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

Result code in 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>

Result on the web

<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>

Result language

angličtina

Original language name

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

Original language description

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

Czech name

—

Czech description

—

Type

J_imp - Article in a specialist periodical, which is included in the Web of Science database

CEP classification

—

OECD FORD branch

10504 - Mineralogy

Project

<a href="/en/project/GA19-05198S" target="_blank" >GA19-05198S: Greisenization and albitization - geological processes potentially concentrating some critical raw materials for modern technologies</a><br>

Continuities

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year

2019

Confidentiality

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

Name of the periodical

Lithos

ISSN

0024-4937

e-ISSN

—

Volume of the periodical

348-349

Issue of the periodical within the volume

December

Country of publishing house

NL - THE KINGDOM OF THE NETHERLANDS

Number of pages

13

Pages from-to

105206

UT code for WoS article

000500375700027

EID of the result in the Scopus database

2-s2.0-85073954379