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Geoscience ›› 2019, Vol. 33 ›› Issue (02): 315-324.DOI: 10.19657/j.geoscience.1000-8527.2019.02.07

• Geophysics • Previous Articles     Next Articles

Quaternary Magnetostratigraphy Record in Sediments from Borehole BHS01 in the Bohai Strait

SUN Jun1,2,3(), YANG Huiliang1,2, HE Lei1,2, CHU Hongxian1,2(), LU Yue1,2,3, LI Panfeng1,2, LIU Changchun1,2, QI Jianghao1,2, QIANG Xiaoke4   

  1. 1. Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, Shandong 266071, China
    2. Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao, Shandong 266071, China
    3. School of Ocean Sciences, China University of Geosciences, Beijing 100083, China
    4. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an,Shaanxi 710075, China
  • Received:2018-12-08 Revised:2019-03-08 Online:2019-05-08 Published:2019-05-08
  • Contact: CHU Hongxian

Abstract:

Magenetostratigraphy is an effective method to establish reliable geochronological framework, which is critical for reconstructing long-term history of climatic and environmental changes in the past. A detailed palaeomagenetism study on sediments from borehole BHS01 (121.3 m) which is located in the Bohai Strait has been carried out. The results show that the core from the borehole consists of three normal magnetozones which can be correlated to Brunhes, Jaramillo, Olduvai. The basal age of the core is estimated at about 2.25 Ma by the extrapolation of the sedimentation rate in the Matuyama Chron. The Brunhes/Matuyama boundary was found at the core depth of 46.4 m. Thus, through the comprehensive analysis of lithologic, magnetic and sedimentary rate characteristics, we divide the evolutional process of BHS01 into three sedimentary phases: phaseⅠ(2.25 to 1.46 Ma) mainly develops in a fluvial sedimentation; phaseⅡ(1.46 to 0.78 Ma) is accompanied with a stable lacustrine sedimentation; and phaseⅢ(0.78 to 0 Ma) develops in a marine and terrestrial sedimentation. Our results provide a reliable chronological framework for the borehole, facilitating the stratigraphic division and evolutional process of the Quaternary in the Bohai Strait and its neighboring regions.

Key words: Bohai Strait, borehole BHS01, magenetostratigraphy, Quaternary

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