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    南黄海盆地地层生热率及岩石圈热结构

    孙旭东 郭兴伟 张训华 李子渊 刘怀山 张升升

    孙旭东, 郭兴伟, 张训华, 李子渊, 刘怀山, 张升升, 2023. 南黄海盆地地层生热率及岩石圈热结构. 地球科学, 48(3): 1040-1057. doi: 10.3799/dqkx.2023.044
    引用本文: 孙旭东, 郭兴伟, 张训华, 李子渊, 刘怀山, 张升升, 2023. 南黄海盆地地层生热率及岩石圈热结构. 地球科学, 48(3): 1040-1057. doi: 10.3799/dqkx.2023.044
    Sun Xudong, Guo Xingwei, Zhang Xunhua, Li Ziyuan, Liu Huaishan, Zhang Shengsheng, 2023. Radiogenic Heat Production of Formation and Thermal Structure of Lithosphere in the South Yellow Sea Basin. Earth Science, 48(3): 1040-1057. doi: 10.3799/dqkx.2023.044
    Citation: Sun Xudong, Guo Xingwei, Zhang Xunhua, Li Ziyuan, Liu Huaishan, Zhang Shengsheng, 2023. Radiogenic Heat Production of Formation and Thermal Structure of Lithosphere in the South Yellow Sea Basin. Earth Science, 48(3): 1040-1057. doi: 10.3799/dqkx.2023.044

    南黄海盆地地层生热率及岩石圈热结构

    doi: 10.3799/dqkx.2023.044
    基金项目: 

    国家自然科学基金项目 41776081

    国家自然科学基金项目 91958210

    详细信息
      作者简介:

      孙旭东(1994—),男,在读博士研究生,从事海洋构造地质及地球动力学方面的研究. ORCID:0000-0002-6307-2170. E-mail:Sunxudong_work@163.com

      通讯作者:

      郭兴伟,E-mail:xwguo_qd@126.com

    • 中图分类号: P314

    Radiogenic Heat Production of Formation and Thermal Structure of Lithosphere in the South Yellow Sea Basin

    • 摘要: 岩石圈热结构的研究不仅可以了解岩石圈深部动力学演化机制,也是含油气区油气资源评价的重要组成部分.由于南黄海盆地生热率数据的匮乏,阻碍了岩石圈热结构的研究进展.本文通过GR(伽马值)-A(岩石生热率)的经验关系,计算了南黄海盆地沉积地层的生热率;在大地热流、地层生热率、南北向贯穿盆地的二维多道地震剖面及OBS2013地壳速度结构剖面的约束下,建立了南黄海盆地地壳生热模型,计算了盆地的岩石圈热结构.岩石圈热结构计算结果表明:(1)南黄海盆地北部坳陷、中部隆起及南部坳陷3个次级单元的平均莫霍面温度依次为602.2±15.25 ℃、592.7±2.56 ℃、650.6±20.24 ℃;(2)平均热岩石圈厚度依次为99.7±2.20 km、101.7±0.51 km、88.2±2.49 km;(3)壳幔热流比分别为0.76±0.02、0.88±0.01、0.71±0.15,具有“冷壳热幔”的特征.研究结果表明,南黄海盆地现今具有与全球新生代拉张构造区相似的较高热流,处于构造活动区向构造稳定区转换的过渡阶段.此外,现今南黄海盆地3个次级单元展现的不同岩石圈热结构特征,可能与印支期至早燕山期扬子块体与华北块体的俯冲碰撞,在苏鲁造山带南侧(现今北部坳陷的位置)形成类前陆盆地的构造背景有关.

       

    • 图  1  南黄海及周边主要构造单元简图

      0BS2013测线据Zhao et al.(2019);AA’BB’两条二维多道地震测线据张训华等(2017);主要构造区块、钻井及断层据侯方辉等(2019)、Wang et al.(2020

      Fig.  1.  Schematic diagram of main structural units in and around the South Yellow Sea

      图  2  南黄海盆地2条综合解释剖面及OBS2013速度地壳模型

      剖面位置见图 1,据张训华等(2013)、Zhao et al.(2019)修改

      Fig.  2.  Two comprehensive interpretation sections in the South Yellow Sea basin

      图  3  南黄海盆地13口钻井的自然伽马曲线

      Fig.  3.  Natural gamma curves of 13 wells in the South Yellow Sea basin

      图  4  南黄海地区地层生热率样本采集堆积柱状图

      Fig.  4.  Stacked histogram of formation radiogenic heat production rate in South Yellow Sea area

      图  5  南黄海地区地层生热率折线和标准偏差

      Fig.  5.  Line chart and standard deviation of radiogenic heat production rate in South Yellow Sea area

      图  6  CSDP-2井U、Th、K计算的生热率与GR计算的生热率比较(a)及二者相关性分析(b)

      Fig.  6.  Comparison of heat generation rates calculated by U, Th and K and GR in CSDP-2 Well (a) and theirs correlation analysis (b)

      图  7  南黄海盆地现今温度温度剖面(BB’

      Fig.  7.  Current temperature profile of the South Yellow Sea basin (BB')

      图  8  南黄海盆地北部坳陷、中部隆起及南部坳陷岩石圈温度-深度剖面

      Fig.  8.  Lithospheric temperature depth-profiles of northern depression, central uplift and southern depression in the South Yellow Sea basin

      图  9  南黄海盆地北部坳陷与南部坳陷热流演化史

      杨树春等(2003)庞玉茂等(2017)李志强等(2022)修改

      Fig.  9.  Thermal evolution history of northern and southern depressions in the South Yellow Sea basin

      表  1  南黄海盆地地层生热率及样本数

      Table  1.   Radiogenic heat production and sample number of formation in the South Yellow Sea basin

      地层 数目 生热率(μW/m3 地层 数目 生热率(μW/m3
      范围 均值±标准偏差 范围 均值±标准偏差
      东台群 1 362 0.10~2.63 0.85±0.43 孤峰组 26 0.37~4.61 1.69±1.19
      上盐城组 1 783 0.42~2.31 1.32±0.44 栖霞组 278 0.80~4.69 1.96±0.50
      下盐城组 2 199 0.36~3.19 1.28±0.49 船山组 162 0.17~2.14 0.58±0.31
      三垛组 1 501 0.36~2.32 1.23±0.37 黄龙组 248 0.17~1.62 0.63±0.27
      戴南组 1 446 0.52~2.60 1.32±0.49 和州组 228 0.10~1.38 0.52±0.21
      阜宁组 2 226 0.18~2.71 1.14±0.37 高骊山组 109 0.33~2.40 1.48±0.35
      泰州组 1 053 0.29~2.36 1.26±0.42 五通群 121 0.51~3.79 2.06±0.73
      赤山组 848 0.31~1.92 1.11±0.32 茅山组 83 0.85~3.35 2.14±0.68
      浦口组 785 0.27~1.38 0.69±0.33 坟头组 107 0.47~3.72 2.46±0.82
      青龙组 1 646 0.60~2.21 1.22±0.52 侯家塘组 66 0.47~3.72 1.74±0.86
      大隆组 206 0.16~2.28 0.85±0.44 高家边组 50 0.73~3.34 2.65±0.57
      龙潭组 724 0.15~4.53 1.70±1.03 - - - -
      下载: 导出CSV

      表  2  南黄海盆地大地热流

      Table  2.   Heat flow in South Yellow Sea basin

      位置 井号 经度 纬度 热流(mW/m2 均值±标准差(mW/m2 数据来源
      北部坳陷 Inga-1 124.95° 35.40° 61.0 63.5±3.5 Lim and Kim,1997
      Kachi-1 123.35° 35.31° 66.0
      中部隆起 CSDP-2 121.26° 34.56° 66.7 66.7 郭兴伟等,2023
      南部坳陷 FN23-1-1 120.78° 33.45° 68.0 67.9±2.65 杨树春等,2003
      CZ24-1-1 121.96° 33.50° 65.5
      WX20ST1 122.17° 33.49° 67.0
      WX-13-3-1 122.12° 33.63° 65.3
      CZ12-1-1A 121.94° 33.82° 73.6
      CZ6-1-1A 121.92° 33.92° 66.7
      WX5T1 122.79° 33.94° 69.3
      勿南沙隆起 CZ35-2-1 121.68° 33.09° 70.4 70.4 杨树春等,2003
      下载: 导出CSV

      表  3  南黄海盆地地层生热率及热导率

      Table  3.   Radiogenic heat generation and thermal conductivity of Formation in the South Yellow Sea basin

      时代 生热率(μW/m3 热导率(W/(m·K))
      范围 数目 均值±标准差 范围 数目 均值±标准差
      Q 0.10~2.63 1 362 0.85±0.43 1.49~2.19 17 1.85±0.24
      N 0.36~3.19 3 982 1.30±0.47 1.19~2.75 39 1.74±0.40
      E 0.36~2.71 5 173 1.22±0.41 - 30 2.18
      K 0.29~2.36 2 686 1.05±0.43 - 17 2.42
      J - 5 1.02 - 5 2.37
      T 0.60~2.21 1 646 1.22±0.52 2.23~3.55 24 3.00±0.33
      P 0.16~4.69 1 234 1.62±0.93 1.89~5.11 97 3.28±0.68
      C 0.10~2.40 747 0.71±0.42 2.89~6.67 32 3.64±0.84
      D 0.15~3.79 121 2.06±0.73 1.98~6.60 17 4.57±1.59
      S 0.28~2.37 17 1.50±0.59 2.20~6.82 71 3.23±1.23
      O 0.10~0.62 28 0.28±0.16 - 22 3.43
      0.05~6.63 40 0.92±1.60 - 14 4.51
      注:地层生热率:Q-K、T-D来源于本文计算;J来源于庞玉茂等(2017);S-∈来源于野外露头样品(测量结果详见附件1);地层热导率:Q-N、T-S来源于郭兴伟等(2023);E来源于陈沪生等(1999);K-J来源于庞玉茂等(2017);O来源于陈沪生等(1999)、Wang et al.2020);∈来源于王良书等(1995)、Wang et al.2020).
      下载: 导出CSV

      表  4  南黄海盆地地壳结构及其热物性参数

      Table  4.   Crustal structure and thermal properties of the South Yellow Sea basin

      层位 生热率(μW/m3 来源 热导率(W/(m·K)) 来源
      Q+N 1.18 本文计算 1.77 郭兴伟等,2023
      E 1.22 本文计算 2.18 陈沪生等,1999
      J+K 1.05 本文计算 2.41 庞玉茂等,2017
      T 1.22 本文计算 3.00 郭兴伟等,2023
      D-P 1.32 本文计算 3.51 郭兴伟等,2023
      ∈-S 0.83 陆区下扬子采样测试计算 3.44 郭兴伟等,2023
      上地壳 1.43 据P波速度估算 3.00 Xia et al., 2020
      中地壳 0.95 据P波速度估算 2.60 Ray et al., 2003
      下地壳 0.47 据P波速度估算 2.50 Ray et al., 2003
      上地幔 0.02 据P波速度估算 3.40 邱楠生等,2015
      下载: 导出CSV

      表  5  南黄海盆地岩石圈热结构

      Table  5.   Lithospheric thermal structure in the South Yellow Sea basin

      位置 莫霍面温度(℃) 热岩石圈厚度(km) 地壳热流(mW/m2 地幔热流(mW/m2 壳幔热流比
      北部坳陷 北凹1 621.0 96.4 26.8 36.7 0.73
      北凸1 587.6 101.9 27.9 35.6 0.78
      北凹2 614.2 97.9 27.3 36.2 0.75
      北凸2 603.6 100.3 27.9 35.6 0.78
      北凹3 584.8 101.9 27.2 36.3 0.75
      均值 602.2±14.25 99.7±2.20 27.4±0.43 36.1±0.43 0.76±0.02
      中部隆起 中1 594.8 101.2 31.2 35.5 0.88
      中2 590.8 101.5 31.1 35.6 0.87
      中3 589.0 102.4 31.4 35.3 0.89
      中4 593.1 102.2 31.6 35.1 0.90
      中5 596.0 101.2 31.2 35.5 0.88
      均值 592.7±2.56 101.7±0.51 31.3±0.18 35.4±0.18 0.88±0.01
      南部坳陷 南凹1 647.3 88.2 27.8 40.1 0.69
      南凸1 626.3 91.5 28.7 39.2 0.73
      南凹2 673.8 85.8 27.8 40.1 0.69
      南凸2 631.7 90.4 28.3 39.5 0.72
      南凹3 674.1 85.1 28.2 39.7 0.71
      均值 650.6±20.24 88.2±2.49 28.2±0.34 39.7±0.34 0.71±0.01
      下载: 导出CSV
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    • 收稿日期:  2022-04-30
    • 网络出版日期:  2023-03-27
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