GRAIN SIZE CHARACTERISTICS OF THE CORE SEDIMENTS IN THE EASTERN LIAODONG BAY AND IMPLICATIONS FOR DEPOSITIONAL ENVIRONMENT

DOU Yanguang; LIU Jingpeng; LI Jun; ZHAO Jingtao

doi:10.3724/SP.J.1140.2013.05027

Marine Geology & Quaternary Geology > 2013 > 33(5): 27-34. > DOI: 10.3724/SP.J.1140.2013.05027

DOU Yanguang, LIU Jingpeng, LI Jun, ZHAO Jingtao. GRAIN SIZE CHARACTERISTICS OF THE CORE SEDIMENTS IN THE EASTERN LIAODONG BAY AND IMPLICATIONS FOR DEPOSITIONAL ENVIRONMENT[J]. Marine Geology & Quaternary Geology, 2013, 33(5): 27-34. DOI: 10.3724/SP.J.1140.2013.05027

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GRAIN SIZE CHARACTERISTICS OF THE CORE SEDIMENTS IN THE EASTERN LIAODONG BAY AND IMPLICATIONS FOR DEPOSITIONAL ENVIRONMENT

1. Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071;
2. Qingdao Institute of Marine Geology, Ministry of Land and Resources, Qingdao 266071

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Received Date: May 20, 2012
Revised Date: August 13, 2012

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Abstract

Abstract

Four cores of sediment taken from the Eastern Liaodong Bay were analyzed for grain sizes. The results indicate that the saltation component of the Core LDC47 sediments on the north of the tidal sand ridge is as high as 70%, which is composed of two straight lines in the probability cumulative frequency diagram. It means that the sediments of Core LDC47 were formed under a to-and-fro current and indicates an origin of tidal sand ridge. It is deduced that these sediments are mainly from the Laotieshan Channel. However, the saltation component of the upper part (0~2.10 m) of the Core LDC30 is less than 40%, showing as a straight line in the probability cumulative frequency diagram, as the lower part shows no difference with the upper. The saltation component in the lower part is even much lower. It suggests that the upper part of Core LDC30 was probably formed in a pro-delta environment of the highstand system tract, whereas the lower part of the Core LDC30 was deposited in a wetland or tidal flat environment. The upper part of the Core LDC71 and LDC82 are thin with high suspension component and become coarser downwards. The sediments of the Core LDC30, LDC71 and LDC82 are all belonging to coastal sands possibly derived from the rivers nearby and coastal bed rock erosion.
- core sediments,
- grain-size characteristics,
- provenance,
- Liaodong Bay

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References (17)

References

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GRAIN SIZE CHARACTERISTICS OF THE CORE SEDIMENTS IN THE EASTERN LIAODONG BAY AND IMPLICATIONS FOR DEPOSITIONAL ENVIRONMENT