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    南黄海中部隆起晚白垩世以来地层剥蚀的磷灰石裂变径迹分析

    庞玉茂 郭兴伟 韩作振 张训华 朱晓青

    庞玉茂, 郭兴伟, 韩作振, 张训华, 朱晓青, 2018. 南黄海中部隆起晚白垩世以来地层剥蚀的磷灰石裂变径迹分析. 地球科学, 43(6): 1921-1930. doi: 10.3799/dqkx.2018.602
    引用本文: 庞玉茂, 郭兴伟, 韩作振, 张训华, 朱晓青, 2018. 南黄海中部隆起晚白垩世以来地层剥蚀的磷灰石裂变径迹分析. 地球科学, 43(6): 1921-1930. doi: 10.3799/dqkx.2018.602
    Pang Yumao, Guo Xingwei, Han Zuozhen, Zhang Xunhua, Zhu Xiaoqing, 2018. Apatite Fission Track Constrains on Denudation since Late Cretaceous in Central Uplift, South Yellow Sea Basin. Earth Science, 43(6): 1921-1930. doi: 10.3799/dqkx.2018.602
    Citation: Pang Yumao, Guo Xingwei, Han Zuozhen, Zhang Xunhua, Zhu Xiaoqing, 2018. Apatite Fission Track Constrains on Denudation since Late Cretaceous in Central Uplift, South Yellow Sea Basin. Earth Science, 43(6): 1921-1930. doi: 10.3799/dqkx.2018.602

    南黄海中部隆起晚白垩世以来地层剥蚀的磷灰石裂变径迹分析

    doi: 10.3799/dqkx.2018.602
    基金项目: 

    国家自然基金项目 41372108

    中国博士后科学基金资助项目 No.2017M620290

    国家海洋地质专项 No.DD20160147

    山东省自然科学基金资助项目 No.ZR2018BD026

    国家自然基金项目 41402182

    全国地质调查项目 No.121201102000150009

    国家自然基金项目 Nos.41776081

    山东科技大学科研创新团队支持计划项目 No.2015TDJH101

    详细信息
      作者简介:

      庞玉茂(1987-), 男, 博士, 主要从事海洋地质、构造地质及石油地质研究

      通讯作者:

      郭兴伟

    • 中图分类号: P618

    Apatite Fission Track Constrains on Denudation since Late Cretaceous in Central Uplift, South Yellow Sea Basin

    • 摘要: 南黄海中部隆起自印支期以来经历显著的构造隆升及剥蚀过程.基于大陆架科学钻探CSDP-2井的钻井岩心,应用磷灰石裂变径迹技术研究了南黄海中部隆起晚白垩世以来的剥蚀过程及响应特征.所获得的8个磷灰石样品的裂变径迹年龄显示出两个年龄组,除单个样品为38±3 Ma外,其余样品都集中在(52±4)~(65±5)Ma范围内,基本反映了同一期构造热事件年龄,并且均远小于样品所处的二叠纪年龄,表明样品完全退火并记录了晚白垩世以来的热历史.样品热史模拟结果表明,基于泥岩镜质体反射率计算的最高古地温处于样品退火带温区范围内,各样品从晚白垩世早期(约100 Ma)以来经历持续的降温过程,在约80~75 Ma开始进入部分退火带.南黄海中部隆起第一期快速冷却降温过程出现在晚白垩世末期,并持续至古新世早期,随后进入古近纪表现为持续相对缓慢的降温过程,降温幅度约30 ℃,渐新世末期到中新世早期存在另一期快速冷却过程.热史模拟结果较好地指示了南黄海中部隆起晚白垩世以来的地层剥蚀响应特征.

       

    • 图  1  南黄海盆地构造纲要图及中部隆起位置

      Fig.  1.  Tectonic outline map of South Yellow Sea basin and the location of the central uplift

      图  2  南黄海中部隆起典型地震剖面及CSDP-2井钻探揭示地层

      剖面位置见图 1

      Fig.  2.  Seismic profile through CSDP-2 well in the central uplift of South Yellow Sea and the stratigraphic framework revealed by the CSDP-2 well

      图  3  磷灰石样品裂变径迹单颗粒年龄直方图及频率曲线

      Fig.  3.  Histograms of apatite single grain ages for each sample and their frequency curves

      图  4  磷灰石样品裂变径迹长度分布直方图

      Fig.  4.  Distribution histograms of apatite fission track lengths

      图  5  磷灰石裂变径迹年龄分布直方图

      Fig.  5.  Distribution histogram of apatite fission track ages

      图  6  样品CSDP-2-1及CSDP-2-8样品裂变径迹热史模拟结果

      Fig.  6.  Modeling results of thermal history from apatite fission track data of sample CSDP-2-1 and sample CSDP-2-8

      表  1  磷灰石裂变径迹测试结果

      Table  1.   Analytical results of apatite fission track

      原样号 垂深(m) 颗粒数 ρs(105/cm2)(Ns) ρi(105/cm2)(Ni) ρd(105/cm2)(Nd) P(χ2)(%) 中心年龄t(Ma)(±1σ) L(μm)(N)
      CSDP-2-1 1 305.8 35 3.808(752) 19.095(3 771) 14.587(7 124) 89.4 59(±4) 12.9±1.7(101)
      CSDP-2-2 1 306.6 35 1.711(394) 13.091(3 015) 14.168(7 124) 96.6 38(±3) 12.8±2.1(99)
      CSDP-2-3 1 311.7 35 4.224(546) 21.978(2 841) 13.541(7 124) 82.2 52(±4) 13.2±1.7(103)
      CSDP-2-4 1 342.6 35 3.716(721) 18.248(3 541) 12.676(7 124) 27.8 52(±4) 13.0±1.9(111)
      CSDP-2-5 1 358.8 36 5.442(306) 20.897(1 175) 12.075(7 124) 80.2 65(±5) 12.5±1.9(53)
      CSDP-2-6 1 379.9 34 2.927(261) 15.018(1339) 16.472(7 124) 84.1 64(±6) 12.7±1.6(96)
      CSDP-2-7 1 431.2 35 4.347(682) 25.063(3 932) 15.843(7 124) 94.3 56(±3) 12.5±1.9(103)
      CSDP-2-8 1 437.6 35 4.327(618) 21.333(3 047) 15.424(7 124) 83.4 64(±4) 12.9±1.4(102)
      注:ρs为自发径迹密度;ρi为诱发径迹密度;ρd为标准径迹密度;Ns为自发径迹数;Ni为诱发径迹数;Nd为标准径迹数;N为径迹长度数.
      下载: 导出CSV
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