Petrogenesis of Middle Jurassic granitoids in Houdaomu, Central Jilin Province: Implications for the growth of Proterozoic continental crust in the eastern CAOB
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摘要:
中亚造山带属于地球上最大的增生型造山带其中之一，中亚造山带东部正是我国东北地区，而该地区的地壳增长时间与地壳增长机制仍然有待于进一步深入的研究。本研究选取中亚造山带东部后倒木地区的花岗质岩石为研究对象，进行岩石学、岩石地球化学、同位素年代学等研究，结合前人的研究成果，探讨其成因岩石学、构造背景以及对地壳增生的指示意义。通过同位素测年研究，发现后倒木地区的花岗岩类岩石就位于175~171Ma；全岩地球化学结果显示SiO2含量为66.58%~76.73%，Al2O3含量为12.21%~16.03%，MgO含量介于0.09%~2.07%之间，显示出高钾钙碱性特征；后倒木地区花岗岩类岩石富集大离子亲石元素，同时亏损高场强元素；Sr-Nd-Hf同位素显示：ISr值介于0.7063~0.7077之间，εNd（t）值介于+2.38~+3.95之间，具年轻的tDM2年龄（639~768Ma），岩浆锆石εHf（t）值介于+4.1~+9.0之间，同样具有年轻的二阶段模式年龄tDM2（554~806Ma），揭示岩石重熔的下地壳物质可能是花岗岩类岩石的源区。综合研究表明，古太平洋板块俯冲导致区域下地壳熔融，形成该类花岗质岩石，而模式年龄揭示新元古代为中亚造山带重要的地壳生长期。
Abstract:The Central Asian Orogenic Belt (CAOB) is one of the largest accretionary orogenic belts in the world. Northeast China is located in the eastern part of the CAOB,and its crustal growth time and mechanism need to be further explored. In this study,we selected the granitoids from Houdaomu area in the CAOB as the research objects,and studied their petrology,LA-ICP-MS zircon U-Pb geochronology,petrochemistry and Sr-Nd-Hf isotope geochemistry. Combined with the previous research results,we discussed their petrogenesis,tectonic setting and the indication of crustal accretion. The zircons from granitoids yield U-Pb concordant ages 175~171Ma. These granitoids are characterized by SiO2 (66.58%~76.73%),Al2O3 (12.21%~16.03%),and MgO (0.09%~2.07%) contents,showing the characteristics of high potassium calc alkaline; the rocks are enriched in LILE and depleted in HFSE,which is consistent with the trace elements of arc igneous rocks. The Sr-Nd-Hf isotopes show that the ISr values range from 0.7063 to 0.7077,the εNd(t) values range from +2.38 to +3.95,and the corresponding tDM2 ages are 639Ma to 768 Ma,the zircon εHf(t) values range from +4.1 to +9.0,and the two-stage model age tDM2 varying from 554Ma to 806Ma,suggesting that the rocks are derived from the remelting of the lower crust. The comprehensive study shows that the subduction of the Paleo Pacific Plate resulted in the melting of the regional lower crust and the formation of this kind of granitoids. The model age indicates that the Neoproterozoic was an important period of crustal growth in the CAOB.
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Key words:
- CAOB /
- Crust accretion /
- Houdaomu /
- Zircon U-Pb age /
- Geochemistry /
- Sr-Nd-Hf isotope
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图 1
中亚造山带构造纲要图(a, 据Ge et al., 2017修改)、研究区构造位置图(b, 据张海洪等, 2016修改)和张广才岭地区地质简图(c, 据鞠楠, 2020修改)
Figure 1.
Tectonic sketch map of CAOB (a, modified after Ge et al., 2017), tectonic sketch map of research area (b, modified after Zhang et al., 2016) and geological map of Zhangguangcai Range (c, modified after Ju, 2020)
图 2
后倒木地区地质图(据杨宝森, 2011修改)
Figure 2.
Geological map of the Houdaomu area (modified after Yang et al., 2011)
图 3
后倒木花岗岩类岩石野外及镜下照片
Figure 3.
Field and petrographic photos of granitoids in the Houdaomu
图 4
后倒木花岗质岩石中锆石阴极发光图像
Figure 4.
Cathodoluminescence (CL) images of representative zircons from granitoids in the Houdaomu
图 5
后倒木花岗质岩石LA-ICP-MS锆石U-Pb年龄谐和图
Figure 5.
U-Pb concordia diagrams of zircons for granitoids in the Houdaomu
图 6
后倒木花岗质岩石QAP图解(a, 据Streckeisen, 1976)、SiO2-K2O图解(b, 据Morrison, 1980)和A/CNK-A/NK判别图解(c, 据Middlemost, 1994)
Figure 6.
QAP diagram (after Streckeisen, 1976), SiO2 vs. K2O diagram (after Morrison, 1980) and A/CNK vs. A/NK diagram (after Middlemost, 1994) of granitoids in the Houdaomu
图 7
后倒木花岗质岩石球粒陨石标准化稀土元素配分图(a、c、e)和原始地幔标准化微量元素蛛网图(b、d、f)(标准化值据Sun and McDonough, 1989)
Figure 7.
REE chondrite-normalized patterns (a, c, e) and primitive mantle-normalized spider diagrams (b, d, f) of granitoids in the Houdaomu (normalization values after Sun and McDonough, 1989)
图 8
后倒木花岗质岩石的成因判别图(底图据Whalen et al., 1987)
Figure 8.
Discrimination diagrams of granitoids in the Houdaomu (base map after Whalen et al., 1987)
图 9
后倒木花岗质岩石SiO2-Ce判别图解(a)、Rb-Y图解(b)和Rb-Th图解(c)(据Li et al., 2007)
Figure 9.
SiO2 vs. Ce diagram (a), Rb vs. Y diagram (b) and Rb vs. Th diagram (c) (after Li et al., 2007) of granitoids in the Houdaomu
图 10
后倒木花岗质岩石(87Sr/86Sr)i-εNd(t)图解(底图据Jahn et al., 1999; Wu et al., 2000)和εHf(t)-t图解
Figure 10.
(87Sr/86Sr)i vs. εNd(t) diagram (after Jahn et al., 1999; Wu et al., 2000) and εHf(t) vs. t diagram of granitoids in the Houdaomu
图 11
后倒木花岗质岩石SiO2-εNd(t)、Eu-Sr、Sr-Rb/Sr和Sr-Ba判别图解
Figure 11.
Diagrams of SiO2 vs. εNd(t), Eu vs. Sr, Sr vs. Rb/Sr and Sr vs. Ba of granitoids in the Houdaomu
图 12
后倒木花岗质岩石Harker图解
Figure 12.
Diagrams of SiO2 against predominant oxides of granitoids in the Houdaomu
图 13
后倒木花岗质岩石的Yb-Ta (a)、Y-Nb (b)、(Y+Nb)-Rb (c)、(Yb+Ta)-Rb (d)构造环境判别图解(据Pearce et al., 1984)
Figure 13.
Tectonic setting discrimination diagrams of Yb vs. Ta (a), Y vs. Nb (b), Y+Nb vs. Rb (c) and Yb+Ta vs. Rb (d) for granitoids in Houdaomu (base map after Pearce et al., 1984)
图 14
后倒木花岗质岩石的Rb/10-Hf-Ta×3 (a)和Rb/30-Hf-Ta×3 (b)构造环境判别图解(据Pearce et al., 1984)
Figure 14.
Tectonic setting discrimination diagrams of Rb/10-Hf-Ta×3 (a) and Rb/30-Hf-Ta×3 (b) for granitoids in the Houdaomu (base map after Pearce et al., 1984)
图 15
松辽地块东部花岗岩锆石(a, 据陈贤, 2018)和中国东北地区河流碎屑锆石(b, 据李明, 2010)Hf同位素二阶段模式年龄(tDM2)频谱图
Figure 15.
Spectrum for Hf isotope two-stage model age (tDM2) of granite zircon in eastern Songliao block (a, after Chen, 2018) and of detrital zircons from rivers in Northeast China (b, after Li, 2010)
表 1
后倒木花岗质岩石LA-ICP-MS锆石测年数据
Table 1.
Zircon U-Pb isotope data of granitoids in the Houdaomu
测点号 Th U Th/U 同位素比值 同位素年龄(Ma) (×10-6) 
1σ 
1σ 
1σ 
1σ 
1σ 
1σ HDM-N1花岗闪长岩 1 76 191 0.40 0.05175 0.00173 0.19227 0.01148 0.02752 0.00037 271.7 79.8 178.9 9.6 175.2 3.2 2 60 124 0.49 0.04957 0.00198 0.18980 0.00929 0.02747 0.00058 172.1 85.6 176.5 7.6 174.6 3.7 3 65 155 0.42 0.05187 0.00384 0.19157 0.00867 0.02751 0.00047 267.6 152.3 177.6 7.2 174.7 3.0 4 58 123 0.47 0.05058 0.00337 0.18987 0.00901 0.02747 0.00061 217.6 147.6 176.6 8.6 174.8 3.0 5 60 159 0.38 0.04988 0.00246 0.18759 0.00999 0.02748 0.00050 157.6 117.6 174.6 9.0 174.8 3.4 6 67 159 0.42 0.05024 0.00258 0.18969 0.01126 0.02750 0.00049 201.5 119.6 177.0 9.6 174.9 3.6 7 62 138 0.45 0.05120 0.00266 0.19279 0.01026 0.02751 0.00056 253.5 115.3 179.6 9.0 175.1 3.4 8 72 187 0.39 0.05026 0.00138 0.19128 0.00866 0.02753 0.00039 199.6 65.6 178.6 7.1 175.1 3.2 9 75 176 0.43 0.04988 0.00246 0.18577 0.01025 0.02753 0.00050 158.6 107.7 173.6 8.6 175.1 3.2 10 68 167 0.41 0.04988 0.00358 0.19276 0.00518 0.02750 0.00042 158.6 171.6 179.2 4.6 175.1 3.0 11 67 157 0.43 0.05024 0.00287 0.18959 0.01094 0.02750 0.00055 207.6 117.6 176.0 8.6 174.7 3.2 12 65 147 0.44 0.05118 0.00276 0.18756 0.01016 0.02749 0.00049 252.6 115.6 174.6 9.0 174.9 3.6 13 67 157 0.43 0.05048 0.00178 0.18758 0.00986 0.02749 0.00056 209.7 79.5 174.6 7.9 175.0 3.1 14 69 175 0.39 0.05076 0.00276 0.18968 0.01088 0.02752 0.00037 211.9 116.0 176.6 8.7 175.2 3.2 15 59 187 0.32 0.05096 0.00258 0.19238 0.01069 0.02751 0.00049 211.9 117.6 179.9 8.6 175.1 3.0 HDM-N2二长花岗岩 1 59 129 0.45 0.05107 0.0025 0.18734 0.00935 0.02721 0.00047 243.8 112.8 174.4 8.0 173.0 3.0 2 91 145 0.63 0.0491 0.00297 0.18327 0.01121 0.02721 0.00048 152.4 141.8 170.9 9.6 173.1 3.0 3 107 174 0.62 0.04908 0.00241 0.18204 0.00873 0.02722 0.00043 151.4 115.1 169.8 7.5 173.1 2.7 4 79 194 0.41 0.05047 0.0016 0.18774 0.00586 0.02722 0.00036 216.9 73.2 174.7 5.0 173.2 2.3 5 60 139 0.43 0.05107 0.00209 0.18831 0.00746 0.02728 0.00044 243.9 94.1 175.2 6.4 173.5 2.7 6 71 150 0.47 0.04887 0.00161 0.18305 0.00616 0.02728 0.00038 141.7 77.2 170.7 5.3 173.5 2.4 7 128 319 0.40 0.05001 0.00135 0.18808 0.00532 0.02728 0.00037 195.4 62.8 175.0 4.5 173.5 2.3 8 65 132 0.50 0.05036 0.00274 0.18739 0.00936 0.02729 0.00055 211.6 126.2 174.4 8.0 173.6 3.5 9 61 125 0.49 0.05248 0.0047 0.188 0.01459 0.02735 0.0006 306.5 204.0 174.9 12.5 173.9 3.8 10 61 125 0.49 0.04915 0.00298 0.18464 0.0113 0.02746 0.00059 155.1 142.0 172.0 9.7 174.6 3.7 11 66 155 0.42 0.05164 0.00285 0.19372 0.01066 0.02747 0.00047 269.5 126.5 179.8 9.1 174.7 3.0 12 59 124 0.47 0.05016 0.00237 0.18867 0.00901 0.02749 0.00047 202.5 109.7 175.5 7.7 174.8 3.0 13 77 191 0.40 0.05108 0.00274 0.19373 0.01049 0.02754 0.00051 244.4 123.5 179.8 8.9 175.2 3.2 14 47 105 0.45 0.05013 0.00519 0.19495 0.01915 0.02735 0.00066 208.1 186.7 197.7 16.0 173.9 4.1 15 68 157 0.43 0.05199 0.00319 0.18717 0.00978 0.02712 0.00056 257.6 157.1 174.7 8.2 173.9 2.2 HDM-N3正长花岗岩 1 89 140 0.63 0.05160 0.00364 0.18246 0.01192 0.02646 0.00061 268.2 162.1 170.2 10.2 168.4 3.9 2 90 201 0.45 0.05121 0.00249 0.18703 0.00911 0.02651 0.00048 250.7 112.0 174.1 7.8 168.7 3.0 3 128 196 0.65 0.05374 0.00450 0.18949 0.01403 0.02663 0.00063 360.2 189.0 176.2 12.0 169.5 4.0 4 113 172 0.65 0.05011 0.00246 0.18209 0.00849 0.02680 0.00042 200.4 114.0 169.9 7.3 170.5 2.7 5 60 133 0.45 0.04951 0.00230 0.18052 0.00839 0.02688 0.00044 172.4 108.6 168.5 7.2 171.0 2.8 6 79 117 0.67 0.04784 0.00309 0.17374 0.01133 0.02689 0.00060 91.6 153.1 162.7 9.8 171.1 3.8 7 120 169 0.71 0.04977 0.00188 0.18279 0.00719 0.02695 0.00039 184.6 88.4 170.5 6.2 171.4 2.4 8 88 196 0.45 0.05020 0.00233 0.18631 0.00909 0.02698 0.00040 204.6 107.8 173.5 7.8 171.7 2.5 9 61 130 0.47 0.05057 0.00258 0.18404 0.00936 0.02700 0.00048 221.5 118.1 171.5 8.0 171.7 3.1 10 61 129 0.47 0.04956 0.00439 0.17767 0.01441 0.02700 0.00071 174.5 206.8 166.1 12.4 171.8 4.5 11 73 159 0.46 0.05121 0.00220 0.18736 0.00743 0.02702 0.00042 250.3 99.2 174.4 6.4 171.9 2.7 12 76 162 0.47 0.05116 0.00209 0.18886 0.00778 0.02706 0.00041 248.3 94.3 175.7 6.6 172.2 2.6 13 77 136 0.57 0.04929 0.00294 0.17992 0.00993 0.02707 0.00054 161.7 139.6 168.0 8.6 172.2 3.4 14 116 171 0.68 0.04945 0.00218 0.18307 0.00809 0.02708 0.00037 169.3 103.2 170.7 6.9 172.3 2.3 15 56 122 0.46 0.05177 0.00414 0.19039 0.01555 0.02710 0.00079 275.5 183.3 177.0 13.3 172.4 5.0 16 57 118 0.48 0.05021 0.00250 0.18180 0.00900 0.02714 0.00047 204.7 115.6 169.6 7.7 172.7 3.0 
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表 2
后倒木花岗质岩石主量元素(wt%)、稀土和微量元素(×10-6)测试结果
Table 2.
Major (wt%) and trace (×10-6) elements data of granitoids in the Houdaomu
样品号 HDM-N1-Q1 -Q2 -Q3 -Q4 -Q5 -Q6 HDM-N2-Q1 -Q2 -Q3 -Q4 -Q5 HDM-N3-Q1 -Q2 -Q3 -Q4 -Q5 -Q6 岩性 花岗闪长岩 二长花岗岩 正长花岗岩 SiO2 67.02 68.17 66.58 67.68 67.27 67.63 69.85 70.73 71.61 70.64 70.42 75.71 76.57 75.95 76.08 76.21 76.73 TiO2 0.47 0.45 0.49 0.41 0.53 0.41 0.36 0.35 0.35 0.37 0.35 0.07 0.06 0.08 0.06 0.08 0.07 Al2O3 15.57 15.67 15.46 15.09 15.67 16.03 15.17 14.85 14.61 15.07 14.89 12.71 12.21 12.57 12.65 12.34 12.42 Fe2O3 1.17 0.87 1.21 1.39 0.93 0.92 0.91 0.85 1.05 0.93 0.83 0.42 0.35 0.37 0.31 0.24 0.31 FeO 2.65 2.16 2.95 2.75 2.65 2.57 1.32 1.12 1.12 1.37 1.07 0.98 1.15 0.95 1.17 1.01 0.99 MnO 0.07 0.10 0.09 0.08 0.11 0.07 0.06 0.08 0.07 0.10 0.09 0.08 0.10 0.10 0.08 0.07 0.11 MgO 2.05 2.07 1.97 1.82 2.05 1.82 0.51 0.57 0.49 0.59 0.52 0.09 0.11 0.11 0.10 0.09 0.11 CaO 2.87 2.54 2.83 2.87 3.31 2.57 2.05 2.11 2.05 1.87 1.95 0.86 0.60 0.75 0.72 0.68 0.82 Na2O 3.72 4.17 4.32 3.87 3.87 3.92 4.15 4.24 4.05 4.05 3.92 3.68 3.95 4.02 3.92 3.85 3.72 K2O 2.57 2.52 3.04 2.97 2.67 3.07 4.05 3.87 3.85 3.91 4.68 3.85 3.95 4.12 4.15 4.01 3.87 P2O5 0.11 0.11 0.12 0.12 0.11 0.12 0.12 0.13 0.12 0.13 0.13 0.01 0.03 0.02 0.03 0.01 0.01 LOI 0.80 0.85 0.57 0.73 0.67 0.57 0.75 0.92 0.57 0.51 0.92 0.37 0.67 0.57 0.70 0.85 0.68 Total 99.07 99.68 99.63 99.78 99.84 99.70 99.30 99.82 99.94 99.54 99.77 98.83 99.75 99.61 99.97 99.44 99.84 La 12.17 18.57 17.25 16.37 17.05 15.27 21.87 30.27 28.57 22.71 26.27 16.87 17.51 17.28 16.98 17.05 17.31 Ce 35.38 27.28 25.37 34.35 29.57 38.97 45.36 53.57 49.64 50.67 47.19 38.21 35.47 36.57 37.58 38.02 36.83 Pr 4.78 3.02 4.25 3.65 3.96 4.15 6.45 5.03 6.02 5.75 5.32 4.80 4.45 4.57 4.65 4.75 4.58 Nd 17.25 13.57 15.57 16.34 14.57 16.37 23.05 19.78 22.09 21.76 20.87 17.25 16.57 16.39 16.52 16.03 16.97 Sm 2.87 2.57 2.14 2.25 2.96 2.78 3.70 3.28 3.54 3.65 3.33 3.08 3.52 3.33 3.47 3.28 3.48 Eu 0.82 0.67 0.75 0.79 0.80 0.70 0.61 0.51 0.56 0.60 0.57 0.24 0.28 0.27 0.26 0.25 0.27 Gd 2.56 1.87 1.98 2.02 2.42 2.24 2.15 2.89 2.54 2.22 2.76 2.25 2.85 2.76 2.65 2.57 2.35 Tb 0.33 0.31 0.26 0.29 0.30 0.31 0.29 0.31 0.32 0.31 0.30 0.31 0.42 0.40 0.36 0.37 0.38 Dy 1.45 1.89 1.65 1.75 1.52 1.49 1.49 1.57 1.52 1.50 1.56 2.15 1.79 1.86 1.97 2.05 2.63 Ho 0.29 0.37 0.35 0.32 0.34 0.31 0.26 0.27 0.27 0.26 0.27 0.35 0.48 0.45 0.42 0.40 0.37 Er 0.79 1.00 0.86 0.98 1.00 0.96 0.70 0.73 0.74 0.75 0.72 0.87 1.32 1.25 1.11 1.05 0.95 Tm 0.12 0.15 0.13 0.14 0.15 0.14 0.09 0.10 0.09 0.10 0.09 0.15 0.22 0.20 0.19 0.17 0.20 Yb 0.75 1.00 0.98 0.85 0.86 0.96 0.64 0.65 0.64 0.66 0.65 0.86 0.98 1.30 1.12 1.02 1.15 Lu 0.15 0.11 0.13 0.12 0.14 0.15 0.09 0.09 0.10 0.10 0.09 0.17 0.25 0.22 0.19 0.21 0.22 ∑REE 80.7 72.1 72.7 80.5 76.1 85.7 107.2 119.5 117.8 111.5 110.7 88.5 86.1 87.5 88.2 87.7 88.1 δEu 0.93 0.94 1.12 1.14 0.92 0.86 0.66 0.51 0.58 0.65 0.57 0.29 0.27 0.28 0.27 0.27 0.30 (La/Yb)N 11.5 13.3 12.6 13.7 14.1 11.3 24.3 33.3 31.6 24.3 28.8 14.0 12.8 9.5 10.8 11.9 10.7 Ti 2857 2982 3125 2875 3257 2987 2238 2229 2368 2403 2298 458.3 487.5 475.3 467.2 478.3 468.9 Zn 157.6 68.26 98.26 117.9 158.3 98.25 51.51 82.87 75.56 65.71 68.24 45.67 62.32 57.35 58.39 51.67 60.35 Ga 20.25 19.25 18.65 20.35 21.05 19.35 20.07 22.91 21.05 22.09 21.79 16.98 18.05 17.89 17.65 17.29 16.83 Rb 75.36 65.36 38.25 45.35 68.37 42.35 87.58 135.4 125.2 107.3 98.37 147.5 180.5 175.7 168.2 159.3 178.9 Sr 75.98 81.98 87.26 78.25 74.29 87.29 45.67 50.57 55.87 49.68 57.28 35.57 41.58 40.76 37.86 36.79 39.75 Y 10.25 9.28 7.29 8.75 9.67 7.76 6.72 7.18 7.57 6.97 7.52 12.57 7.86 8.67 9.37 8.27 11.57 Zr 98.2 110.5 93.5 102.5 87.2 108.7 147.8 237.9 220.6 201.7 187.5 85.6 128.5 98.5 117.8 105.8 115.7 Nb 3.58 4.75 4.57 3.86 4.02 4.57 7.70 8.25 9.05 7.95 8.57 10.57 7.58 8.57 9.37 10.08 9.37 Ba 598.2 602.3 487.2 395.2 547.3 475.2 578.5 605.7 684.5 621.7 697.5 170.5 165.2 157.5 159.6 162.8 158.8 Hf 3.72 5.87 4.35 3.89 4.57 5.35 5.65 7.02 7.32 6.68 6.57 3.57 5.02 4.25 3.95 4.75 4.35 Ta 0.33 0.53 0.45 0.47 0.49 0.42 0.65 0.70 0.66 0.68 0.68 0.58 0.68 0.70 0.59 0.65 0.61 Th 3.72 8.02 7.25 6.35 5.24 4.25 8.78 11.05 10.65 9.59 10.57 15.85 18.03 17.65 16.52 17.2 16.71 U 2.02 2.57 2.35 2.46 2.27 2.18 2.98 3.95 3.25 3.68 4.02 3.85 5.57 6.23 7.58 5.35 5.95
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表 3
后倒木花岗质岩石中锆石的Hf同位素组成
Table 3.
Zircon Hf isotopic compositions of granitoids in the Houdaomu
测点号 176Yb/177Hf 2σ 176Lu/177Hf 2σ 176Hf/177Hf 2σ t(Ma) εHf(t) tDM2 (Ma) fLu/Hf HDM-N1花岗闪长岩 1 0.017280 0.000561 0.000547 0.000021 0.282875 0.000015 7.4 634 -0.98 2 0.013441 0.000177 0.000434 0.000010 0.282904 0.000014 8.5 580 -0.99 3 0.016786 0.000207 0.000553 0.000010 0.282864 0.000015 7.1 653 -0.98 4 0.021081 0.000292 0.000701 0.000005 0.282919 0.000017 9.0 554 -0.98 5 0.018066 0.000339 0.000618 0.000019 0.282889 0.000016 7.9 609 -0.98 6 0.018298 0.000432 0.000558 0.000012 0.282907 0.000014 8.6 575 -0.98 7 0.018196 0.000110 0.000599 0.000006 0.282854 0.000014 6.7 672 -0.98 8 0.022268 0.000539 0.000711 0.000009 0.282881 0.000016 175 7.6 623 -0.98 9 0.020327 0.000148 0.000681 0.000010 0.282872 0.000018 7.3 640 -0.98 10 0.018861 0.000207 0.000603 0.000012 0.282885 0.000015 7.8 615 -0.98 11 0.022599 0.000369 0.000726 0.000018 0.282903 0.000015 8.4 584 -0.98 12 0.024459 0.000906 0.000793 0.000020 0.282896 0.000014 8.1 598 -0.98 13 0.056960 0.001325 0.001714 0.000021 0.282784 0.000015 4.1 806 -0.95 14 0.017273 0.000586 0.000539 0.000012 0.282894 0.000015 8.1 599 -0.98 15 0.028054 0.000508 0.000893 0.000009 0.282886 0.000016 7.8 616 -0.97 HDM-N2二长花岗岩 1 0.017751 0.000706 0.000600 0.000017 0.282902 0.000020 8.3 586 -0.98 2 0.031521 0.000299 0.000945 0.000009 0.282863 0.000014 6.9 658 -0.97 3 0.029870 0.000459 0.000893 0.000009 0.282877 0.000015 7.4 633 -0.97 4 0.019215 0.000322 0.000630 0.000006 0.282865 0.000014 7.0 653 -0.98 5 0.020865 0.000890 0.000650 0.000022 0.282911 0.000016 8.6 569 -0.98 6 0.040067 0.000224 0.001213 0.000006 0.282871 0.000016 7.2 646 -0.96 7 0.027375 0.000509 0.000840 0.000013 0.282884 0.000016 7.7 619 -0.97 8 0.025043 0.000437 0.000795 0.000016 0.282855 0.000016 173 6.6 673 -0.98 9 0.024137 0.000347 0.000781 0.000017 0.282855 0.000015 6.7 671 -0.98 10 0.020681 0.000113 0.000696 0.000007 0.282904 0.000015 8.4 583 -0.98 11 0.024686 0.000936 0.000753 0.000018 0.282867 0.000015 7.1 651 -0.98 12 0.026996 0.000248 0.000830 0.000006 0.282870 0.000016 7.2 645 -0.98 13 0.020894 0.000131 0.000695 0.000011 0.282870 0.000013 7.2 645 -0.98 14 0.023981 0.000139 0.000735 0.000007 0.282875 0.000014 7.4 635 -0.98 15 0.028356 0.000592 0.000870 0.000008 0.282874 0.000015 7.3 637 -0.97 HDM-N3正长花岗岩 1 0.020549 0.000251 0.000649 0.000007 0.282872 0.000014 7.2 641 -0.98 2 0.018243 0.000231 0.000612 0.000016 0.282877 0.000014 7.4 632 -0.98 3 0.020553 0.000121 0.000653 0.000010 0.282891 0.000015 7.9 606 -0.98 4 0.022328 0.000530 0.000687 0.000019 0.282884 0.000016 7.6 619 -0.98 5 0.020017 0.000381 0.000664 0.000020 0.282893 0.000015 8.0 602 -0.98 6 0.018902 0.000191 0.000624 0.000011 0.282882 0.000013 7.6 622 -0.98 7 0.018983 0.000419 0.000635 0.000007 0.282878 0.000017 7.4 631 -0.98 8 0.019030 0.000195 0.000615 0.000008 0.282866 0.000016 171 7.0 652 -0.98 9 0.014267 0.000232 0.000465 0.000003 0.282918 0.000015 8.9 556 -0.99 10 0.014181 0.000249 0.000438 0.000011 0.282904 0.000014 8.4 581 -0.99 11 0.038796 0.000278 0.001275 0.000017 0.282883 0.000016 7.6 624 -0.96 12 0.017600 0.000177 0.000547 0.000010 0.282896 0.000014 8.1 597 -0.98 13 0.019199 0.000242 0.000593 0.000011 0.282894 0.000017 8.0 600 -0.98 14 0.015228 0.000394 0.000469 0.000008 0.282915 0.000015 8.7 562 -0.99 15 0.014193 0.000458 0.000440 0.000009 0.282895 0.000016 8.1 597 -0.99 16 0.019872 0.000192 0.000579 0.000008 0.282892 0.000015 7.9 604 -0.98
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表 4
后倒木花岗质岩石Sr-Nd同位素组成
Table 4.
Sr-Nd isotopic compositions of granitoids in the Houdaomu
样品号 Age Rb Sr 
2σ Sm Nd 
2σ ISr εNd(t) tDM2 (Ma) (×10-6) (×10-6) (Ma) HDM-N1-Q1 175 70.58 51.22 3.987 0.716875 0.000005 2.20 11.30 0.117633 0.512697 0.000005 0.706954 2.92 724 HDM-N1-Q2 175 61.79 47.92 3.731 0.716157 0.000007 1.92 11.17 0.103856 0.512685 0.000007 0.706874 2.99 718 HDM-N1-Q3 175 37.71 45.31 2.408 0.712983 0.000007 2.07 15.02 0.083269 0.512708 0.000006 0.706991 3.90 644 HDM-N1-Q4 175 43.95 48.57 2.618 0.712992 0.000005 2.21 16.09 0.082989 0.512671 0.000007 0.706477 3.19 702 HDM-N1-Q5 175 67.82 55.72 3.522 0.715082 0.000006 2.15 14.01 0.092722 0.512692 0.000005 0.706319 3.38 686 HDM-N1-Q6 175 41.02 55.99 2.120 0.712005 0.000005 2.02 15.58 0.078337 0.512705 0.000007 0.706730 3.95 639 HDM-N2-Q1 173 81.72 37.71 6.271 0.722005 0.000005 3.39 21.52 0.095179 0.512685 0.000007 0.706582 3.19 702 HDM-N2-Q2 173 75.71 42.75 5.125 0.719879 0.000007 3.01 18.05 0.100757 0.512705 0.000005 0.707275 3.45 680 HDM-N2-Q3 173 72.82 38.67 5.449 0.720089 0.000006 3.51 21.17 0.100178 0.512692 0.000001 0.706687 3.21 700 HDM-N2-Q4 173 78.89 41.85 5.455 0.720978 0.000005 3.58 20.51 0.105493 0.512672 0.000007 0.707562 2.70 741 HDM-N2-Q5 173 82.57 39.91 5.987 0.721982 0.000007 3.07 20.05 0.092514 0.512702 0.000005 0.707257 3.58 670 HDM-N3-Q1 171 57.65 30.82 5.413 0.719875 0.000005 3.01 17.02 0.106854 0.512657 0.000008 0.706716 2.38 768 HDM-N3-Q2 171 51.57 31.17 4.787 0.719017 0.000007 2.31 16.57 0.084231 0.512669 0.000007 0.707378 3.11 708 HDM-N3-Q3 171 47.73 32.92 4.195 0.717982 0.000007 3.01 16.32 0.111437 0.512702 0.000005 0.707782 3.15 704 HDM-N3-Q4 171 41.07 30.57 3.887 0.717015 0.000005 3.07 16.52 0.112283 0.512689 0.000007 0.707564 2.88 727 HDM-N3-Q5 171 45.72 32.15 4.115 0.717057 0.000007 3.08 16.01 0.116237 0.512675 0.000005 0.707053 2.52 756 HDM-N3-Q6 171 50.07 30.02 4.826 0.719005 0.000005 3.02 16.92 0.107843 0.512682 0.000007 0.707272 2.84 730 注：(87Sr/86Sr)CHUR=0.7045，(87Rb/86Sr)CHUR=0.0827，λRb=0.0142Ga-1，(143Nd/144Nd)CHUR=0.5126，(147Sm/144Nd)CHUR=0.1967，(143Nd/144Nd)DM=0.5132，(147Sm/144Nd)DM=0.2137，λSr=0.0065Ga-1(Hart, 1984)，fSm/Nd=(147Sm/144Nd)s/(147Sm/144Nd)CHUR-1，s代表样品
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