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Article Navigation >  Acta Sedimentologica Sinica  > 1997  >  15(3): 141-144

Zhang Jiaqiang, Cong Youzi, Li Congxian. Magnetic Fabric Features and Significace of Changshan Archipelago Loess in Shandong Province, China[J]. Acta Sedimentologica Sinica, 1997, 15(3): 141-144.
Citation: Zhang Jiaqiang, Cong Youzi, Li Congxian. Magnetic Fabric Features and Significace of Changshan Archipelago Loess in Shandong Province, China[J]. Acta Sedimentologica Sinica, 1997, 15(3): 141-144.
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Magnetic Fabric Features and Significace of Changshan Archipelago Loess in Shandong Province, China

  • 1 Department of Marine Geolog y and Geophysics of Tongji University, Shanghai 200092;

  • 2 First Institute of Oceanography, State Oceanic Administration, Qingdao 266003

  • Received Date: 1996-06-12
  • The Middle Pleistocent loes and the Late Pleistocene loess at changshan archipelago were previouslyseen as eolian deposit, which were deposited by north-west monsoon. Comparative analyses on magneticfabric features of them show that the Middle Pleistocene loess belongs to proluvium of talus whose mate-rials prtially came from local crust of weathering and were partially brought to here from the vicinity bywind; the late pleistocene loess belongs to eoilan deposit whose materials were brought to here from ex-posed sea floor nearby by wind. In the Late Pleistocene epoch, surface wind field changed with topogra-phy, and wind dircction may be different in different places.
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    [2] 曹家欣. 山东庙岛列岛与蓬莱沿岸地貌. 海洋学报, 1989, 11( 5): 602 ～ 610.
    [3] 曹家欣,严润娥,王欢. 山东庙岛群岛的红色风化壳与棕红色土及其古气候意义. 中国科学, B辑, 1994, 24( 2): 216 ～ 224.
    [4] 丛友滋,李培英. 沉积磁化率各向异性与古水流、古砂堤对应关系的研究. 第四届全国古地磁学术会议论文摘要汇编. 1989, 52.
    [5] B. B. Ellwood. Eared and planetary science letters, 1979, 43:309 ～ 314.
    [6] 刘秀铭,许同春,许东生. 中国黄土磁化率各向异性怀成因及其对第四纪研究的意义. 中国科学, B 辑, 1989, ( 4): 441～448.
    [7] 许峰宁. 下蜀土的岩石磁学特征. 南京师范大学学报 (自然科学版 ). 1993, 16(增刊): 44 ～ 50.
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  • Received:  1996-06-12

Magnetic Fabric Features and Significace of Changshan Archipelago Loess in Shandong Province, China

  • 1 Department of Marine Geolog y and Geophysics of Tongji University, Shanghai 200092;
  • 2 First Institute of Oceanography, State Oceanic Administration, Qingdao 266003
  • Received Date: 1996-06-12

Abstract: The Middle Pleistocent loes and the Late Pleistocene loess at changshan archipelago were previouslyseen as eolian deposit, which were deposited by north-west monsoon. Comparative analyses on magneticfabric features of them show that the Middle Pleistocene loess belongs to proluvium of talus whose mate-rials prtially came from local crust of weathering and were partially brought to here from the vicinity bywind; the late pleistocene loess belongs to eoilan deposit whose materials were brought to here from ex-posed sea floor nearby by wind. In the Late Pleistocene epoch, surface wind field changed with topogra-phy, and wind dircction may be different in different places.

Zhang Jiaqiang, Cong Youzi, Li Congxian. Magnetic Fabric Features and Significace of Changshan Archipelago Loess in Shandong Province, China[J]. Acta Sedimentologica Sinica, 1997, 15(3): 141-144.
Citation: Zhang Jiaqiang, Cong Youzi, Li Congxian. Magnetic Fabric Features and Significace of Changshan Archipelago Loess in Shandong Province, China[J]. Acta Sedimentologica Sinica, 1997, 15(3): 141-144.
shu

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