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    中国大陆科学钻探主孔正片麻岩磁性及深部流体活动

    曾庆理 刘庆生 郑建平 刘志峰 王红才

    曾庆理, 刘庆生, 郑建平, 刘志峰, 王红才, 2014. 中国大陆科学钻探主孔正片麻岩磁性及深部流体活动. 地球科学, 39(12): 1915-1926. doi: 10.3799/dqkx.2014.176
    引用本文: 曾庆理, 刘庆生, 郑建平, 刘志峰, 王红才, 2014. 中国大陆科学钻探主孔正片麻岩磁性及深部流体活动. 地球科学, 39(12): 1915-1926. doi: 10.3799/dqkx.2014.176
    Zeng Qingli, Liu Qingsheng, Zheng Jianping, Liu Zhifeng, Wang Hongcai, 2014. Magnetism of Granitic Gneiss from Chinese Continental Scientific Drilling Main Hole and Fluid Activities. Earth Science, 39(12): 1915-1926. doi: 10.3799/dqkx.2014.176
    Citation: Zeng Qingli, Liu Qingsheng, Zheng Jianping, Liu Zhifeng, Wang Hongcai, 2014. Magnetism of Granitic Gneiss from Chinese Continental Scientific Drilling Main Hole and Fluid Activities. Earth Science, 39(12): 1915-1926. doi: 10.3799/dqkx.2014.176

    中国大陆科学钻探主孔正片麻岩磁性及深部流体活动

    doi: 10.3799/dqkx.2014.176
    基金项目: 

    "973"项目 2012CB416604

    国家自然科学基金 41139315

    国家自然科学基金 91214204

    国家自然科学基金 41374094

    中国博士后科学基金面上资助 2013M542084

    国家自然科学基金青年基金 41304050

    详细信息
      作者简介:

      曾庆理(1984-), 男, 博士后, 主要从事深部岩石磁性及岩石地球物理性质研究.E-mail: Zengqingli@gmail.com

    • 中图分类号: P318.4

    Magnetism of Granitic Gneiss from Chinese Continental Scientific Drilling Main Hole and Fluid Activities

    • 摘要: 通过对中国大陆科学钻探工程主孔花岗质片麻岩进行详细的岩石磁学研究及岩石矿物学分析表明: 花岗质片麻岩磁化率(0.570×10-7~120.450×10-7m3·kg-1, 平均29.996×10-7m3·kg-1)在主孔所有岩石中仅次于蛇纹石化石榴石橄榄岩, 而其天然剩余磁化强度(0.002×10-3~2.109×10-3Am2·kg-1, 平均0.210×10-3Am2·kg-1)则是所有岩性中最低的.磁化率随温度变化曲线、交变退磁曲线及磁滞回线特征表明, 花岗质片麻岩中磁性矿物组合主要成分为磁铁矿, 小部分样品中含有赤铁矿, 其中磁铁矿以多畴为主, 伪单畴磁铁矿仅在少量样品中出现.和同为完全退变质岩的角闪岩(完全退变质榴辉岩)相比, 花岗质片麻岩具有相似的磁性矿物组合, 但其磁铁矿的颗粒明显较大.多畴磁铁矿的形成, 可能和超高压变质岩折返过程中, 花岗质片麻岩较强的流体活动相关.部分分布于花岗质片麻岩主体岩性段外的样品, 具有较高的天然剩余磁化强度, 则可能反映了花岗质片麻岩及周围榴辉岩之间的流体交换.

       

    • 图  1  CCSD主孔位置及采样点位(Xu et al., 2009b)

      TLF.郯庐断裂;JXF.嘉山-响水断裂;WQYF.武梁-青岛-烟台断裂

      Fig.  1.  Location map of CCSD main hole with the simplified lithological profile of the depth interval 100-2 000 m and sample location

      图  2  花岗质片麻岩显微照片

      a, b.187和152号样品透射光照片;c, d.样品252反射光照片;e, f.样品278和190反射光照片.Amp.角闪石;Bt.黑云母;Epi.绿帘石;Hem.赤铁矿;Ilm.钛铁矿;Mt.磁铁矿;Opaque.不透明矿物;Pl.斜长石;Py.辉石;Pyr.黄铁矿;Q.石英;Spn.榍石

      Fig.  2.  Microscopy photo of granitic gneiss under transmitted and reflected light

      图  3  代表性样品中不透明矿物显微激光拉曼光谱分析

      a.黄铁矿; b.具赤铁矿反应边的磁铁矿; c.和绿帘石共生的拉长型磁铁矿; d.赤铁矿-钛铁矿颗粒

      Fig.  3.  Micro Raman spectrum of typical opaque mineral of the granitic gneiss

      图  4  代表性样品的典型磁滞回线(顺磁性校正后)

      Fig.  4.  Typical hysteresis curves (after paramagnetic slope correction) of selected samples

      图  5  代表性样品的热磁曲线特征(升降温曲线如箭头所示)

      a.229号; b.230号; c.259号; d.266号; e.278号

      Fig.  5.  χ-T curves for representative samples

      图  6  花岗质片麻岩代表性样品交变退磁(AF demagnetization)曲线

      Fig.  6.  AF demagnetization curves of typical samples

      图  7  正片麻岩Mrs/χ v.s. Bcr交会图(Perters and Dekkers, 2003)

      Fig.  7.  Mrs/χ vs Bcr plot of granitic gneiss

      图  8  片麻岩样品Day氏图(Dunlop, 2002)

      Fig.  8.  Day-plot of gneiss samples

      图  9  CCSD主孔100~2 000 m花岗质片麻岩样品NRM-χ交会

      Fig.  9.  NRM-χ plot for granitic gneiss in CCSD MH 100-2 000 m

      表  1  花岗质片麻岩样品密度、磁化率及天然剩余磁化强度统计

      Table  1.   The summary of density, susceptibility and NRM of granitic gneiss

      类别 ρ (g·cm-3) χ(10-7 m3·kg-1) NRM(10-3 Am2·kg-1) Q
      全体样品 范围 2.581~2.878 0.570~120.450 0.002~2.109 0.100~28.590
      全体样品 Mean±SD 2.649±0.039 29.996±32.418 0.210±0.444 2.562±5.548
      主体岩性段 范围 2.606~2.878 0.570~120.450 0.003~1.142 0.100~20.310
      内样品 Mean±SD 2.645±0.040 22.988±25.478 0.098±0.252 1.573±3.582
      主体岩性段 范围 2.581~2.693 0.590~115.240 0.002~2.109 0.150~28.590
      外样品 Mean±SD 2.653±0.030 49.682±40.581 0.504±0.663 5.197±8.452
      下载: 导出CSV

      表  2  代表性样品磁滞回线参数

      Table  2.   Magnetic hysteresis parameters of selected samples

      编号 深度(m) Mrs(10-3 Am2·kg-1) Ms(10-3 Am2·kg-1) Bc(mT) Bcr(mT) Mrs/χ(kAm-1) Mrs/Ms Bcr/Bc
      187 1 023.30 9.256 4 101.900 0.402 10.3 0.738 0.002 25.622
      204 1 103.10 2.431 302.732 1.080 14.3 2.524 0.008 13.241
      207 1 113.85 3.820 1 326.527 0.515 12.1 0.667 0.003 23.495
      210 1 134.09 10.795 2 914.471 0.594 12.6 1.084 0.004 21.212
      219 1 175.38 5.510 1 201.784 0.747 17.3 1.042 0.005 23.159
      222 1 191.81 0.635 19.326 5.050 66.2 11.437 0.033 13.109
      224 1 200.00 2.125 249.313 1.370 19.4 1.667 0.009 14.161
      227 1 216.50 1.941 8.124 26.600 35.0 27.190 0.239 1.316
      229 1 227.48 1.178 26.673 6.970 92.9 9.567 0.044 13.329
      230 1 242.50 4.843 258.580 2.820 56.3 3.527 0.019 19.965
      239 1 305.17 1.774 282.314 1.140 24.2 1.491 0.006 21.228
      240 1 313.26 0.573 5.487 16.600 196.0 14.111 0.105 11.807
      243 1 343.19 0.805 227.930 0.613 21.3 0.734 0.004 34.747
      249 1 394.38 0.876 165.494 0.916 20.9 1.155 0.005 22.817
      251 1 420.00 2.073 639.551 0.621 17.0 0.829 0.003 27.375
      252 1 422.50 6.375 886.693 1.080 14.4 1.420 0.007 13.333
      255 1 443.50 3.532 997.163 0.700 12.7 0.836 0.004 18.143
      259 1 475.00 5.466 578.362 1.740 16.2 2.672 0.009 9.310
      266 1 514.50 8.757 1 999.339 0.731 14.5 1.004 0.004 19.836
      268 1 523.20 2.716 271.584 1.610 16.2 2.125 0.010 10.062
      274 1 552.65 10.774 310.391 4.820 22.0 6.149 0.035 4.564
      278 1 591.50 18.740 476.798 6.120 27.8 11.053 0.039 4.542
      318 1 843.57 3.910 82.713 9.280 111.0 10.576 0.047 11.961
      注:Mrs.饱和等温剩余磁化强度; Ms.饱和磁化强度; Bc.矫顽力; Bcr.剩磁矫顽力; χ.低场磁化率.
      下载: 导出CSV
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    • 收稿日期:  2014-01-03
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