哈尔滨地区罗家窝棚组地层的沉积学、矿物学及地球化学特征:对沉积环境的指示

魏春艳, 谢远云, 康春国, 迟云平, 孙磊, 吴鹏, 魏振宇, 冷宇坤. 2022. 哈尔滨地区罗家窝棚组地层的沉积学、矿物学及地球化学特征:对沉积环境的指示. 地质科学, 57(1): 172-189. doi: 10.12017/dzkx.2022.011
引用本文: 魏春艳, 谢远云, 康春国, 迟云平, 孙磊, 吴鹏, 魏振宇, 冷宇坤. 2022. 哈尔滨地区罗家窝棚组地层的沉积学、矿物学及地球化学特征:对沉积环境的指示. 地质科学, 57(1): 172-189. doi: 10.12017/dzkx.2022.011
Wei Chunyan, Xie Yuanyun, Kang Chunguo, Chi Yunping, Sun Lei, Wu Peng, Wei Zhenyu, Leng Yukun. 2022. Sedimentological, mineralogical, and geochemical characteristics of the Luojiawopeng Fm. in Harbin: Implications for the sedimentary environment. Chinese Journal of Geology, 57(1): 172-189. doi: 10.12017/dzkx.2022.011
Citation: Wei Chunyan, Xie Yuanyun, Kang Chunguo, Chi Yunping, Sun Lei, Wu Peng, Wei Zhenyu, Leng Yukun. 2022. Sedimentological, mineralogical, and geochemical characteristics of the Luojiawopeng Fm. in Harbin: Implications for the sedimentary environment. Chinese Journal of Geology, 57(1): 172-189. doi: 10.12017/dzkx.2022.011

哈尔滨地区罗家窝棚组地层的沉积学、矿物学及地球化学特征:对沉积环境的指示

  • 基金项目:

    国家自然科学基金项目(编号:42171006,41871013)和黑龙江省自然科学基金项目(编号:LH2020D009)资助。

详细信息
    作者简介:

    魏春艳,女,1999年生,硕士研究生,第四纪地质学专业。E-mail:1359473230@qq.com

    通讯作者: 谢远云,男,1971年生,博士,教授,第四纪地质学专业。本文通讯作者。E-mail:xyy0451@hrbnu.edu.cn
  • 中图分类号: P588.21;P594

Sedimentological, mineralogical, and geochemical characteristics of the Luojiawopeng Fm. in Harbin: Implications for the sedimentary environment

More Information
  • 罗家窝棚组是哈尔滨地区的第四纪下限地层,其岩性是紫红色砂砾石,被认为是冰碛物堆积。早期的区测资料对其进行了岩性描述,对于其它地层属性,特别是地球化学属性的认识尚未涉及。为此,本文选择黑龙江五常拉林镇罗家窝棚村层型剖面作为研究对象,首次对其沉积学、矿物学、元素地球化学展开综合研究,以揭示其沉积过程和沉积环境。结果表明,这套砾石分选和磨圆较差,风化程度很高,无定向性排列,砾石成分以陆源碎屑岩(砂岩和粉砂岩,44.2%)和花岗岩(37.4%)为主,其次为凝灰岩(11.2%),石英质、闪长岩、流纹岩和玄武岩等少量出现。重矿物组成以赤/褐铁矿占绝对优势(87.5%),其次是白钛石(5.0%),其它重矿物含量较少。元素地球化学揭示,罗家窝棚组中的细颗粒碎屑以及泥质基质经历了很强的化学风化过程,是初次循环的结果。砾石岩性和地球化学组成共同揭示了这些碎屑主要来源于长英质母岩,但中性和铁镁质母岩也有少量贡献。综合沉积学、矿物学和地球化学地层属性,本文认为罗家窝棚组地层是在炎热气候条件下的洪积物堆积,而非寒冷气候条件下的冰碛物。这项研究对于哈尔滨地区第四纪地层的划分和早更新世构造—地貌—气候—水系演化等地质事件的重建具有重要意义。
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收稿日期:  2021-07-06
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