Preliminary study of quaternary magnetostratigraphy in the coastal region of Jiangsu[J]. 海洋湖沼学报(英文), 1988,6(1):71-80.
Songling, Z., Hongcai, Z. & Shuxi, C. Preliminary study of quaternary magnetostratigraphy in the coastal region of Jiangsu., Chin. J. Ocean. Limnol. 6, 71–80 (1988). https://doi.org/10.1007/BF02846569
Preliminary study of quaternary magnetostratigraphy in the coastal region of Jiangsu[J]. 海洋湖沼学报(英文), 1988,6(1):71-80. DOI: 10.1007/BF02846569.
Songling, Z., Hongcai, Z. & Shuxi, C. Preliminary study of quaternary magnetostratigraphy in the coastal region of Jiangsu., Chin. J. Ocean. Limnol. 6, 71–80 (1988). https://doi.org/10.1007/BF02846569DOI:
Preliminary study of quaternary magnetostratigraphy in the coastal region of Jiangsu
摘要
Abstract
The authors obtained the magnetostratigraphic division of Quaternary from the palaeomagnetic records of 7 cores taken from the northern plain of Jiangsu Province. The depositional characteristics of this area are now described. The core near the coastal region of the Yellow Sea showed the sedimentary rate was higher during Brunhes chron
but lower or nearly zero during Matuyama chron. The core located in the middle of the northern plain of Jiangsu Province showed the depositional formation was thin during Brunhes chron
but thicker in Matuyama. This depositional difference indicated obvious differences in the tectonic units
geological basement
and depositional environments of the two periods. This study provides information for the subdivision of Quaternary magnetostratigraphy.
关键词
Keywords
references
Berggren, W.A. et al, 1980. Towards a Quaternary time scale.Quaternary Research 13: 277–302.
Harland, W.B. et al, 1982. A Geologic Time Scale, Cambridge University Press p. 66.
Zhao Songling & Qin Yunshan, 1982. Transgression and Sea Level Changes in the Eastern Coastal Region of China in the Last 300,000 Years. Quaternary Geology and Environment of China, China Ocean Press pp. 147–154.
Zhao Songling, Zhang Hongcai, Huang Qingfu and Cang Shuxi, 1983. Paleogeographic changes of the Yangtze River delta region since the late Pleistocene.Marine geology & Quaternary geology 3(4): 35–45.
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