江西九江中更新世红土物质来源研究

林旭, 胡程伟, 吴中海, 赵希涛, 陈济鑫, 李玲玲. 2023. 江西九江中更新世红土物质来源研究[J]. 地球学报, 44(3): 511-521. doi: 10.3975/cagsb.2022.053101
引用本文: 林旭, 胡程伟, 吴中海, 赵希涛, 陈济鑫, 李玲玲. 2023. 江西九江中更新世红土物质来源研究[J]. 地球学报, 44(3): 511-521. doi: 10.3975/cagsb.2022.053101
LIN Xu, HU Cheng-wei, WU Zhong-hai, ZHAO Xi-tao, CHEN Ji-xin, LI Ling-ling. 2023. Provenance Tracing of Middle Pleistocene Red Earth in the Jiujiang Area, Jiangxi Province. Acta Geoscientica Sinica, 44(3): 511-521. doi: 10.3975/cagsb.2022.053101
Citation: LIN Xu, HU Cheng-wei, WU Zhong-hai, ZHAO Xi-tao, CHEN Ji-xin, LI Ling-ling. 2023. Provenance Tracing of Middle Pleistocene Red Earth in the Jiujiang Area, Jiangxi Province. Acta Geoscientica Sinica, 44(3): 511-521. doi: 10.3975/cagsb.2022.053101

江西九江中更新世红土物质来源研究

  • 基金项目:

    本文由国家自然科学基金项目(编号: 41972212)、湖北省楚天学者人才项目(编号: 8210403)和土木工程防灾减灾湖北省引智创新示范基地(编号: 2021EJD026)联合资助

详细信息
    作者简介: 林旭, 男, 1984年生。博士, 副教授, 博士生导师。主要从事青藏高原隆升、中国大河起源和黄土物源研究。通讯地址: 443002, 湖北省宜昌市西陵区三峡大学。E-mail: hanwuji-life@163.com
  • 中图分类号: P534.631; P597.3

Provenance Tracing of Middle Pleistocene Red Earth in the Jiujiang Area, Jiangxi Province

  • 华南地区广泛分布中更新世红土。目前, 对其物质来源尚有争议。九江红土剖面的沉积时代已得到很好限定, 同时由于其沉积连续、地层出露较好, 是开展中更新世红土物质来源研究的理想剖面。通过对九江中更新世红土2件碎屑锆石样品的分析, 共获得177颗谐和锆石U-Pb年龄, 主要峰值集中在新元古代(816 Ma、801 Ma和991 Ma)、古元古代(2019 Ma、2022 Ma和2481 Ma)和新太古代(2502 Ma), 并具有不显著的中生代峰值(135 Ma)。将其与潜在远源和近源物源区的锆石U-Pb年龄组成进行对比, 结果发现中国北方戈壁、沙漠和黄土高原、塔里木盆地、华北平原并不是九江中更新世红土的主要源区。庐山北麓早更新世发育的洪积扇为九江中更新世红土发育提供了充足物质。九江中更新世红土和九江晚更新世黄土的碎屑锆石U-Pb年龄组成存在明显差别, 后者主要来自长江河漫滩的碎屑物质。不同的气候条件主导了九江地区红土和黄土的发育, 二者都受控于青藏高原构造隆升产生的环境变化。
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出版历程
收稿日期:  2022-04-22
修回日期:  2022-05-25

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