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Factors controlling mud accumulation in the Heuksan mud belt off southwestern Korea

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Abstract

The Heuksan mud belt (hereafter HMB) is 20~50 km wide, ~200 km long, and ~50 m thick, having accumulated in the course of the Holocene transgression on the tide-dominated epicontinental shelf southwest of Korea. The internal architecture of the HMB is characterized by offshore prograding clinoforms. Of particular interest are the depositional processes responsible for this anomalously thick mud accumulation within a relatively short period of time. Tidal currents are important in the dispersal of mud in the HMB, although these alone cannot explain such an enormous mud deposit. In order to understand the formative processes of the HMB, a detailed sedimentary facies analysis, including high-resolution grain-size measurements, has been conducted on more than 30 short cores and three long drill cores recovered from the mud belt. Five major mud facies were identified. Of these, mud sequences showing a thickening–thinning trend of alternating silt and clay laminae suggestive of a tidal origin occur dominantly at inner to mid shelf locations. By contrast, internally structureless muds with sharp bases and no bioturbation, which are interpreted of representing fluid-mud deposits, are widespread at mid to outer shelf locations. Wave-generated mud ripples and storm beds on the inner shelf suggest that storm waves in winter resuspend previously deposited mud to form near-bed fluid-mud suspensions with resulting gravity-driven mud transport across the low-gradient outer shelf. This previously not recognized process is probably a major factor controlling depositional processes on the giant mud belt, enabling rapid accumulation and offshore progradation even during transgression, i.e., at times of sea-level rise.

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Acknowledgments

This study is part of the MSc thesis of the co-author Hun Jun Ha, which was financially supported by the KIGAM basic research program (GP2015-040). We are grateful to Young Sook Baek for the identification of ichnofabrics. We also wish to thank the crew of the research vessel Tamhae II for logistic support during the survey. We acknowledge Burg W. Flemming for his review and language corrections of an earlier draft, and Steve A. Kuehl for additional comments.

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The authors declare that there is no conflict of interest with third parties.

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Correspondence to Tae Soo Chang.

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Chang, T.S., Ha, H.J. & Chun, S.S. Factors controlling mud accumulation in the Heuksan mud belt off southwestern Korea. Geo-Mar Lett 35, 461–473 (2015). https://doi.org/10.1007/s00367-015-0421-7

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