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10.1016/J.PRECAMRES.2021.106363

A coeval unconformity in the Sino-Korean Block has recently been documented from several different areas of China; however, the stratigraphic position of this boundary in the eastern margin of the Sino-Korean Block in the Taebaek Group, central-eastern Korea, is still elusive.

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10.1007/s00531-019-01717-7

Results indicate that the two distinct age spectra of detrital zircon resulted from provenance change combined with a strong function of sediment grain size within host siliciclastic rocks of the Taebaek Group.

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10.1007/s12303-018-0085-1

The Furongian Hwajeol Formation of the Taebaek Group in mid-eastern Korea is host to such early Paleozoic subtidal cyclic successions, showing limestone- mudstone alternations.

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Taebaek Group

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Mar 21, 2023

What is/are Taebaek Group?

Taebaek Group - A coeval unconformity in the Sino-Korean Block has recently been documented from several different areas of China; however, the stratigraphic position of this boundary in the eastern margin of the Sino-Korean Block in the Taebaek Group, central-eastern Korea, is still elusive. ^[1] Results indicate that the two distinct age spectra of detrital zircon resulted from provenance change combined with a strong function of sediment grain size within host siliciclastic rocks of the Taebaek Group. ^[2] The Furongian Hwajeol Formation of the Taebaek Group in mid-eastern Korea is host to such early Paleozoic subtidal cyclic successions, showing limestone- mudstone alternations. ^[3]