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      서부 경기육괴에 분포하는 태안층의 퇴적시기와 기원지에 대한 고찰 = A Review on the Depositional Age and Provenance of the Taean Formation in the Western Gyeonggi Massif

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      다국어 초록 (Multilingual Abstract)

      Various studies regarding the sedimentary environment, depositional age, provenance, and metamorphic history have been carried out on the Taean Formation in the western part of Gyeonggi Massif, since the unique detrital zircon age pattern was revealed. This review paper introduces the previous researches on the Taean Formation and discusses the depositional age and provenance. The Taean Formation was traditionally regarded as a Precambrian stratigraphic unit, but recently it is interpreted to be a middle or upper Paleozoic formation due to the occurrence of large amounts of Early to Middle Paleozoic detrital zircons. The Taean Formation consists of metasandstone, argillaceous schist, and phyllite which are mainly made up of quartz and mica. The protoliths are interpreted as turbidites deposited in deep sea fan environment. The Taean Formation has been interpreted to be deposited between the Devonian to Triassic ages given the age differences between detrital zircons and intrusive rocks. There are two opinions that the deposition age is close to the Devonian or the Permian period. The provenance of this formation is supposed to be South China block, Chinese collisional belt, or Gyeonggi Massif. Given the available detrital zircon ages of the Taean Formation and other Korean (meta)sedimentary rocks, the Taean Formation shares major source rocks with Yeoncheon Group and Pibanryeong Unit of the Okcheon Supergroup, but their source regions are not entirely consistent. Considering the existing hypotheses about the depositional timing and provenance, we put weight on the possibility that the Taean Formation was deposited between Permian and Early Triassic periods. However, further studies on the stratigraphy and sedimentary petrology are needed to clarify its definition and to elucidate the provenance.
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      Various studies regarding the sedimentary environment, depositional age, provenance, and metamorphic history have been carried out on the Taean Formation in the western part of Gyeonggi Massif, since the unique detrital zircon age pattern was revealed...

      Various studies regarding the sedimentary environment, depositional age, provenance, and metamorphic history have been carried out on the Taean Formation in the western part of Gyeonggi Massif, since the unique detrital zircon age pattern was revealed. This review paper introduces the previous researches on the Taean Formation and discusses the depositional age and provenance. The Taean Formation was traditionally regarded as a Precambrian stratigraphic unit, but recently it is interpreted to be a middle or upper Paleozoic formation due to the occurrence of large amounts of Early to Middle Paleozoic detrital zircons. The Taean Formation consists of metasandstone, argillaceous schist, and phyllite which are mainly made up of quartz and mica. The protoliths are interpreted as turbidites deposited in deep sea fan environment. The Taean Formation has been interpreted to be deposited between the Devonian to Triassic ages given the age differences between detrital zircons and intrusive rocks. There are two opinions that the deposition age is close to the Devonian or the Permian period. The provenance of this formation is supposed to be South China block, Chinese collisional belt, or Gyeonggi Massif. Given the available detrital zircon ages of the Taean Formation and other Korean (meta)sedimentary rocks, the Taean Formation shares major source rocks with Yeoncheon Group and Pibanryeong Unit of the Okcheon Supergroup, but their source regions are not entirely consistent. Considering the existing hypotheses about the depositional timing and provenance, we put weight on the possibility that the Taean Formation was deposited between Permian and Early Triassic periods. However, further studies on the stratigraphy and sedimentary petrology are needed to clarify its definition and to elucidate the provenance.

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      참고문헌 (Reference)

      1 김성원, "한국 경기지괴 서부와 중국 주요지괴에 분포하는 신원생대 및 고생대 암류의 지구조적 특성 대비: 지질연대학적 의미" 대한지질학회 51 (51): 511-524, 2015

      2 박계헌, "옥천변성대 대향산규암층 쇄설성 저어콘의 SHRIMP U-Pb 연령" 대한지질학회 47 (47): 423-431, 2011

      3 Koenraad DE JONG, "안면도에 분포하는 태안층의 변성연대 최초 측정: 233 Ma U-Pb 티타나이트 연대와 231-229 Ma 40Ar/39Ar 백운모 일치 연대" 대한지질학회 50 (50): 593-609, 2014

      4 김명정, "신원생대 백령층군 사암의 쇄설성 저어콘 LA-MC-ICPMS U-Pb 연령: 중원생대집중연령의 의미" 대한자원환경지질학회 49 (49): 433-444, 2016

      5 나준석, "경기육괴 북서부 영흥도-선재도-대부도에 분포하는 변성퇴적암 내 쇄설성 저어콘의 SHRIMP U-Pb 연대" 한국암석학회 21 (21): 31-45, 2012

      6 Mckenzie, N. R., "Trilobites and zircons link north China with the eastern himalaya during the Cambrian" 39 : 591-594, 2011

      7 Kim, S. W., "Tracking Paleozoic evolution of the South Korean Peninsula from detrital zircon records: Implications for the tectonic history of East Asia" 50 : 195-215, 2017

      8 Kim, H. S., "Tectonic linkage between the Korean Peninsula and mainland Asia in the Cambrian: insights from U-Pb dating of detrital zircon" 368 : 204-218, 2013

      9 Kee, W. -S., "Tectonic evolution of the upper crustal units in the mid-western part of the Korean peninsula" Korea Institute of Geoscience and Mineral Resources 242-, 2011

      10 추문섭, "Tectonic evolution of Precambrian basement massifs and an adjoining fold-and-thrust belt (Gyeonggi Marginal Belt), Korea: An overview" 한국지질과학협의회 21 (21): 845-865, 2017

      1 김성원, "한국 경기지괴 서부와 중국 주요지괴에 분포하는 신원생대 및 고생대 암류의 지구조적 특성 대비: 지질연대학적 의미" 대한지질학회 51 (51): 511-524, 2015

      2 박계헌, "옥천변성대 대향산규암층 쇄설성 저어콘의 SHRIMP U-Pb 연령" 대한지질학회 47 (47): 423-431, 2011

      3 Koenraad DE JONG, "안면도에 분포하는 태안층의 변성연대 최초 측정: 233 Ma U-Pb 티타나이트 연대와 231-229 Ma 40Ar/39Ar 백운모 일치 연대" 대한지질학회 50 (50): 593-609, 2014

      4 김명정, "신원생대 백령층군 사암의 쇄설성 저어콘 LA-MC-ICPMS U-Pb 연령: 중원생대집중연령의 의미" 대한자원환경지질학회 49 (49): 433-444, 2016

      5 나준석, "경기육괴 북서부 영흥도-선재도-대부도에 분포하는 변성퇴적암 내 쇄설성 저어콘의 SHRIMP U-Pb 연대" 한국암석학회 21 (21): 31-45, 2012

      6 Mckenzie, N. R., "Trilobites and zircons link north China with the eastern himalaya during the Cambrian" 39 : 591-594, 2011

      7 Kim, S. W., "Tracking Paleozoic evolution of the South Korean Peninsula from detrital zircon records: Implications for the tectonic history of East Asia" 50 : 195-215, 2017

      8 Kim, H. S., "Tectonic linkage between the Korean Peninsula and mainland Asia in the Cambrian: insights from U-Pb dating of detrital zircon" 368 : 204-218, 2013

      9 Kee, W. -S., "Tectonic evolution of the upper crustal units in the mid-western part of the Korean peninsula" Korea Institute of Geoscience and Mineral Resources 242-, 2011

      10 추문섭, "Tectonic evolution of Precambrian basement massifs and an adjoining fold-and-thrust belt (Gyeonggi Marginal Belt), Korea: An overview" 한국지질과학협의회 21 (21): 845-865, 2017

      11 Choi, P. -Y., "Technical Development of Tectonic Evolution and Geologic Information Construction" Korea Institute of Geoscience and Mineral Resources 189-218, 2014

      12 최범영, "Subdivision of the Upper Paleozoic Taean Formation in the Anmyeondo-Boryeong area, west Korea: a preliminary approach to the sedimentary organization and structural features" 한국지질과학협의회 12 (12): 373-384, 2008

      13 Song, M.Y., "Structural and physical properties of the earth crust material in the middle of the Korean Peninsula (1): geology in the vicinity of Chunsu Bay" 13 : 53-65, 1992

      14 Na, K. C., "Stratigraphy and metamorphism of Seosan Group" 15 : 33-39, 1982

      15 Cho, D. -L., "SHRIMP zircon dating of a low-grade meta-sandstone from the Taean Formation: provenance and its tectonic implications" 11 : 3-14, 2007

      16 Cho, M., "SHRIMP U-Pb ages of detrital zircons in metasedimentary rocks of the central ogcheon foldthrust belt, Korea: Evidence for tectonic assembly of Paleozoic sedimentary protoliths" 63 : 234-249, 2013

      17 조문섭, "SHRIMP U-Pb ages of detrital zircons in metasandstones of the Taean Formation, western Gyeonggi massif, Korea: Tectonic implications" 한국지질과학협의회 14 (14): 99-109, 2010

      18 Park, S. -I., "Paleozoic tectonics of the southwestern Gyeonggi massif, South Korea: Insights from geochemistry, chromian-spinel chemistry and SHRIMP U-Pb geochemistry" 26 : 684-698, 2014

      19 Vermeesch, P., "On the visualisation of detrital age distributions" 312-313 : 190-194, 2012

      20 Kim, S. W., "Neoproterozoic plutonic rocks from the western Gyeonggi massif, South Korea: implications for the amalgamation and break-up of the Rodinia supercontinent" 227 : 349-367, 2013

      21 Park, S. -I., "Nature of Late Mesoproterozoic to Early Neoproterozoic magmatism in the western Gyeonggi massif, Korean Peninsula and its tectonic significance" 47 : 291-307, 2017

      22 Vermeesch, P., "Multi-sample comparison of detrital age distributions" 341 : 140-146, 2013

      23 Hu, B., "Mesoproterozoic magmatic events in the eastern North China Craton and their tectonic implications: Geochronological evidence from detrital zircons in the Shandong Peninsula and North Korea" 22 : 828-842, 2012

      24 Vermeesch, P., "IsoplotR: A free and open toolbox for geochronology" 9 : 1479-1493, 2018

      25 Choi, P. -Y., "Geological report of the Yeongheungdo, Pungdo, Gyeongnyeolbiyeoldo, Gungsido, Geoado and Naepasudo sheets"

      26 Lee, S. M., "Geological Report of the Tangjin-Changgohang Sheet (1:50,000)" Korea Institute of Energy and Resources 15-, 1989

      27 Lee, C. W., "Formation and evolution history of the Cretaceous Chunsuman Formation, Korea" 16 : 222-231, 1995

      28 Chang, T.W., "Explanatory text of the geological map of 1:50,000 Seosan·Mohang Sheet"

      29 Kim, D.H., "Explanatory text of the geological map of 1:50,000 Daesan-Igog Sheet"

      30 Kim, S. W., "Early to Middle Paleozoic arc magmatism in the Korean Peninsula: Constraints from zircon geochronology and geochemistry" 113 : 866-882, 2015

      31 Young Seok So, "Distal turbidite fan/lobe succession of the Late Paleozoic Taean Formation, western Korea" 한국지질과학협의회 17 (17): 9-25, 2013

      32 Lee, Y. I., "Detrital zircon geochronology and Nd isotope geochemistry of the basal succession of the Taebaeksan Basin, South Korea: Implications for the Gondwana linkage of the Sino-Korean (North China) block during the Neoproterozoic-early Cambrian" 441 : 770-786, 2016

      33 Han, S., "Detrital zircon ages in Korean mid-Paleozoic meta-sandstones (Imjingang Belt and Taean Formation): Constraints on tectonic and depositional setting, source regions and possible affinity with Chinese terranes" 143 : 191-217, 2017

      34 Kim, S. W., "Detrital zircon U-Pb geochronology and tectonic implications of the Paleozoic sequences in western South Korea" 95 : 217-227, 2014

      35 Lim, S. B., "Depositional systems of the sedimentary basin (I):depositional systems and their evolution of the Proterozoic Paegryeong group and Taean formation" Korea Institute of Geoscience and Mineral Resources 116-, 1999

      36 Guynn, J., "Comparison of detrital zircon age distributions using the K-S test" University of Arizona 2006

      37 Lee, S. R., "Age geochemistry, and tectonic significance of Neoproterozoic alkakine granitoids in the northwestern margin of the Gyeonggi massif, South Korea" 112 : 297-310, 2003

      38 Na, K. C., "A study on the metamorphism in the southwestern part of Gyeonggi Massif" 1 : 25-33, 1992

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