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南黄海北部晚更新世以来常量元素记录的化学风化作用

梅西 张训华 李日辉 蓝先洪

梅西, 张训华, 李日辉, 蓝先洪. 南黄海北部晚更新世以来常量元素记录的化学风化作用[J]. 沉积学报, 2014, 32(5): 846-854.
引用本文: 梅西, 张训华, 李日辉, 蓝先洪. 南黄海北部晚更新世以来常量元素记录的化学风化作用[J]. 沉积学报, 2014, 32(5): 846-854.
MEI Xi, ZHANG Xun-hua, LI Ri-hui, LAN Xian-hong. Chemical Weathering Recorded by Major Element of Northern South Yellow Sea since Late Pleistocene[J]. Acta Sedimentologica Sinica, 2014, 32(5): 846-854.
Citation: MEI Xi, ZHANG Xun-hua, LI Ri-hui, LAN Xian-hong. Chemical Weathering Recorded by Major Element of Northern South Yellow Sea since Late Pleistocene[J]. Acta Sedimentologica Sinica, 2014, 32(5): 846-854.

南黄海北部晚更新世以来常量元素记录的化学风化作用

基金项目: 国土资源部海洋地质调查专项(编号:GZH200800501,GZH201100202、1212011220113)、自然科学基金(41206051)与国土资源部海洋油气与环境地质重点实验室开放式基金(编号:MRE201227)联合资助
详细信息
    通讯作者:

    张训华 男 研究员 E-mail:xunhuazh@vip.sina.com

  • 中图分类号: P736.2

Chemical Weathering Recorded by Major Element of Northern South Yellow Sea since Late Pleistocene

  • 摘要: 以南黄海北部高沉积速率柱状样DLC70-3孔作为研究对象,对沉积物的黏土矿物和常量元素地球化学组成进行了综合分析。结果显示,DLC70-3孔沉积物中黏土矿物组合以伊利石为主,其次为蒙皂石,绿泥石和高岭石含量较低;绝大部分样品中伊利石与蒙皂石含量的比值<6,表明沉积物主要来源于黄河物质的输送。研究认为DLC70-3孔沉积物的化学风化指标CIA值受到海平面变化和源区气候变化共同控制,其中源区的气候变化为主要控制因素,而海平面变化造成的机械沉积分异作用主要影响27.80~38.00 m(MIS 4)层位沉积物的CIA值。CIA值显示在MIS 5和MIS 3期大陆化学风化作用较强,与内陆黄土高原地区夏季风和化学风化指标的变化趋势一致,尤其是在MIS 3早期(40~60 ka)记录的化学风化作用非常强,反映了黄河流域地区出现强夏季风降雨过程。
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目录

    南黄海北部晚更新世以来常量元素记录的化学风化作用

      基金项目:  国土资源部海洋地质调查专项(编号:GZH200800501,GZH201100202、1212011220113)、自然科学基金(41206051)与国土资源部海洋油气与环境地质重点实验室开放式基金(编号:MRE201227)联合资助
      通讯作者: 张训华 男 研究员 E-mail:xunhuazh@vip.sina.com
    • 中图分类号: P736.2

    摘要: 以南黄海北部高沉积速率柱状样DLC70-3孔作为研究对象,对沉积物的黏土矿物和常量元素地球化学组成进行了综合分析。结果显示,DLC70-3孔沉积物中黏土矿物组合以伊利石为主,其次为蒙皂石,绿泥石和高岭石含量较低;绝大部分样品中伊利石与蒙皂石含量的比值<6,表明沉积物主要来源于黄河物质的输送。研究认为DLC70-3孔沉积物的化学风化指标CIA值受到海平面变化和源区气候变化共同控制,其中源区的气候变化为主要控制因素,而海平面变化造成的机械沉积分异作用主要影响27.80~38.00 m(MIS 4)层位沉积物的CIA值。CIA值显示在MIS 5和MIS 3期大陆化学风化作用较强,与内陆黄土高原地区夏季风和化学风化指标的变化趋势一致,尤其是在MIS 3早期(40~60 ka)记录的化学风化作用非常强,反映了黄河流域地区出现强夏季风降雨过程。

    English Abstract

    梅西, 张训华, 李日辉, 蓝先洪. 南黄海北部晚更新世以来常量元素记录的化学风化作用[J]. 沉积学报, 2014, 32(5): 846-854.
    引用本文: 梅西, 张训华, 李日辉, 蓝先洪. 南黄海北部晚更新世以来常量元素记录的化学风化作用[J]. 沉积学报, 2014, 32(5): 846-854.
    MEI Xi, ZHANG Xun-hua, LI Ri-hui, LAN Xian-hong. Chemical Weathering Recorded by Major Element of Northern South Yellow Sea since Late Pleistocene[J]. Acta Sedimentologica Sinica, 2014, 32(5): 846-854.
    Citation: MEI Xi, ZHANG Xun-hua, LI Ri-hui, LAN Xian-hong. Chemical Weathering Recorded by Major Element of Northern South Yellow Sea since Late Pleistocene[J]. Acta Sedimentologica Sinica, 2014, 32(5): 846-854.
    参考文献 (41)

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