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Taebaeksan Basin

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Journal Article
Journal: GSA Bulletin
Published: 30 June 2020
GSA Bulletin (2021) 133 (3-4): 488–504.
.... Our new sensitive high-resolution ion microprobe data from 14 sandstones of the Taebaeksan Basin, Korea, indicate that its platform shelf sequences, typified by trilobite faunal assemblages diagnostic of the NCC, record the vestige of coeval arc magmatism. Detrital zircons analyzed from the sandstones...
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Journal Article
Published: 11 September 2015
Journal of Paleontology (2015) 89 (3): 377–384.
... the macroinvertebrate fossil assemblage from the Machari Formation of the Yeongwol Group, Taebaeksan Basin, Korea, and comprises diverse trilobites of Cambrian Series 3 to Furongian, with some inarticulate brachiopods, monoplacophorans, gastropods, and hyoliths. It was partly introduced...
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Journal Article
Published: 01 May 2010
Journal of Paleontology (2010) 84 (3): 417–443.
... Supergroup in the Taebaeksan Basin. The formation yields a variety of marine invertebrate fossils, including brachiopods, molluscs, echinoderms, corals, fusulinids, and conodonts. Diverse brachiopods are described from six siliciclastic horizons of the formation at three localities, including 23 species...
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Journal Article
Published: 01 November 2007
Journal of Paleontology (2007) 81 (6): 1454–1465.
...SEUNG-BAE LEE; DUCK K. CHOI Abstract The Pseudokoldinioidia Fauna is a newly documented uppermost Cambrian trilobite assemblage from the Dongjeom Formation of the Taebaek Group, Taebaeksan Basin, Korea. It is characterized by low species diversity comprising six trilobite taxa: Micragnostus...
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Journal Article
Published: 01 January 2005
Journal of Paleontology (2005) 79 (1): 139–151.
...SEUNG-BAE LEE; BERTRAND LEFEBVRE; DUCK K. CHOI Abstract The oldest echinoderms and first cornute stylophorans ever reported from Korea are described, based on more than 40 specimens collected from the Late Cambrian of the Taebaeksan Basin. New material doubles the number of stylophorans described...
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Series: Geological Society, London, Special Publications
Published: 17 May 2023
DOI: 10.1144/SP533-2022-48
EISBN: 9781786209658
... Abstract The Ordovician succession of the Korean Peninsula is part of the Cambro-Ordovician Joseon Supergroup exposed in the Taebaeksan Basin of South Korea and the Pyeongnam Basin of North Korea. This review summarizes the advances made on these successions over the past two decades, focusing...
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Figure 1. Location maps. 1, tectonic map of Korean peninsula and surrounding area which shows the location of the Taebaeksan Basin. Q–D  =  Qinling–Dabie belt, S  =  Sulu Belt, N  =  Nangnim Massif, P  =  Pyeongnam Basin, I  =  Imjingang Belt, G  =  Gyeonggi Massif, O  =  Okcheon Belt, T  =  Taebaeksan Basin, Y  =  Yeongnam Massif; 2, Geological map of the Taebaeksan Basin which shows the distribution of the lower Palaeozoic Joseon Supergroup in the Taebaeksan Basin. The asterisk indicates the location of the Sagundari section from which the material for this study was collected.
Published: 01 March 2010
Figure 1. Location maps. 1 , tectonic map of Korean peninsula and surrounding area which shows the location of the Taebaeksan Basin. Q–D  =  Qinling–Dabie belt, S  =  Sulu Belt, N  =  Nangnim Massif, P  =  Pyeongnam Basin, I  =  Imjingang Belt, G  =  Gyeonggi Massif, O  =  Okcheon Belt, T
Journal Article
Published: 01 November 2013
Journal of Paleontology (2013) 87 (6): 991–1003.
... between the Daegi and Sesong formations is diachronous within the Taebaeksan Basin. The Daegi/Sesong formation boundary in Korea is comparable to the Zhangxia/Gushan boundary in North China in that it displays an abrupt change from a carbonate-dominant facies to a shale-dominant facies. The correlation...
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 Figure1—Index maps. 1, Tectonic map of the Korean peninsula and surrounding area showing the location of the Taebaeksan Basin. Q-D = Qinling-Dabie Belt, S = Sulu Belt, N = Nangnim Massif, P = Pyeongnam Basin, I = Imjingang Belt, G = Gyeonggi Massif, O = Okcheon Belt, T = Taebaeksan Basin, Y = Yeongnam Massif; 2, Simplified geologic map showing the distribution of the lower Paleozoic Joseon Supergroup in the Taebaeksan Basin. The fossil locality of the Pseudokoldinioidia Fanua is indicated by a solid arrow near the eastern edge of the map. Modified from Choi et al. (2001)
Published: 01 November 2007
Figure 1 —Index maps. 1 , Tectonic map of the Korean peninsula and surrounding area showing the location of the Taebaeksan Basin. Q-D = Qinling-Dabie Belt, S = Sulu Belt, N = Nangnim Massif, P = Pyeongnam Basin, I = Imjingang Belt, G = Gyeonggi Massif, O = Okcheon Belt, T = Taebaeksan Basin, Y
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Locality maps. 1, index map showing the distribution of Cambro–Ordovician strata in the Korean peninsula and adjacent area; star with ‘J' denotes the location of the Jiulongshan section; and ‘T' indicates the location of the Taebaeksan Basin; 2, simplified geological map of the Taebaeksan Basin which shows the distribution of the lower Paleozoic Joseon Supergroup in the Taebaeksan Basin; star with ‘G' indicates the location of the Gadeoksan section; the rectangle in the south represents the location of the Taebaek area represented in 3; 3, geological map of the Taebaek area. The asterisks indicate the locations of the Jikdong and Seokgaejae sections from which the material for this study was collected.
Published: 01 November 2013
Figure 1 Locality maps. 1 , index map showing the distribution of Cambro–Ordovician strata in the Korean peninsula and adjacent area; star with ‘J' denotes the location of the Jiulongshan section; and ‘T' indicates the location of the Taebaeksan Basin; 2 , simplified geological map
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(a) Simplified tectonic map of the Sino–Korean Block (yellow colour). Light yellow colour in the Korean Peninsula and Japan represents the tectonic provinces under debate. NM – Nangrim Massif; PB – Pyeongnam Basin; IB – Imjingang Belt; GM – Gyeonggi Massif; OMB – Okcheon Metamorphic Belt; TB – Taebaeksan Basin; YM – Yeongnam Massif; HB – Hida Belt. (b) Simplified geologic map of the Taebaeksan Basin (modified after Korea Institute of Geoscience and Mineral Resources (KIGAM), 1995).
Published: 20 November 2017
Belt; TB – Taebaeksan Basin; YM – Yeongnam Massif; HB – Hida Belt. (b) Simplified geologic map of the Taebaeksan Basin (modified after Korea Institute of Geoscience and Mineral Resources (KIGAM), 1995 ).
Journal Article
Published: 20 November 2017
Geological Magazine (2019) 156 (3): 471–484.
... Belt; TB – Taebaeksan Basin; YM – Yeongnam Massif; HB – Hida Belt. (b) Simplified geologic map of the Taebaeksan Basin (modified after Korea Institute of Geoscience and Mineral Resources (KIGAM), 1995 ). ...
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Journal Article
Published: 01 March 2011
Journal of Paleontology (2011) 85 (2): 279–297.
...Seung-Bae Lee; Duck K. Choi Abstract The Eosaukia fauna is proposed for the upper Furongian trilobite assemblage from the interval spanning from the upper part of the Hwajeol Formation to the lowermost part of the Dongjeom Formation in the Taebaek Group, Taebaeksan Basin, Korea. It is characterized...
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Journal Article
Published: 09 February 2017
Geological Magazine (2018) 155 (6): 1247–1262.
... the ontogeny of the two co-occurring shumardiid trilobites, Akoldinioidia latus Park and Kihm and Koldinioidia choii Park and Kihm, from the middle Furongian Hwajeol Formation, Taebaeksan Basin, Korea. Interestingly, protaspides of the two shumardiids have a bulbous morphology. Given the stratigraphic...
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Journal Article
Published: 01 May 2013
Journal of Paleontology (2013) 87 (3): 379–390.
.... This study deals with the ontogeny of the Furongian (late Cambrian) ptychaspidid trilobite, Quadraticephalus elongatus ( Kobayashi, 1935 ), from the Hwajeol Formation of the Taebaek Group, Taebaeksan Basin, Korea, with a special focus on the segmentation process during the meraspid pygidial development...
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Journal Article
Published: 01 November 2006
Journal of Paleontology (2006) 80 (6): 1072–1086.
...SEUNG-BAE LEE; BERTRAND LEFEBVRE; DUCK K. CHOI Abstract Abundant isolated elements of cornute and mitrate stylophorans were recovered from the upper Tremadocian Tumugol Formation in the Taebaeksan Basin, Korea. Cornute skeletal elements comprise a diverse assemblage of marginals and brachials...
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Journal Article
Published: 01 September 2003
Journal of Paleontology (2003) 77 (5): 895–907.
...PAUL S. HONG; JEONG GU LEE; DUCK K. CHOI Abstract Acid-resistant specimens of trilobites were recovered from the dissolved residues of lime mudstone collected from the lower part of the Machari Formation, Yongwol Group, Taebaeksan Basin, Korea. One of the samples yields a trilobite assemblage...
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Regional geology and distribution of various types of skarn deposits within the Taebaeksan Basin, South Korea.
Published: 01 May 2012
Fig. 2 Regional geology and distribution of various types of skarn deposits within the Taebaeksan Basin, South Korea.
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(A) Simplified paleogeographic map, showing the location of the North China Craton (NCC) and other Asian continental blocks along the northern Gondwana margin at ca. 500 Ma (modified after Cawood et al., 2018). The shared detrital belt of the Pacific Gondwana zircons (dotted) is an approximation; the transport of detritus from the Paterson-Petermann orogen (PPO) is denoted by blue arrows. Note that the Terra Australis Orogen might have extended toward the proto-Japan arc; this arc complex might have supplied the Cambrian–Ordovician detritus to the Taebaeksan Basin and southeastern NCC (dark blue arrows). (B) Early Paleozoic (ca. 500 Ma) paleogeography of the NCC, schematically showing hypothesized areal distributions of paleolands, shelf areas, and open oceans (modified after Wang et al., 2016b). Present boundaries of the NCC together with post-Ordovician arc complexes are shown for reference. PB—Pyeongnam Basin; TB—Taebaeksan Basin.
Published: 30 June 2020
) is an approximation; the transport of detritus from the Paterson-Petermann orogen (PPO) is denoted by blue arrows. Note that the Terra Australis Orogen might have extended toward the proto-Japan arc; this arc complex might have supplied the Cambrian–Ordovician detritus to the Taebaeksan Basin and southeastern NCC
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Stratigraphies and detrital zircon ages of the Taebaek and Yeongwol groups, Taebaeksan Basin. Left: Stratigraphy of units of the Taebaek Group shown on the Cambrian–Ordovician chronostratigraphic chart (Gradstein et al., 2012). The simplified lithologic column and water-depth curve are adopted from Kwon et al. (2006). Sandstones (Ss) and mudstones (Ms) are shown in white, whereas limestones (Ls) and dolostones (Ds) are in gray. Sample numbers are shown with arrows indicating approximate positions in the lithologic column. Center: Early Paleozoic detrital zircon ages analyzed from the Taebaeksan Basin sandstones of this study (open diamonds) and previous studies (open squares). Uncertainties for the sensitive high-resolution ion microprobe U-Pb ages are shown in black bars. The uncertainties in two ages estimated from the Dongjeom Formation by Kim et al. (2019a) are close to the symbol size. Right: Stratigraphy of units of the Yeongwol Group adopted from Chough (2013).
Published: 30 June 2020
Figure 3. Stratigraphies and detrital zircon ages of the Taebaek and Yeongwol groups, Taebaeksan Basin. Left: Stratigraphy of units of the Taebaek Group shown on the Cambrian–Ordovician chronostratigraphic chart ( Gradstein et al., 2012 ). The simplified lithologic column and water-depth curve