Subdivision of the Upper Paleozoic Taean Formation in the Anmyeondo-Boryeong area, west Korea: a preliminary approach to the sedimentary organization and structural features

Choi, Pom-yong;Rhee, Chul-Woo;Lim, Soon-Bok;So, Yeong-Seok

  • Published : 2008.12.10

Abstract

A preliminary analysis of sedimentary organization and detailed geological mapping of the Upper Paleozoic Taean Formation have been conducted in the Anmyeondo-Boryeong area. The Taean Formation comprises the ‘sandy unit’ and ‘sandy-muddy unit’. The former unit consists of massive or bedded sandstone beds often with scoured base, and the latter unit consists of sandstone beds graded from the massive sandstone to laminated siltstone or pelagic mudstone, representing the Bouma sequence. Based on the differing patterns of facies stacking, the Taean Formation is informally divided into the Sinni, Sinon, Kkotji, Seungeon, Jungjang and Nudong units in ascending order. The lower four units show largely N-S trending paleoflow, while the upper two ones show NE-SW to E-W trending paleoflows. Such a change in sedimentary supply directions could be resulted from changes in depositional regime and/or allogenic controls including tectonics

Keywords

References

  1. Bouma, A.H., Kuenen, P.H., and Shepard, F. P., 1962, Sedimentology of some Flysch deposits; a graphic approach to facies interpretation. Elsevier Publishing, Amsterdam, 168 p.
  2. Chang, T.W. and Lee, S.Y., 1982, Explanatory text of the geological map of 1:50,000 Seosan.Mohang Sheet. Korea Institute of Energy and Resources, 30 p.
  3. Cheong, C.H., 1969, Stratigraphy and paleontology of the Samcheog coalfield, Gangweondo, Korea (1). Journal of the Geological Society of Korea, 5, 13-56
  4. Cheong, C.H., 1973, A paleontological study of the fusulinids from the Samcheog coalfield, Korea. Journal of the Geological Society of Korea, 9, 47-88
  5. Cho, D.L., 2007a, SHRIMP zircon dating of a low-grade meta-sandstone from the Taean Formation: Provenance and its tectonic implications. KIGAM Bulletin, 11, 3-14
  6. Cho, D.L., 2007b, Chronostratigraphy of the Imjingang Belt (in Korean). In: Kee, W.S.(ed.), Tectonic correlation of major crustal units and construction of geoscience system of Northeast Asia, GP2007-004-2007(1), KIGAM/MOST, 63-78
  7. Choi, P.Y., 1995, Aspects of stress inversion methods in fault tectonic analysis. Annales Tectonicae, 9, 22-28
  8. Chough S.K., Kwon S.T., Ree J.H., and Choi D.K., 2000, Tectonic and sedimentary evolution of the Korean Peninsula: a review and new view. Earth-Science Reviews, 52, 175-235 https://doi.org/10.1016/S0012-8252(00)00029-5
  9. KIGAM, 2001, Tectonic map of Korea (1:1,000,000 scale). Korea Institute of Geoscience and Mineral Resources
  10. Kim, D.H. and Hwang, J.H., 1982, Explanatory text of the geological map of 1:50,000 Daesan-Igog Sheet. Korea Institute of Energy and Resources, 27 p.
  11. Lee, B.J., Kim, D.H., Choi, H.I., Kee, W.S., and Park, K.H., 1996, Explanatory note of the 1:250,000 Daejeon Sheet. MOST/KIGAM, 59 p.
  12. Lee, B.J., Lee, S.R., and Cho, D.L., 1999, Explanatory text of the geological map of Daebudo Sheet. Korea Institute of Geoscience and Mineral Resources, 33 p.
  13. Lee, C.H. and Kim, S.S., 1963, Explanatory text of the geological map of Hongsong Sheet. Geological Survey of Korea, 33 p.
  14. Lee, C.W., Baik, C.H., and Lee, D.W., 1995, Formation and evolution history of the Cretaceous Cheonsuman Formation, Korea. Journal of the Korean Earth Science Society, 16, 222-231
  15. Lee, S.M., Kim, H.S., Na, K.C., and Park, B.Y., 1989, Geological Report of the Tangjin-Changgohang Sheet (1:50,000). Korea Institute of Energy and Resources, 15 p.
  16. Lim, S.B., Choi, H.I., Kim, B.C., and Kim, J.C., 1999, Depositional systems of the sedimentary basins (I): Depositional systems and their evolution of the Proterozoic Paegryeong Group and Taean Formation. MOST/KIGAM, 116 p.
  17. Lim, S.B., Chun, H.Y., Kim, Y.B., Kim, B.K., and Cho, D.L., 2005, Geologic ages, stratigraphy and geological structures of the metasedimentary strata in Bibong-Yeonmu area, NW Okcheon belt, Korea. Journal of the Geological Society of Korea, 41, 335-368
  18. Lim, S.B., Chun, H.Y., Kim, Y.B., Kim, B.K., and Song, K.Y., 2006, Stratigraphy and geological ages of the metasedimentary strata in Jinsan-Boksu area, NW Okcheon belt. Journal of the Geological Society of Korea, 42, 149-174
  19. Lim, S.B., Chun, H.Y., Kim, Y.B., Lee, S.R., and Kee, W.S., 2007, Geological ages and stratigraphy of the metasedimentary strata in Hoenam-Miwon area, NW Okcheon belt. Journal of the Geological Society of Korea, 43, 33-39
  20. Na, K.C., Kim, H.S., and Lee S.H., 1982, Stratigraphy and metamorphism of Seosan Group. Journal of Economic and Environmental Geology, 15, 33-39
  21. Na, K.C., 1992, A study on the metamorphism in the southwestern part of Gyeonggi Massif. Journal of Petrological Society of Korea, 1, 25-33
  22. Pickering, K.T., Hiscott, R.N., and F.J. Hein., 1989, Deep marine environments: Clastic sedimentation and tectonics. Unwin Hyman, London, 416 p.
  23. Ree, J.H., Cho, M., Kwon, S.T., and Nakamura, E., 1996, Possible eastward extension of Chinese collision belt in South Korea: the Imjingang belt. Geology, 24, 1071-1074 https://doi.org/10.1130/0091-7613(1996)024<1071:PEEOCC>2.3.CO;2
  24. Song, M.Y. and Woo, Y.K, 1992, Structural and physical properties of the earth curst material in the middle of the Korean Peninsula (1): geology in the vicinity of Chonsu Bay. Journal of the Korean Earth Science Society, 13, 53-65
  25. Stow, D.A.V. and Shanmugam, G., 1980, Sequence of structures in fine-grained turbidites: comparison of recent deep-sea and ancient flysch sediments. Sedimentary Geology, 25, 23-42 https://doi.org/10.1016/0037-0738(80)90052-4
  26. Stow, D.A.V. and Mayall, M., 2000, Deep-water sedimentary systems: New models for the 21st century. Marine and Petroleum Geology, 17, 125-135 https://doi.org/10.1016/S0264-8172(99)00064-1
  27. Yin, A. and Nie, S., 1993, An indentation model for the North and South China collision and the development of the Tan-Lu and Honam fault systems, eastern Asia. Tectonics, 12, 801-813 https://doi.org/10.1029/93TC00313