Chemistry of quartz - A new insight into the origin of the Orlovka Ta-Li deposit, Eastern Transbaikalia, Russia

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F19%3A00511042" target="_blank" >RIV/67985831:_____/19:00511042 - isvavai.cz</a>

Výsledek na webu

<a href="https://www.sciencedirect.com/science/article/pii/S0024493719303652?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0024493719303652?via%3Dihub</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.lithos.2019.105206" target="_blank" >10.1016/j.lithos.2019.105206</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Chemistry of quartz - A new insight into the origin of the Orlovka Ta-Li deposit, Eastern Transbaikalia, Russia

Popis výsledku v původním jazyce

The Ta-Li deposit of Orlovka in Eastern Transbaikalia, Russia, is one of the best known rare-metal deposits in cupola-shaped plutons of Li, F-rich rare-metal granites. Quartz from all granite varieties from the deposit was studied using automated mineralogy (TIMA), cathodoluminescence (CL), and laser-ablation inductively-coupled mass spectrometry (LA-ICP MS) in order to find new constraints on the origin of the deposit. Subhedral to euhedral quartz crystals, strongly zoned in CL, relatively enriched in Ti and Li (up to 95 and 33 ppm respectively), and free of mineral inclusions were found in all varieties of biotite granites forming the deeper part of the pluton. Crystals of “snow-ball” quartz with zonally arranged inclusions of albite, with low intensity of CL, and slightly enriched in Al and Ge (up to 350 and 4.8 ppm, respectively) are common in all types of Li-mica granites forming the cupola-shaped upper part of the pluton. The distinction between the two principal types of quartz is generally consistent with the already proposed model of two comagmatic intrusions: deeper-seated biotite granites underwent a complicated magmatic evolution with repeated episodes of crystallization and resorption of quartz, only a limited degree of fractionation, and a small e if any e reaction with fluid. Li-mica granites, taking position within the cupola, strongly fractionated upwards. The upward transfer of Li and rare metals was, moreover, supported by fluid unmixed in the middle level of the cupola.n

Název v anglickém jazyce

Chemistry of quartz - A new insight into the origin of the Orlovka Ta-Li deposit, Eastern Transbaikalia, Russia

Popis výsledku anglicky

The Ta-Li deposit of Orlovka in Eastern Transbaikalia, Russia, is one of the best known rare-metal deposits in cupola-shaped plutons of Li, F-rich rare-metal granites. Quartz from all granite varieties from the deposit was studied using automated mineralogy (TIMA), cathodoluminescence (CL), and laser-ablation inductively-coupled mass spectrometry (LA-ICP MS) in order to find new constraints on the origin of the deposit. Subhedral to euhedral quartz crystals, strongly zoned in CL, relatively enriched in Ti and Li (up to 95 and 33 ppm respectively), and free of mineral inclusions were found in all varieties of biotite granites forming the deeper part of the pluton. Crystals of “snow-ball” quartz with zonally arranged inclusions of albite, with low intensity of CL, and slightly enriched in Al and Ge (up to 350 and 4.8 ppm, respectively) are common in all types of Li-mica granites forming the cupola-shaped upper part of the pluton. The distinction between the two principal types of quartz is generally consistent with the already proposed model of two comagmatic intrusions: deeper-seated biotite granites underwent a complicated magmatic evolution with repeated episodes of crystallization and resorption of quartz, only a limited degree of fractionation, and a small e if any e reaction with fluid. Li-mica granites, taking position within the cupola, strongly fractionated upwards. The upward transfer of Li and rare metals was, moreover, supported by fluid unmixed in the middle level of the cupola.n

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10504 - Mineralogy

Projekt

<a href="/cs/project/GA19-05198S" target="_blank" >GA19-05198S: Greisenizace a albitizace - geologické procesy s potenciálem koncentrovat některé kritické suroviny pro moderní technologie</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2019

Kód důvěrnosti údajů

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

Název periodika

Lithos

ISSN

0024-4937

e-ISSN

—

Svazek periodika

348-349

Číslo periodika v rámci svazku

December

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

13

Strana od-do

105206

Kód UT WoS článku

000500375700027

EID výsledku v databázi Scopus

2-s2.0-85073954379