Late Paleoproterozoic ultrahigh-temperature metamorphism in the Korean Peninsula

Late Paleoproterozoic ultrahigh-temperature metamorphism in the Korean Peninsula Precambrian Research 308 (2018) 111–125 Contents lists available at ScienceDirect Precambrian Research journal homepage: www.elsevier.com/locate/precamres Late Paleoproterozoic ultrahigh-temperature metamorphism in the Korean Peninsula a,b,c, a d a d M. Santosh , Chao-Nan Hu , Sung Won Kim , Li Tang , Weon-Seo Kee School of Earth Sciences and Resources, China University of Geosciences Beijing, 29 Xueyuan Road, Beijing 100083, China Centre for Tectonics, Resources and Exploration, Department of Earth Sciences, University of Adelaide, SA 5005, Australia Key Lab of Submarine Geosciences and Prospecting Techniques, MOE AND College of Marine Geosciences, Ocean University of China, Qingdao 266100, China Geological Research Division, Korea Institute of Geoscience and Mineral Resources, Daejeon 305-350, Republic of Korea ARTICLE I NFO ABSTRACT Keywords: The Paleoproterozoic rock record from the Sino-Korean Peninsula was fundamental to the models on evolution Ultrahigh temperature metamorphism: of the Asian continental collage and its relationship with the amalgamation and disruption of Proterozoic su- Petrology and P-T pseudosections percontinents such as Columbia and Rodinia. In this study, we present results from a comprehensive in- Zircon U – Pb geochronology vestigation on the khondalites in the Hongseong area, along the western part of the Gyeonggi massif within the Khondalite central Korean Peninsula involving http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Precambrian Research Elsevier

Late Paleoproterozoic ultrahigh-temperature metamorphism in the Korean Peninsula

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Publisher
Elsevier
Copyright
Copyright © 2018 Elsevier B.V.
ISSN
0301-9268
eISSN
1872-7433
D.O.I.
10.1016/j.precamres.2018.02.010
Publisher site
See Article on Publisher Site

Abstract

Precambrian Research 308 (2018) 111–125 Contents lists available at ScienceDirect Precambrian Research journal homepage: www.elsevier.com/locate/precamres Late Paleoproterozoic ultrahigh-temperature metamorphism in the Korean Peninsula a,b,c, a d a d M. Santosh , Chao-Nan Hu , Sung Won Kim , Li Tang , Weon-Seo Kee School of Earth Sciences and Resources, China University of Geosciences Beijing, 29 Xueyuan Road, Beijing 100083, China Centre for Tectonics, Resources and Exploration, Department of Earth Sciences, University of Adelaide, SA 5005, Australia Key Lab of Submarine Geosciences and Prospecting Techniques, MOE AND College of Marine Geosciences, Ocean University of China, Qingdao 266100, China Geological Research Division, Korea Institute of Geoscience and Mineral Resources, Daejeon 305-350, Republic of Korea ARTICLE I NFO ABSTRACT Keywords: The Paleoproterozoic rock record from the Sino-Korean Peninsula was fundamental to the models on evolution Ultrahigh temperature metamorphism: of the Asian continental collage and its relationship with the amalgamation and disruption of Proterozoic su- Petrology and P-T pseudosections percontinents such as Columbia and Rodinia. In this study, we present results from a comprehensive in- Zircon U – Pb geochronology vestigation on the khondalites in the Hongseong area, along the western part of the Gyeonggi massif within the Khondalite central Korean Peninsula involving

Journal

Precambrian ResearchElsevier

Published: May 1, 2018

References

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