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首页> 外文期刊>Gondwana research: international geoscience journal >Paleozoic tectonics of the southwestern Gyeonggi massif, South Korea: Insights from geochemistry, chromian-spinel chemistry and SHRIMP U-Pb geochronology
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Paleozoic tectonics of the southwestern Gyeonggi massif, South Korea: Insights from geochemistry, chromian-spinel chemistry and SHRIMP U-Pb geochronology

机译:韩国西南京畿地块的古生代构造学:来自地球化学,生辉石-脊柱化学和SHRIMP U-Pb地球年代学的见解

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摘要

Arc magmas, metavolcanics and hydrated mantle peridotite from the Hongseong area in western Gyeonggi massif provide evidence for Paleozoic subduction tectonics in the Korean Peninsula. Zircons in a tonalitic orthogmeiss from the Wolhyeonri complex dated in this study through SHRIMP U-Pb technique yield ages of ca. 437 Ma and ca. 414 Ma. In addition, SHRIMP U-Pb zircon dating of a garnet-bearing paragneiss in the Wolhyeonri complex records evidence for Middle Paleozoic (ca. 427 Ma) thermal metamorphism. Petrological and geochemical data from the Paleozoic suite provide robust evidence for mid Paleozoic arc-related magmatism.
机译:来自京畿道西部洪城地区的弧浆岩浆,超火山岩和水合地幔橄榄岩为朝鲜半岛的古生代俯冲构造提供了证据。通过SHRIMP U-Pb技术,本研究中的Wolhyeonri配合物制成的眼状正长形锆石中的锆石产生的年龄大约为。约437 Ma。 414马。此外,Wolhyeonri复合体中的带石榴石的石阶的SHRIMP U-Pb锆石测年记录了中古生代(约427 Ma)热变质的证据。来自古生代组的岩石学和地球化学数据为中古生代弧相关的岩浆作用提供了有力的证据。

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