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    闽西南龙岩地区印支期天宫山花岗岩体成因

    康丛轩 周延 宗雯 范飞鹏 李凤春 孙建东 吕劲松

    康丛轩, 周延, 宗雯, 范飞鹏, 李凤春, 孙建东, 吕劲松, 2018. 闽西南龙岩地区印支期天宫山花岗岩体成因. 地球科学, 43(12): 4621-4637. doi: 10.3799/dqkx.2017.602
    引用本文: 康丛轩, 周延, 宗雯, 范飞鹏, 李凤春, 孙建东, 吕劲松, 2018. 闽西南龙岩地区印支期天宫山花岗岩体成因. 地球科学, 43(12): 4621-4637. doi: 10.3799/dqkx.2017.602
    Kang Congxuan, Zhou Yan, Zong Wen, Fan Feipeng, Li Fengchun, Sun Jiandong, Lü Jinsong, 2018. Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian. Earth Science, 43(12): 4621-4637. doi: 10.3799/dqkx.2017.602
    Citation: Kang Congxuan, Zhou Yan, Zong Wen, Fan Feipeng, Li Fengchun, Sun Jiandong, Lü Jinsong, 2018. Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian. Earth Science, 43(12): 4621-4637. doi: 10.3799/dqkx.2017.602

    闽西南龙岩地区印支期天宫山花岗岩体成因

    doi: 10.3799/dqkx.2017.602
    基金项目: 

    中国地质调查局项目 D20160037

    中国地质调查局项目 12120113071400

    详细信息
      作者简介:

      康丛轩(1985-), 男, 博士研究生, 助理研究员, 主要从事矿物、岩石、矿床学研究

    • 中图分类号: P59

    Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian

    • 摘要: 天宫山花岗岩体成因的研究对闽西南地区岩浆演化及动力学过程有重要意义.天宫山岩体岩性主要为正长花岗岩.前人于天宫山岩体中利用K-Ar法测得年龄值为146~149 Ma,天宫山正长花岗岩中测得锆石LA-ICP-MS U-Pb年龄为233±2.0 Ma、230±2.8 Ma,为晚三叠世,属印支期.该岩体富硅,富碱,σ=1.21~2.55,A/CNK=0.97~1.73,属钙碱性系列,准铝质到过铝质范畴.岩石ΣREE较高,LREE相对富集,贫Al2O3和Sr,富Y和Yb,发育有明显的显微文象结构,具有较强的铕负异常,中等铈负异常到弱正异常;亏损大离子亲石元素,富集高场强元素.Ga/Al值高,具有A型花岗岩特征.w(P2O5)平均值为0.02%,低于高分异S型花岗岩;w(Na2O)平均值为2.93%,高于高分异S型花岗岩;全铁含量w(TFeO)平均值为1.15%,高于高分异I型花岗岩.锆石饱和温度平均值为729.8℃.εHft)全部为负值(-5.29~-10.69),表明其物质起源可能主要为古元古代下地壳物质.参与成岩作用的岩浆来源于地壳物质的部分熔融,为同碰撞环境下形成的壳源型铝质A型花岗岩.在印支期碰撞-挤压为主的造山运动背景下,岩体在高温环境中经历了古元古代下地壳物质的初步熔融,经印支期运动伸展,部分地幔物质参与了经底侵作用.

       

    • 图  1  天宫山岩体区域地质简图及采样位置

      据福建省地质调查研究院, 2005.1:250 000龙岩市幅区域地质调查报告.1.第四纪地层;2.晚三叠-白垩世地层;3.泥盆-三叠世地层;4.早古生代地层;5.侵入岩;6.采样位置及编号;7.断层

      Fig.  1.  Geological sketch and sampling location map of the Tiangongshan pluton

      图  2  天宫山岩体正长花岗岩标本及显微照片

      a.浅肉红色正长花岗岩;b, c.花岗结构,钾长石、斜长石具卡式双晶;d.显微文象结构(花斑结构).Q.石英;Pl.斜长石;Kfs.钾长石;Bt.黑云母

      Fig.  2.  Specimen and microphotographs of the Tiangongshan pluton

      图  3  岩浆岩系统全碱-硅(TAS)分类图解

      Middlemost(1994).Ir.Irvine分界线,上方为碱性,下方为亚碱性

      Fig.  3.  Total alkali silica (TAS) classification of magmatic rock system

      图  4  岩体K2O-SiO2图解(a)及A/CNK-A/NK图解(b)

      a.实线据Peccerillo and Taylor(1976); 虚线据Middlemost(1985).b.底图据Middlemost(1994)

      Fig.  4.  K2O-SiO2 diagram (a) and A/CNK-A/NK diagram (b) of the granites

      图  5  岩体球粒陨石标准化稀土元素配分图(a)及原始地幔标准化微量元素蛛网图(b)

      蛛网标准化数值据Sun and McDonough(1989)

      Fig.  5.  Chondrite-normalized REE distribution patterns (a) and primitive mantle-normalized trace element diagram (b) of the granites

      图  7  天宫山岩体代表性锆石阴极发光图像

      Fig.  7.  Representative zircon cathodoluminescence images of the Tiangongshan pluton

      图  8  天宫山岩体锆石稀土元素球粒陨石标准化分布型式图

      标准化数值据Sun and McDonough(1989)

      Fig.  8.  Zircon chondrite standard curves of REE abundance patterns of the Tiangongshan pluton

      图  6  天宫山岩体锆石U-Pb谐和图和加权平均年龄

      Fig.  6.  U-Pb concordia diagram and weighted average age of the Tiangongshan pluton

      图  10  天宫山岩体锆石Lu-Hf同位素组成和模式年龄统计直方图

      Fig.  10.  Statistical histogram of zircon Lu-Hf isotopic composition and model ages of the Tiangongshan pluton

      图  9  天宫山岩体锆石Hf同位素特征

      Fig.  9.  Zircon Hf isotopic features of the Tiangongshan pluton

      图  11  天宫山岩体成因类型判别图解

      Whalen et al.(1987)

      Fig.  11.  Genetic types of discrimination diagram of the Tiangongshan pluton

      图  12  天宫山岩体A型花岗岩亚类判别图

      底图据Eby(1990, 1992)

      Fig.  12.  A-type granite subclass discrimination diagrams of the Tiangongshan pluton

      图  13  天宫山岩体Y-Nb(a)及Yb-Ta(b)构造环境判别图解

      syn-COLG.同碰撞花岗岩;WPG.板内花岗岩;VAG.火山弧花岗岩;ORG.洋脊花岗岩

      Fig.  13.  Y-Nb (a) and Yb-Ta (b) structural environment discrimination diagrams of the Tiangongshan pluton

      表  1  岩体主量元素组成(%)

      Table  1.   Major element compositions of the granites (%)

      样号 TGS-1 TGS-2 TGS-3 TGS-4 TGS-5 TGS-6 TGS-7
      SiO2 76.16 76.20 75.01 78.20 75.64 75.85 76.20
      TiO2 0.11 0.11 0.06 0.14 0.12 0.12 0.08
      Al2O3 12.77 12.97 12.76 11.93 12.30 11.84 12.12
      Fe2O3 1.23 0.54 0.49 0.44 0.54 0.38 0.41
      FeO 0.27 0.36 0.58 0.57 0.81 1.22 0.92
      MnO 0.07 0.01 0.05 0.03 0.03 0.04 0.03
      MgO 0.21 0.08 0.05 0.27 0.20 0.19 0.15
      CaO 0.22 0.12 0.72 0.22 0.86 0.56 0.81
      Na2O 0.24 1.27 3.83 4.61 3.36 3.79 3.38
      K2O 6.09 5.37 5.20 2.05 4.82 4.74 4.63
      P2O5 0.02 0.01 0.01 0.02 0.02 0.02 0.02
      LOI 2.14 2.47 0.74 1.06 0.86 0.94 0.73
      Total 99.53 99.52 99.50 99.54 99.56 99.69 99.48
      Na2O+K2O 6.33 6.64 9.03 6.66 8.18 8.53 8.01
      K2O/Na2O 25.38 4.23 1.36 0.44 1.43 1.25 1.37
      σ 1.21 1.33 2.55 1.26 2.05 2.21 1.93
      A/CNK 1.73 1.60 0.97 1.17 1.00 0.96 1.01
      A/NK 1.840 1.620 1.070 1.220 1.144 1.040 1.150
      注:TGS-1~TGS-4数据为本文实测,TGS-5~TGS-7测试数据来源于1:25万龙岩市幅区域地质调查报告(福建省地质调查研究院,2005).
      下载: 导出CSV

      表  2  岩体微量元素组成(10-6)

      Table  2.   Trace element compositions of the granites (10-6)

      样号 TGS-1 TGS-2 TGS-3 TGS-4 TGS-5 TGS-6 TGS-7
      Rb 585.00 425.00 547.00 153.00
      Sr 20.50 16.10 12.30 66.50
      Nb 49.30 50.60 59.10 22.80 20.00 30.00 32.00
      Mo 17.10 1.10 0.45 1.08 14.00 5.00 2.00
      Cd 0.16 0.04 0.05 0.05
      Sn 27.60 9.92 14.80 5.24 38.00 22.00 18.00
      Cs 13.50 9.01 11.30 4.97
      Ba 110.00 128.00 16.80 96.10 100.00 120.00 113.00
      Ta 6.47 5.86 10.10 2.83
      W 5.74 3.47 4.33 1.19
      Tl 3.46 2.11 2.62 0.81
      Pb 73.50 49.20 59.80 60.70 44.00 43.00 58.00
      Bi 2.10 0.29 0.19 1.48
      Th 56.20 92.10 74.80 42.90
      U 7.66 10.20 16.60 14.20
      Sc 4.22 3.46 3.21 3.22
      V 7.03 1.53 0.91 10.60 8.00 6.00 9.00
      Cr 5.44 3.98 4.80 5.02 5.00 5.00 5.00
      Co 1.22 1.28 0.39 1.08
      Ni 2.40 3.96 1.66 2.90
      Cu 3.53 2.86 2.58 26.40 2.00 3.00 4.00
      Zn 31.70 56.90 39.70 22.00 24.00 22.00 28.00
      Ga 23.30 21.70 23.30 15.50
      Zr 107.00 157.00 99.10 87.50 56.00 78.00 80.00
      Hf 3.90 5.90 4.80 3.60
      F 941.00 959.00 3 879.00 850.00 800.00 840.00 3340.00
      As 12.90 0.64 0.48 0.57
      Sb 0.23 0.13 0.13 0.09
      Ag 0.15 0.02 0.01 0.88
      注:TGS-1~TGS-4数据为本文实测,TGS-5~TGS-7测试数据来源于1:25万龙岩市幅区域地质调查报告(福建省地质调查研究院,2005),“—”表示未测.
      下载: 导出CSV

      表  3  岩体稀土元素组成(10-6)

      Table  3.   Rare earth element compositions of the granites (10-6)

      样号 TGS-1 TGS-2 TGS-3 TGS-4 TGS-5 TGS-6 TGS-7
      La 60.60 231.00 38.50 45.90 37.52 61.39 46.05
      Ce 62.50 114.00 79.20 79.60 63.50 105.83 50.47
      Pr 18.50 72.90 10.40 7.09 6.67 13.34 8.00
      Nd 65.10 252.00 37.00 21.30 29.49 55.72 31.55
      Sm 16.20 60.10 12.10 3.56 4.14 9.14 4.14
      Eu 0.34 1.40 0.16 0.50 0.59 0.56 0.55
      Gd 12.80 29.60 13.70 2.69 2.08 5.64 1.87
      Tb 1.99 4.11 2.75 0.40 0.71 1.28 0.61
      Dy 11.80 20.30 18.40 2.25 2.06 5.14 1.74
      Ho 2.38 3.28 4.12 0.47 0.65 1.15 0.51
      Er 7.22 9.00 12.30 1.72 1.96 3.87 1.61
      Tm 1.02 1.26 1.93 0.28 0.33 0.57 0.28
      Yb 7.18 8.25 13.00 2.18 2.11 3.78 2.04
      Lu 0.91 1.13 1.92 0.33 0.47 0.74 0.46
      Y 55.10 80.50 130.00 14.60 13.23 24.57 10.39
      ΣREE 317.94 705.33 223.78 218.47 152.28 268.15 149.88
      LREE 272.64 628.40 155.66 208.15 141.91 245.98 140.76
      HREE 45.30 76.93 68.12 10.32 10.37 22.17 9.12
      LREE/HREE 6.02 8.17 2.29 20.17 13.68 11.10 15.43
      LaN/YbN 10.99 11.13 0.93 31.62 12.76 11.65 16.19
      δEu 0.07 0.09 0.04 0.47 0.55 0.22 0.52
      δCe 0.31 0.28 1.44 0.54 0.91 0.87 0.59
      注:TGS-1~TGS-4数据为本文实测,TGS-5~TGS-7测试数据来源于1:25万龙岩市幅区域地质调查报告(福建省地质调查研究院,2005).
      下载: 导出CSV

      表  4  岩体锆石LA-ICP-MS U-Pb测试结果

      Table  4.   Zircon LA-ICP-MS U-Pb data of the granites

      测点号 含量(10-6) Th/U 同位素比值 年龄(Ma)
      Th U 207Pb/206Pb 207Pb/235U 206Pb/238U 207Pb/206Pb 207Pb/235U 207Pb/235U 207Pb/206Pb 207Pb/235U
      T1-1 727 862 0.84 0.051 8 0.001 1 0.262 0 0.006 6 0.036 3 0.000 5 0.010 8 0.000 3 276.0 45.4 236.2 5.3 230.1 3.0 217.3 5.3
      T1-3 162 192 0.84 0.052 3 0.002 1 0.268 3 0.011 0 0.037 3 0.000 6 0.010 4 0.000 3 298.2 88.0 241.4 8.8 236.3 3.6 208.7 6.8
      T1-4 577 941 0.61 0.051 0 0.001 3 0.260 5 0.006 6 0.036 8 0.000 5 0.011 3 0.000 3 242.7 57.4 235.1 5.3 233.3 3.2 227.6 6.1
      T1-5 368 318 1.16 0.055 7 0.002 4 0.278 7 0.011 8 0.036 3 0.000 7 0.009 6 0.000 4 442.6 128.7 249.6 9.3 230.0 4.1 194.1 7.8
      T1-8 160 199 0.81 0.048 6 0.002 0 0.244 6 0.010 2 0.036 8 0.000 7 0.010 9 0.000 5 127.9 93.5 222.2 8.3 232.7 4.2 219.6 9.8
      T1-9 218 287 0.76 0.048 6 0.001 9 0.244 6 0.009 7 0.036 3 0.000 6 0.010 4 0.000 4 127.9 90.7 222.1 8.0 230.1 3.9 209.1 8.2
      T1-10 117 125 0.93 0.047 3 0.002 9 0.237 7 0.014 3 0.037 1 0.000 8 0.011 1 0.000 5 64.9 146.3 216.6 11.7 235.1 4.9 222.9 10.0
      T1-11 602 844 0.71 0.049 6 0.001 3 0.255 5 0.006 5 0.037 1 0.000 5 0.011 3 0.000 3 176.0 59.2 231.0 5.3 235.1 3.1 227.7 7.0
      T1-12 250 321 0.78 0.049 2 0.001 7 0.245 4 0.008 5 0.036 4 0.000 6 0.011 1 0.000 4 166.8 83.3 222.8 6.9 230.6 3.7 223.1 8.1
      T1-13 223 211 1.06 0.045 3 0.002 1 0.222 0 0.010 3 0.035 7 0.000 6 0.011 0 0.000 4 203.6 8.5 225.9 4.0 220.6 8.4
      T1-14 96 133 0.72 0.069 3 0.006 3 0.371 6 0.037 5 0.037 5 0.001 0 0.013 6 0.001 0 905.6 187.0 320.9 27.8 237.5 6.0 272.8 20.3
      T1-15 204 211 0.97 0.055 7 0.002 6 0.281 1 0.013 0 0.036 9 0.000 7 0.012 0 0.000 5 442.6 99.1 251.5 10.3 233.8 4.4 241.5 10.4
      T1-17 78 90 0.86 0.067 6 0.004 6 0.319 3 0.023 4 0.036 8 0.001 0 0.011 5 0.000 6 857.4 141.5 281.4 18.0 233.2 6.1 231.0 12.0
      T1-18 129 154 0.83 0.054 3 0.003 6 0.271 5 0.017 7 0.036 8 0.000 9 0.012 7 0.000 6 383.4 148.1 243.9 14.2 233.2 5.3 255.2 12.7
      T1-19 140 163 0.86 0.049 5 0.002 9 0.251 4 0.014 0 0.037 5 0.000 9 0.012 0 0.000 5 172.3 135.2 227.7 11.4 237.6 5.4 240.4 10.5
      T1-20 286 460 0.62 0.050 7 0.001 9 0.262 1 0.010 0 0.037 3 0.000 7 0.011 5 0.000 5 233.4 54.6 236.4 8.1 236.0 4.6 230.7 9.6
      T3-2 314 509 0.62 0.049 6 0.001 6 0.255 4 0.008 3 0.037 5 0.000 6 0.013 4 0.000 4 176.0 77.8 230.9 6.7 237.2 3.5 268.4 8.1
      T3-3 105 134 0.78 0.047 9 0.002 5 0.229 0 0.011 7 0.035 3 0.000 7 0.012 2 0.000 5 100.1 112.9 209.4 9.7 223.6 4.1 244.2 10.0
      T3-4 157 197 0.80 0.051 7 0.002 3 0.259 3 0.010 3 0.037 2 0.000 6 0.014 4 0.000 5 272.3 101.8 234.1 8.3 235.4 4.0 289.3 10.5
      T3-5 158 173 0.91 0.052 6 0.002 8 0.258 9 0.012 7 0.036 4 0.000 6 0.014 6 0.000 5 309.3 122.2 233.8 10.2 230.4 3.9 292.4 10.5
      T3-6 239 288 0.83 0.051 6 0.002 0 0.262 9 0.010 2 0.037 0 0.000 6 0.015 7 0.000 6 333.4 95.4 237.0 8.2 234.4 3.7 314.8 11.4
      T3-7 274 348 0.79 0.054 7 0.002 1 0.254 5 0.008 5 0.034 2 0.000 5 0.014 7 0.000 6 398.2 80.5 230.2 6.9 216.6 3.3 294.9 11.1
      T3-8 425 646 0.66 0.052 0 0.001 9 0.247 5 0.008 6 0.034 4 0.000 6 0.015 9 0.000 6 287.1 78.7 224.5 7.0 217.8 3.5 318.6 12.4
      T3-9 185 188 0.98 0.050 5 0.002 6 0.249 0 0.011 4 0.037 0 0.000 7 0.018 2 0.000 8 216.7 122.2 225.8 9.3 234.2 4.2 365.0 15.6
      T3-10 432 710 0.61 0.050 8 0.001 5 0.254 0 0.007 5 0.036 3 0.000 6 0.016 2 0.000 6 227.8 66.7 229.8 6.1 230.1 3.4 324.6 12.4
      T3-11 168 147 1.14 0.059 1 0.003 2 0.281 5 0.015 6 0.035 4 0.000 8 0.015 7 0.000 7 572.3 116.7 251.8 12.3 224.4 4.8 315.7 13.5
      T3-12 443 537 0.83 0.053 0 0.001 8 0.269 3 0.010 3 0.036 3 0.000 7 0.015 4 0.000 6 331.5 77.8 242.1 8.3 229.6 4.4 308.5 11.2
      T3-13 106 84 1.26 0.055 2 0.003 4 0.263 9 0.014 5 0.036 6 0.000 9 0.014 3 0.000 6 420.4 140.7 237.8 11.6 232.0 5.5 286.7 11.4
      T3-14 155 153 1.01 0.052 9 0.002 6 0.259 1 0.014 3 0.036 3 0.000 8 0.013 7 0.000 6 324.1 109.2 233.9 11.5 230.0 5.1 275.4 12.0
      T3-15 167 217 0.77 0.053 9 0.002 1 0.274 7 0.010 6 0.037 0 0.000 7 0.013 5 0.000 5 364.9 87.0 246.5 8.5 234.3 4.4 272.0 10.3
      T3-16 132 127 1.04 0.061 9 0.003 2 0.309 2 0.015 5 0.037 3 0.000 8 0.012 3 0.000 5 733.3 104.6 273.5 12.0 236.3 4.9 247.5 9.2
      T3-17 336 422 0.79 0.049 4 0.001 6 0.253 4 0.008 5 0.037 0 0.000 6 0.011 4 0.000 3 168.6 71.3 229.3 6.9 234.0 3.8 229.6 6.7
      T3-19 228 305 0.75 0.054 7 0.002 3 0.273 7 0.011 7 0.036 9 0.000 7 0.011 2 0.000 4 398.2 99.1 245.7 9.3 233.8 4.5 224.9 7.4
      T3-20 151 190 0.80 0.056 5 0.002 3 0.280 3 0.012 1 0.036 1 0.000 7 0.011 7 0.000 4 472.3 86.1 250.9 9.6 228.7 4.5 234.4 8.6
      T3-21 175 183 0.96 0.051 8 0.002 5 0.258 1 0.011 6 0.036 9 0.000 7 0.011 7 0.000 4 276.0 109.2 233.1 9.3 233.8 4.1 235.2 8.1
      T3-22 170 190 0.90 0.053 9 0.002 8 0.259 4 0.012 8 0.035 4 0.000 6 0.011 6 0.000 3 368.6 112.0 234.2 10.3 224.4 3.9 233.2 6.6
      T3-24 169 143 1.18 0.055 1 0.002 8 0.273 5 0.014 5 0.036 2 0.000 7 0.011 5 0.000 3 416.7 114.8 245.5 11.6 229.3 4.4 231.4 6.9
      T3-25 202 251 0.80 0.051 4 0.002 2 0.260 0 0.011 0 0.037 0 0.000 7 0.011 6 0.000 4 261.2 96.3 234.7 8.8 234.4 4.2 233.1 7.8
      注:数据为本文实测,测试单位为中国冶金地质总局山东局测试中心;“—”表示未测出.
      下载: 导出CSV

      表  6  岩体Lu-Hf同位素分析结果

      Table  6.   Zircon Lu-Hf isotopic compositions of the granites

      测点编号 t(Ma) 176Yb/177Hf 176Lu/177Hf 176Hf/177Hf 176Hf/177Hf εHf(t) TDM1(Ga) TDM2(Ga) fLu-Hf
      T1-1 230 0.021 047 0.000 677 0.282 406 0.000 019 0.282 403 -8.39 1.19 1.77 -0.98
      T1-2 222 0.017 015 0.000 563 0.282 422 0.000 024 0.282 419 -8.01 1.16 1.74 -0.98
      T1-3 236 0.017 513 0.000 569 0.282 406 0.000 020 0.282 404 -8.25 1.18 1.77 -0.98
      T1-4 233 0.016 979 0.000 560 0.282 416 0.000 020 0.282 414 -7.94 1.17 1.75 -0.98
      T1-5 230 0.029 125 0.000 925 0.282 400 0.000 018 0.282 396 -8.66 1.20 1.79 -0.97
      T1-6 222 0.022 929 0.000 753 0.282 431 0.000 021 0.282 428 -7.69 1.15 1.72 -0.98
      T1-7 213 0.014 228 0.000 466 0.282 425 0.000 021 0.282 423 -8.07 1.15 1.74 -0.99
      T1-8 233 0.040 871 0.001 196 0.282 420 0.000 025 0.282 415 -7.91 1.18 1.74 -0.96
      T1-9 230 0.021 081 0.000 684 0.282 416 0.000 023 0.282 413 -8.04 1.17 1.75 -0.98
      T1-10 235 0.062 914 0.002 099 0.282 392 0.000 028 0.282 383 -9.01 1.25 1.81 -0.94
      T1-11 235 0.017 466 0.000 578 0.282 417 0.000 021 0.282 414 -7.90 1.17 1.74 -0.98
      T1-12 231 0.019 854 0.000 668 0.282 366 0.000 026 0.282 363 -9.80 1.24 1.86 -0.98
      T1-13 226 0.032 511 0.001 085 0.282 423 0.000 023 0.282 418 -7.96 1.18 1.74 -0.97
      T1-14 238 0.022 421 0.000 772 0.282 454 0.000 029 0.282 451 -6.54 1.12 1.66 -0.98
      T1-15 234 0.011 114 0.000 381 0.282 412 0.000 030 0.282 411 -8.05 1.17 1.75 -0.99
      T1-16 225 0.018 516 0.000 620 0.282 497 0.000 022 0.282 494 -5.29 1.06 1.57 -0.98
      T1-17 233 0.035 832 0.001 140 0.282 412 0.000 033 0.282 407 -8.18 1.19 1.76 -0.97
      T1-18 233 0.019 791 0.000 668 0.282 425 0.000 028 0.282 422 -7.68 1.16 1.73 -0.98
      T1-19 238 0.019 598 0.000 653 0.282 445 0.000 024 0.282 442 -6.85 1.13 1.68 -0.98
      T1-20 236 0.042 546 0.001 394 0.282 341 0.000 025 0.282 335 -10.69 1.30 1.92 -0.96
      注:本文实测测试单位:南京大学内生金属矿床成矿机制国家重点实验室.
      下载: 导出CSV

      表  5  天宫山岩体锆石Ti含量地质温度计计算结果

      Table  5.   Calculation results of zircon Ti content geological thermometer of the Tiangongshan pluton

      点号 t(℃) 点号 t(℃) 点号 t(℃) 点号 t(℃)
      T1-01 572.3 T1-14 739.0 T3-01 717.3 T3-14 776.6
      T1-02 765.9 T1-15 725.0 T3-02 692.8 T3-15 768.0
      T1-03 761.6 T1-16 833.8 T3-03 736.9 T3-16 770.1
      T1-04 680.1 T1-17 713.4 T3-04 763.7 T3-17 692.8
      T1-05 689.1 T1-18 637.4 T3-05 739.0 T3-18 741.0
      T1-06 732.9 T1-19 698.3 T3-06 729.0 T3-19 751.2
      T1-07 713.4 T1-20 713.4 T3-07 741.0 T3-20 700.2
      T1-08 774.4 T3-08 536.0 T3-21 761.6
      T1-09 768.0 T3-09 751.2 T3-22 772.3
      T1-10 753.3 T3-10 702.1 T3-23 723.1
      T1-11 705.8 T3-11 763.7 T3-24 780.9
      T1-12 725.0 T3-12 732.9 T3-25 749.1
      T1-13 755.3 T3-13 789.8
      下载: 导出CSV
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    • 收稿日期:  2017-12-19
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