Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (1): 85-95.doi: 10.13278/j.cnki.jjuese.20180099

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Provenance Discrimination of Detrital Zircon U-Pb Dating in the Core CSDP-1 in the Continental Shelf of South Yellow Sea

He Mengying1,2, Mei Xi3,4, Zhang Xunhua5, Liu Jian3,4, Guo Xingwei3,4, Zheng Hongbo6,7   

  1. 1. School of Geography Science, Nanjing Normal University, Nanjing 210023, China;
    2. Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, China;
    3. Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, Shandong, China;
    4. Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266071, Shandong, China;
    5. Nanjing Center, China Geological Survey, Nanjing 210016, China;
    6. Research Center of Earth System Science, Yunnan University, Kunming 650500, China;
    7. Institute of Tibetan Plateau Research, CAS, Beijing 100101, China
  • Received:2018-05-10 Published:2019-01-18
  • Supported by:
    Supported by National Marine Geology Special Project of China (DD20160147),Natural Science Foundation of China (41602180) and Natural Science Foundation of Jiangsu Province (BK20150974)

Abstract: South Yellow Sea is the part of the eastern shelf sea,and its sediments record the information of the sources, the climate and the paleo-environmental evolution. The detrital zircon U-Pb dating of the Core CSDP-1 in the western South Yellow Sea was determined by laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS). The results show that the zircon age distribution of the Core CSDP-1 sediment mainly falls into five groups:300-100, 500-300,1 000-700,2 100-1 700 and 2 600-2 300 Ma. From the bottom to the top, the zircon contents in the sediments do not vary greatly except in the age groups of 1 000-700 Ma and 2 100-1 700 Ma; The Yangtze River, the Yellow River, the Old Yellow River and the Huaihe River are the possible sources of the drilling area. The detrital zircon U-Pb age distribution in sediments is significantly different, among which the Yangtze River sediments are characterized by 1 000-700 Ma zircons,and the content of 2 100-1 700 Ma zircon in the Yellow River sediments is the highest. The content of 500-300 Ma zircons from the Old Yellow River and the Huaihe River sediments are higher than that in the Yellow River and the Yangtze River. Combined with the Core CSDP-1 and the river sediments,it can be concluded that the core site has been contributed by multi-source materials since 3.20 Ma. The Yangtze River is the dominant source, followed by the Huaihe River. However, the Huaihe River didn't affected the core area until 2.16 Ma. The material of the Yellow River started to be found in the drilling area at about 0.78 Ma; and since then,the Yellow River has been the main material source of the core site. The Old Yellow River had almost no effect on the drilling area.

Key words: South Yellow Sea, Core CSDP-1, detrital zircon U-Pb dating, provenance tracing

CLC Number: 

  • P736.4
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