EVOLUTIONARY MODEL OF THE MELIATA BLUESCHISTS

The Meliata blueschists are subdivided into four groups which are characterized by different litholo-gies and metamorphic histories: (1) Marbles, intercalated with metabasalts and glaucophane-bearing phyllites. Phengite from this group metabasalts and phyllites records the Middle Jurassic age which...

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Main Author: Shah Wali Faryad
Format: Article
Language:English
Published: Technical University of Kosice 1997-10-01
Series:Acta Montanistica Slovaca
Online Access:http://actamont.tuke.sk/pdf/1997/n5/8faryad1.pdf
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author Shah Wali Faryad
author_facet Shah Wali Faryad
author_sort Shah Wali Faryad
collection DOAJ
description The Meliata blueschists are subdivided into four groups which are characterized by different litholo-gies and metamorphic histories: (1) Marbles, intercalated with metabasalts and glaucophane-bearing phyllites. Phengite from this group metabasalts and phyllites records the Middle Jurassic age which is interpreted to date the high-pressure metamorphism; (2) Metabasites and micaschists, devoid of marbles contain relic muscovite and newly formed high-Si phengite. The relic muscovite gives Palaeozoic age; (3) Quartz phyllites indicate a polyphase evolution characterized by greenschist facies metamorphism followed by blueschist-facies over-print; the high-Si micas provide evidence of an early Middle Jurassic age of the high-pressure metamorphism; (4) Amphibolite-facies slices and blocks, overprinted by blueschist-facies metamorphism, represent old base-ment rocks. Lithological and metamorphic characteristics together with radiogenic ages of high-pressure micas indicate a subduction of a continental wedge prior to that of oceanic crust can be assumed.
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spelling doaj.art-a35e851a07744ff5a9a86933f29357202022-12-22T02:47:21ZengTechnical University of KosiceActa Montanistica Slovaca1335-17881997-10-012special issue 12731EVOLUTIONARY MODEL OF THE MELIATA BLUESCHISTSShah Wali FaryadThe Meliata blueschists are subdivided into four groups which are characterized by different litholo-gies and metamorphic histories: (1) Marbles, intercalated with metabasalts and glaucophane-bearing phyllites. Phengite from this group metabasalts and phyllites records the Middle Jurassic age which is interpreted to date the high-pressure metamorphism; (2) Metabasites and micaschists, devoid of marbles contain relic muscovite and newly formed high-Si phengite. The relic muscovite gives Palaeozoic age; (3) Quartz phyllites indicate a polyphase evolution characterized by greenschist facies metamorphism followed by blueschist-facies over-print; the high-Si micas provide evidence of an early Middle Jurassic age of the high-pressure metamorphism; (4) Amphibolite-facies slices and blocks, overprinted by blueschist-facies metamorphism, represent old base-ment rocks. Lithological and metamorphic characteristics together with radiogenic ages of high-pressure micas indicate a subduction of a continental wedge prior to that of oceanic crust can be assumed.http://actamont.tuke.sk/pdf/1997/n5/8faryad1.pdf
spellingShingle Shah Wali Faryad
EVOLUTIONARY MODEL OF THE MELIATA BLUESCHISTS
Acta Montanistica Slovaca
title EVOLUTIONARY MODEL OF THE MELIATA BLUESCHISTS
title_full EVOLUTIONARY MODEL OF THE MELIATA BLUESCHISTS
title_fullStr EVOLUTIONARY MODEL OF THE MELIATA BLUESCHISTS
title_full_unstemmed EVOLUTIONARY MODEL OF THE MELIATA BLUESCHISTS
title_short EVOLUTIONARY MODEL OF THE MELIATA BLUESCHISTS
title_sort evolutionary model of the meliata blueschists
url http://actamont.tuke.sk/pdf/1997/n5/8faryad1.pdf
work_keys_str_mv AT shahwalifaryad evolutionarymodelofthemeliatablueschists