1ST EVIDENCE OF BLUESCHIST-FACIES METAMOR PHISM IN THE CIRCUM-RHODOPENAPPES, INTERNAL HELLENIDES, GREECE

Citation
A. Michard et al., 1ST EVIDENCE OF BLUESCHIST-FACIES METAMOR PHISM IN THE CIRCUM-RHODOPENAPPES, INTERNAL HELLENIDES, GREECE, Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre, 318(11), 1994, pp. 1535-1542
Citations number
32
Categorie Soggetti
Multidisciplinary Sciences
ISSN journal
07644450
Volume
318
Issue
11
Year of publication
1994
Part
2
Pages
1535 - 1542
Database
ISI
SICI code
0764-4450(1994)318:11<1535:1EOBMP>2.0.ZU;2-V
Abstract
High-pressure, low-temperature assemblages are described for the first time in the Circum-Rhodope nappes east of the Vardar-Axios ophiolites . These assemblages occur in Permo-Triassic metavolcanics and metapeli tes, and include high-Si phengite and glaucophane. The estimated P-T c onditions range from 6-7 kbar at 300-degrees-C to 8-9 kbar at 400-degr ees-C. These nappes, together with the juxtaposed, eclogite-bearing Se rbo-Macedonian and Rhodopian nappes, and with the Paikon blueschist-fa cies rocks, could represent relics of an Eo-Hellenic (Late Jurassic) H P-LT belt.