), which are mainly composed of phlogopite, dolomite, calcite, apatite, graphite, monazite, thorianite, and sulfides, and priderite and burbankite are newly identified as rare accessory minerals in such MSIs.Most of these MSIs contained significant amounts of carbonates. The presence of peculiar accessory minerals in MSIs characterizes the nature of parental melts. The formation of priderite requires an ultrapotassic condition, which is usual

Název v anglickém jazyce

Accessory priderite and burbankite in multiphase solid inclusions in the orogenic garnet peridotite from the Bohemian Massif, Czech Republic

Popis výsledku anglicky

This paper reports on priderite (potassium titanate) and burbankite (alkali Sr Ca REE Ba carbonate) from an orogenic garnet peridotite body enclosed in high pressure garnet-kyanite-bearing quartzo-feldspathic Gföhl granulite in the Bohemian Massif of theVariscan belt. The garnet peridotite contains ubiquitous phlogopite and was interpreted to be derived from the mantle wedge formed at the convergent plate margin. The earliest generation of chromian spinel, surrounded by kelyphitized garnet, ubiquitously contains multiphase solid in-clusions (MSIs), which are mainly composed of phlogopite, dolomite, calcite, apatite, graphite, monazite, thorianite, and sulfides, and priderite and burbankite are newly identified as rare accessory minerals in such MSIs.Most of these MSIs contained significant amounts of carbonates. The presence of peculiar accessory minerals in MSIs characterizes the nature of parental melts. The formation of priderite requires an ultrapotassic condition, which is usual

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

—

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Journal of Mineralogical and Petrological Sciences

ISSN

1345-6296

e-ISSN

—

Svazek periodika

110

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

JP - Japonsko

Počet stran výsledku

9

Strana od-do

20-28

Kód UT WoS článku

000352426700003

EID výsledku v databázi Scopus

2-s2.0-84946184318