Coincidence of gabbro and granulite formation and their implication for Variscan HT metamorphism in the Moldanubian Zone (Bohemian Massif), example from the Kutná Hora Complex
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- 作者：Shah Wali Faryada ; faryad@natur.cuni.cz" class="auth_mail" title="E-mail the corresponding author ; Vá ; clav Kachlí ; kb ; Jiří ; Slá ; mac ; Radim Jedlickaa
- 关键词：Spinel-bearing gabbro ; Variscan age ; Granulite ; Heat source
- 刊名：Lithos
- 出版年：2016
- 出版时间：1 November 2016
- 年：2016
- 卷：264
- 期：Complete
- 页码：56-69
- 全文大小：3770 K
文摘
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Coronitic gabbro and related ultramafic rocks occur with felsic granulite.
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The felsic granulite were subducted to mantle depths and then rapidly exhumed.
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The granulite facies overprint was coeval with gabbro crystallization.
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The mantle derived magma resulted heating of exhumed high-pressure rocks.