J 2020

Variscan high-pressure metamorphism of kyanite-bearing paragneisses hosting eclogites in the Veporic unit, Western Carpathians: Evidence from Th-U-Pb dating of monazite

PETRIK, I., M. JANAK, Tomáš VACULOVIČ, P. KONECNY, S. MERES et. al.

Basic information

Original name

Variscan high-pressure metamorphism of kyanite-bearing paragneisses hosting eclogites in the Veporic unit, Western Carpathians: Evidence from Th-U-Pb dating of monazite

Authors

PETRIK, I., M. JANAK, Tomáš VACULOVIČ (203 Czech Republic, guarantor, belonging to the institution), P. KONECNY and S. MERES

Edition

Geologica Carpathica, BRATISLAVA, SLOVAK ACAD SCIENCES GEOLOGICAL INST, 2020, 1335-0552

Other information

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

10505 Geology

Country of publisher

Slovakia

Confidentiality degree

není předmětem státního či obchodního tajemství

References:

Impact factor

Impact factor: 1.875

RIV identification code

RIV/00216224:14740/20:00118369

Organization unit

Central European Institute of Technology

DOI

UT WoS

000607216600001

Keywords in English

monazite; Th-U-Pb dating; high-pressure metamorphism; Variscan orogeny; Veporic unit; Western Carpathians

Tags

Tags

International impact, Reviewed
Změněno: 11/3/2021 09:18, Mgr. Pavla Foltynová, Ph.D.

Abstract

V originále

In view of a polyphase development of the northern Veporic pre-Alpine basement of the Western Carpathians it is important to determine the age of high pressure (HP) metamorphism known from eclogites occurring in this area. To do this, several monazite-bearing paragneisses were studied petrologically and monazite was dated by chemical (U-Th-Pb) method. Identified were remnants from high-pressure stage, i.e. phengite (Si apfu =3.2-3.3), kyanite, rutile and Ca-rich garnet rims. Part of the present mineral assemblage may have been preserved from prograde stage (plagioclase) and part reflects re-equilibration during retrogression (biotite, major elements in garnet cores). However, Y and HREE in garnet cores were not homogenised and their profiles indicate origin during temperature rise. Peak metamorphic conditions (P =21 kbar; T =650 degrees C), and retrogression stage (P = 9 kbar; T =520 degrees C) were calculated using Zr-in-rutile, and Y-in-garnet and monazite thermometry, phengite composition and pseudosection modelling. Monazite yielded dominant Early Carboniferous age (354 Ma) with subordinate amounts of Ordovician (485 Ma) and Cambrian (505 Ma) ones, and no Alpine record. The monazite position in garnet cores predating the growth of Ca rims suggest that the Carboniferous age of 354 Ma probably predates the peak conditions and refers to the prograde stage of the Variscan metamorphic evolution.