CRETACEOUS THERMAL EVENT AROUND THE GONGSUWON THRUST IN THE NORTHEASTERN OKCHEON BELT: EVIDENCE FROM RB−SR GEOCHRONOLOGY OF PALEOZOIC SEDIMENTARY ROCKS

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dc.contributor.author Sagong H.
dc.contributor.author Kwon S.
dc.contributor.author Han R.
dc.contributor.author Ree J.
dc.date.accessioned 2025-02-22T06:18:08Z
dc.date.available 2025-02-22T06:18:08Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=53143678
dc.identifier.citation Geosciences Journal, 2006, 10, 1, 59-66
dc.identifier.issn 1226-4806
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/48111
dc.description.abstract The Gongsuwon thrust together with the Deokpori (Gakdong) thrust in northeastern Okcheon belt is considered to be an important structure in understanding the tectonic evolution of the Korean peninsula following the Permian-Triassic collision between North and South China continents. We obtained Rb-Sr ages for Paleozoic sedimentary rocks around the Gongsuwon thrust to determine the age of petrographically observed thermal metamorphism and possibly constrain the movement age of the thrust. Andalusite, codierite and biotite porphyroblasts overgrow cataclastic foliation of siliceous fault rocks in the Gongsuwon thrust, indicating a post-faulting thermal metamorphism. A marble of the early Paleozoic Makgol Formation in the hanging wall (~200 m northwest from the fault zone center) and a siliceous cataclasite in the fault zone center gave Cretaceous Rb-Sr whole rock fragment ages: 113±21 (2σ) Ma and 68±17 (2σ) Ma, respectively. Sandstones of the late Paleozoic Hambaeksan Formation in the footwall (about 680 m southeast from the fault zone center) yielded an early Tertiary Rb-Sr biotite age of 56.3±6.0 (2σ) Ma, but a Paleoproterozoic Rb-Sr muscovite age of 1774±30 (2σ) Ma, suggesting that the early Tertiary thermal effect for the sandstones was strong enough to reset the Rb-Sr biotite age but weak enough not to affect the Rb-Sr muscovite age, i.e., between ~300°C and ~500°C, and that detrital muscovites in the sandstones were derived from the Precambrian basement rocks. These isotopic ages suggest that there was Cretaceous to early Tertiary thermal event around the Gongsuwon thrust, which is probably associated with well-known plutonism at that time (so-called Bulguksa granite). Available age data, albeit limited, suggest that Cretaceous to early Tertiary thermal metamorphism in the Taebaeksan basin might have been extensive. The movement age of the Gongsuwon thrust is constrained to be older than ~60 Ma.
dc.subject GONGSUWON THRUST
dc.subject CRETACEOUS THERMAL EVENT
dc.subject RB−SR GEOCHRONOLOGY
dc.subject Cretaceous
dc.subject Triassic
dc.subject Permian
dc.subject Cambrian
dc.subject Paleoproterozoic
dc.title CRETACEOUS THERMAL EVENT AROUND THE GONGSUWON THRUST IN THE NORTHEASTERN OKCHEON BELT: EVIDENCE FROM RB−SR GEOCHRONOLOGY OF PALEOZOIC SEDIMENTARY ROCKS
dc.type Статья
dc.identifier.doi 10.1007/bf02910332
dc.subject.age Mesozoic::Cretaceous
dc.subject.age Мезозой::Меловая
dc.subject.age Mesozoic::Triassic
dc.subject.age Мезозой::Триасовая
dc.subject.age Paleozoic::Permian
dc.subject.age Палеозой::Пермская
dc.subject.age Paleozoic::Cambrian
dc.subject.age Палеозой::Кембрийская
dc.subject.age Precambrian::Proterozoic::Paleoproterozoic
dc.subject.age Докембрий::Протерозой::Палеопротерозойская


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