The metamorphic evolution from ultrahigh-temperature to amphibolite facies metamorphism in the Odaesan area after the collision between the North and South China Cratons in the Korean Peninsula
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- 作者：Byung Choon Leea ; Chang Whan Oha ; ocwhan@jbnu.ac.kr" class="auth_mail" title="E-mail the corresponding author ; Tae Sung Kima ; b ; Keewook Yic
- 关键词：Gyeonggi Massif ; Hongseong&ndash ; Odaesan belt ; Dabie&ndash ; Sulu collision belt ; Ultrahigh-temperature metamorphism ; SHRIMP U&ndash ; Pb dating
- 刊名：Lithos
- 出版年：2016
- 出版时间：July 2016
- 年：2016
- 卷：256-257
- 期：Complete
- 页码：109-131
- 全文大小：5576 K
文摘
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Study area underwent regional ultra-high-temperature metamorphism at 247–245 Ma.
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UHT metamorphism occurred in the post-collision tectonic setting.
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UHT metamorphism was followed by upper amphibolite facies migmatization at 227 Ma.