Petrogenesis and Tectonic Settings of Volcanic Rocks from Late Triassic Hadataolegai Fm. at Central Part of Great Xing'an Range
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摘要: 为了解大兴安岭中段晚三叠世时期的构造背景，对该时期哈达陶勒盖组火山岩进行了岩石学、锆石U-Pb年代学及地球化学等方面的研究.哈达陶勒盖组火山岩可划分为中性系列安粗岩、安山岩，中酸性系列石英粗安岩及酸性系列流纹岩，形成年龄分别为：210.9±3.5 Ma、216.6±3.1 Ma、216.9±2.1 Ma和230.2±2.2 Ma.中性系列岩浆来源于原始地幔的部分熔融，并遭受俯冲板片释放流体的强烈富集作用.岩浆演化过程中结晶分异作用不明显，但遭受较强的地壳混染.中酸性系列和酸性系列岩浆来源于相对较浅的地壳物质深熔，前者岩浆演化过程中结晶分异作用较弱，而后者则较强.大兴安岭中段晚三叠世时期的构造演化背景受蒙古-鄂霍茨克洋板块向南俯冲作用的影响明显，在研究区表现为弧后伸展的构造背景.俯冲板片的断离拆沉引起了软流圈物质上涌，并导致伸展构造背景的形成，也为哈达陶勒盖组火山岩原始岩浆的形成提供了热量来源.Abstract: To realize the tectonic setting at central part of Great Xing'an Range during Late Triassic, petrology, zircon U-Pb chronology and geochemical of the Late Triassic Hadataolegai Fm. were analyzed in this paper. The volcanic rocks from Late Triassic Hadataolegai Fm. can be divided into three rock series which are intermediate latite and andesite, intermediate to acidic quartz trachyandensite and acid rhyolite, and their formation ages are 210.9±3.5 Ma, 216.6±3.1 Ma, 216.9±2.1 Ma and 230.2±2.2 Ma, respectively.The magma of intermediate series was derived from partial melting of lithospheric mantle which fully enriched by fluids released from subduction oceanic lithosphere.There have no or slightly crystallization fractionation but suffered seriously crustal contamination during magma upwelling.Intermediate to acidic and acidic series rocks have crustal-derived magma source features, the crystallization fractionation of intermediate to acidic magma was unconspicuous during its evolution course, but it was quite obvious to the acidic series.The southward subduction of the Okhotsk oceanic lithosphere has played an important role to the tectonic setting at central part of Great Xing'an Range during Late Triassic, and appear back-arc extension signiture at the study area.This extension background leaded by asthenosphere magma upwelling which caused by subduction oceanic lithosphere delamination, and the asthenosphere magma upwelling provides energy to the primary magma generation for volcanic rocks of the Late Triassic Hadataolegai Fm. meanwhile.
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图 1 (a) 中亚造山带及邻区构造简图；(b)东北地区构造格架图；(c)研究区地质图
F1.新林-喜桂图缝合带；F2.贺根山-黑河缝合带；F3.索伦克尔-西拉木伦-长春缝合带；F4.依兰-伊通断裂；F5.敦化-密山断裂；F6.牡丹江断裂；a.根据Safonova and Santosh (2014)修改；b.根据Liu et al.(2017)、Zhou and Wilde(2013)修改
Fig. 1. (a) Simplified tectonic framework of CAOB and surround areas; (b) Tectonic division of Northeast China; and (c) Detailed geological maps of study area
图 2 晚三叠世哈达陶勒盖组火山岩典型岩石露头及显微照片
a.安粗岩镜下照片：斑晶钾长石遭受明显的熔蚀及轻微碎裂；b.安山岩镜下照片：斑晶斜长石碎裂明显；c.石英粗安岩野外露头；d.石英粗安岩镜下照片；e.流纹岩野外露头；f.流纹岩镜下照片(斜长石及石英斑晶遭受明显熔蚀)；Kfs.钾长石；PI.斜长石；Aug.普通辉石；Bt.黑云母；Qtz.石英
Fig. 2. Typical filed rock outcrops and its microscopic photomicrographs for the volcanic rocks from Late Triassic Hadataolegai Fm.
图 4 晚三叠世哈达陶勒盖组火山岩U-Pb年龄谐和图
Fig. 4. U-Pb Concordia diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.
图 3 晚三叠世哈达陶勒盖组火山岩典型锆石阴极发光(CL)图像
Fig. 3. Typical Cathodoluminescence (CL) images of selected zircon grains for the volcanic rocks from Late Triassic Hadataolegai Fm.
图 5 晚三叠世哈达陶勒盖组火山岩主量元素图解
a.(K2O+Na2O)-SiO2图解；b.(K2O+Na2O-CaO)-SiO2图解, 根据Frost et al.(2001)绘制；c.K2O-SiO2图解, 根据Peccerillo and Taylor(1976)绘制；d.A/KN-A/KNC图解, 根据Maniar and Piccoli(1989)绘制; A/CNK=分子数Al2O3/(Na2O+K2O+CaO)，A/NK=分子数Al2O3/(Na2O+K2O)
Fig. 5. Major element diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.
图 6 晚三叠世哈达陶勒盖组火山岩主量元素Harker图解
TFeO= FeO+0.899 8Fe2O3
Fig. 6. Major element Harker diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.
图 7 晚三叠世哈达陶勒盖组火山岩微量元素与SiO2含量协变图解
Fig. 7. Plots of various trace elements vs.SiO2 for the volcanic rocks from Late Triassic Hadataolegai Fm.
图 8 晚三叠世哈达陶勒盖组火山岩球粒陨石标准化稀土元素配分模式图(a, c, e)和原始地幔标准化微量元素蛛网图(b, d, f)
a, c, e.标准化值据Boynton(1984)；b, d, f.标准值化据Sun and McDonough(1989)
Fig. 8. Chondrite-normalized rare earth element patterns (a, c, e) and Primitive mantle-normalized trace element spider diagrams (b, d, f) for the volcanic rocks from Late Triassic Hadataolegai Fm.
图 9 晚三叠世哈达陶勒盖组火山岩
a.Sm/Yb-Sm图解；b.La/Ba-La/Nb图解；c.Th/Y-Sm/Th图解；d.Ba/Th-(La/Sm)N图解；其中图a中分别由原始地幔及亏损地幔为源区的尖晶石二辉橄榄岩(Ol0.53+Opx0.27+Cpx0.17+Sp0.13)及石榴石二辉橄榄岩(Ol0.60+Opx0.20+Cpx0.10+Gt0.10)熔融曲线根据Aldanmaz et al.(2000)和Zhao and Zhou(2007b, 2009)的数据模式绘制.实线代表由原始地幔熔融的曲线，虚线代表由亏损地幔熔融的曲线，各熔融曲线上短线段旁的数字代表熔融程度；DM.亏损地幔(McKenzie and O'Nions，1991)；PM.原始地幔(Sun and McDonough, 1989)；HIMU.高U/Pb比值地幔源区(Saunders et al., 1992)；MORB.大洋中脊玄武岩源区；OIB.洋岛玄武岩源区(Sun and McDonough, 1989)；CLM.大陆岩石圈地幔(Sun and McDonough, 1989)；N-MORB.正常的大洋中脊玄武岩(Sun and McDonough, 1989)
Fig. 9. The volcanic rocks from Late Triassic Hadataolegai Fm.
图 10 晚三叠世哈达陶勒盖组火山岩岩石类型判别图解
a.[(K2O+Na2O)/CaO]-(Zr+Nb+Ce+Y)图解；b.(TFeO/MgO)-(Zr+Nb+Ce+Y)图解；a和b据Whalen et al.(1987)绘制
Fig. 10. Diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.with rock type discrimination purpose
图 11 晚三叠世哈达陶勒盖组火山岩
a.(La/Yb)N-YbN图解，跟据Drummond and Defant(1990)；b.Sr/Y-Y图解，跟据Martin(1999)
Fig. 11. Diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.
图 12 晚三叠世哈达陶勒盖组火山岩图解
a.Hf/3-Th-Nb/16图解，跟据Wood(1980)；b.Rb-Y+Nb图解，跟据Pearce et al.(1984)
Fig. 12. Diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.
图 13 大兴安岭中段地区晚三叠世哈达陶勒盖组火山岩成因模式及构造背景简图
Fig. 13. Schematic diagram showing the petrogenetic model and tectonic background for the volcanic rocks from Late Triassic Hadataolegai Fm.at central Great Xing'an Rang
表 1 晚三叠世哈达陶勒盖组火山岩主量(wt%)、稀土和微量元素(10-6)分析结果
Table 1. Major (wt%) and trace elements (10-6) analysis result of the volcanic rocks from Late Triassic Hadataolegai Fm.
样号 中性系列 中酸性系列 酸性系列 PM305-5-1YQ TC303Q1 TC106Q2 TC107Q2 TC125YQ1 PM101-18-1Q PM302-1-1Q PM206-13-1YQ PM209-5-1YQ PM209-7-1YQ PM206-37-1YQ PM208-9-1YQ TC128YQ1 t1106YQ3 SiO2 55.86 55.98 53.59 60.17 56.26 57.28 61.44 66.18 67.42 67.51 70.60 79.37 72.92 75.60 TiO2 1.17 1.12 1.19 0.80 0.92 1.00 0.69 0.76 0.59 0.61 0.35 0.14 0.36 0.13 Al2O3 17.41 18.06 17.51 16.85 17.82 17.20 15.85 16.33 15.52 15.10 14.47 10.85 14.38 12.58 Fe2O3 5.52 7.42 5.79 2.92 3.56 4.57 3.41 3.61 1.84 1.29 2.74 1.09 1.73 1.20 FeO 1.28 1.71 4.04 3.23 4.36 3.55 2.56 0.76 0.81 1.17 0.31 0.22 0.67 0.56 TFeO 6.25 8.39 9.25 5.86 7.57 7.66 5.63 4.01 2.47 2.33 2.78 1.20 2.23 1.64 MnO 0.08 0.13 0.13 0.09 0.11 0.13 0.09 0.04 0.06 0.08 0.07 0.01 0.03 0.02 MgO 2.17 1.68 4.05 4.24 4.42 3.21 2.96 0.60 0.56 0.79 0.48 0.02 0.47 1.66 CaO 5.29 1.99 6.37 2.56 4.52 5.72 5.06 1.42 1.06 1.53 1.40 0.43 0.43 0.29 Na2O 5.84 6.10 4.44 4.33 3.86 4.49 4.31 4.63 5.56 4.70 3.36 1.66 3.08 3.98 K2O 2.30 2.21 1.74 2.14 1.40 1.92 2.92 4.63 4.76 4.86 5.12 5.49 4.57 3.21 P2O5 0.42 0.41 0.44 0.31 0.32 0.31 0.23 0.21 0.13 0.16 0.15 0.06 0.11 0.03 LOI 1.63 3.61 1.09 2.36 3.11 0.87 0.55 0.99 0.85 0.96 1.06 0.59 1.27 0.93 Total 98.97 100.41 100.37 99.99 100.66 100.23 100.07 100.16 99.17 98.75 100.10 99.93 100.03 100.18 K2O+ Na2O 8.37 8.58 6.22 6.63 5.39 6.45 7.26 9.34 10.50 9.78 8.56 7.20 7.75 7.24 A/CNK 0.80 1.12 0.85 1.19 1.11 0.87 0.82 1.07 0.95 0.95 1.06 1.14 1.32 1.18 La 39.46 28.16 21.35 27.63 19.87 20.71 24.73 39.73 43.77 42.84 30.80 17.14 34.98 23.21 Ce 84.90 71.16 43.93 55.99 40.26 43.38 48.48 81.41 89.85 88.44 61.76 35.72 65.95 47.83 Pr 11.59 8.45 6.57 7.68 5.46 6.46 6.42 10.58 11.71 11.33 7.16 4.47 7.58 6.43 Nd 46.82 34.88 28.21 31.08 24.19 27.62 25.43 42.81 43.98 42.58 26.36 18.23 28.14 27.12 Sm 8.05 6.93 5.46 5.53 4.85 5.38 4.45 8.11 8.05 7.85 4.56 4.00 4.84 5.91 Eu 2.47 2.13 1.77 2.17 1.47 2.11 2.11 1.67 2.11 1.92 0.74 0.59 0.87 1.26 Gd 6.08 5.20 4.52 4.43 3.72 4.51 3.77 6.35 6.89 6.49 3.53 3.36 3.98 5.10 Tb 0.80 0.70 0.66 0.55 0.57 0.68 0.50 1.01 1.03 1.00 0.57 0.66 0.63 0.91 Dy 4.07 3.63 3.50 2.64 2.69 3.61 2.60 5.08 6.24 6.01 2.97 3.74 3.25 5.37 Ho 0.68 0.67 0.68 0.50 0.59 0.72 0.48 1.00 1.14 1.10 0.56 0.88 0.68 1.19 Er 1.75 1.83 1.66 1.24 1.59 1.84 1.26 2.80 3.06 3.03 1.77 2.64 2.02 2.92 Tm 0.27 0.25 0.28 0.21 0.25 0.32 0.20 0.49 0.53 0.53 0.33 0.50 0.38 0.51 Yb 1.60 1.75 1.71 1.32 1.52 1.99 1.28 3.11 3.35 3.42 2.40 3.27 2.38 3.95 Lu 0.21 0.23 0.24 0.19 0.24 0.28 0.17 0.48 0.47 0.50 0.36 0.54 0.36 0.53 Y 16.49 16.88 19.40 15.66 12.97 20.48 12.71 25.72 29.74 28.30 17.22 23.55 18.45 31.20 ΣREE 208.75 165.97 120.55 141.15 107.25 119.62 121.88 204.63 222.17 217.05 143.86 95.73 156.03 132.23 (La/Yb)N 17.64 11.55 8.96 14.97 9.41 7.48 13.87 9.17 9.37 9.00 9.22 3.76 10.54 4.22 δEu 1.04 1.04 1.06 1.29 1.02 1.28 1.53 0.69 0.85 0.80 0.54 0.48 0.59 0.69 Li 9.65 72.16 8.03 19.76 33.02 5.56 8.45 17.31 13.25 18.52 17.71 2.74 21.47 11.94 Be 1.46 4.57 0.84 1.28 1.24 0.84 0.94 2.31 2.51 2.88 2.23 0.87 1.81 1.30 Th 5.61 10.32 6.59 16.10 8.80 12.04 9.27 10.92 8.22 11.48 11.23 7.90 6.94 7.28 U 1.18 1.89 0.79 2.44 0.82 1.07 1.75 3.60 2.49 4.05 3.48 1.93 2.62 2.37 Hf 4.54 5.35 3.74 5.09 9.96 5.78 6.03 12.23 8.61 9.74 9.88 4.71 5.51 6.09 Ta 0.25 0.49 0.31 0.63 0.37 0.46 0.33 1.05 0.34 0.72 1.22 0.92 0.99 1.02 Sc 13.12 19.71 13.29 9.78 13.84 11.88 9.67 6.73 7.72 6.96 3.44 4.18 5.13 7.45 Ba 829 827 550 1 100 460 663 882 1 056 1 162 1 103 1 045 1 417 769 772 Nb 3.35 8.28 6.39 6.39 4.30 6.44 6.29 11.24 15.33 15.12 10.69 9.11 9.52 9.97 Rb 31 63 33 41 24 33 56 116 99 120 129 77 84 65 Sr 1814 960 937 778 995 798 706 384 295 360 246 109 308 74 Zr 150 185 119 177 147 166 162 409 403 418 245 166 236 213 Co 20.81 31.66 22.74 19.05 27.21 19.46 15.82 8.57 5.00 6.09 7.70 4.63 6.00 0.91 V 148.0 161.4 176.8 93.0 112.7 133.9 93.2 39.7 31.8 38.7 23.3 12.4 31.1 17.6 (La/Sm)N 3.17 2.62 2.53 3.22 2.65 2.48 3.59 3.16 3.51 3.52 4.36 2.77 4.67 2.54 Ba/Th 147.7 80.11 83.39 68.33 52.29 55.08 95.16 96.71 141.38 96.06 93.11 179.26 110.75 105.97 La/Nb 11.78 3.40 3.34 4.32 4.62 3.22 3.93 3.53 2.86 2.83 2.88 1.88 3.67 2.33 La/Ba 0.05 0.03 0.04 0.03 0.04 0.03 0.03 0.04 0.04 0.04 0.03 0.01 0.05 0.03 Sm/Yb 5.01 3.96 3.19 4.18 3.20 2.71 3.48 2.61 2.40 2.30 1.90 1.22 2.03 1.50 Sm/Th 1.43 0.67 0.83 0.34 0.55 0.45 0.48 0.74 0.98 0.68 0.41 0.51 0.70 0.81 Th/Y 0.34 0.61 0.34 1.03 0.68 0.59 0.73 0.42 0.28 0.41 0.65 0.34 0.38 0.23 
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表 2 晚三叠世哈达陶勒盖组火山岩LA-ICP-MS锆石U-Pb测年数据
Table 2. LA-ICP-MS Zircon U-Pb data for the volcanic rocks from Late Triassic Hadataolegai Fm.
测点号 Th/U 同位素比值 同位素年龄(Ma) 207Pb/206Pb ±1δ 206Pb/238U ±1δ 207Pb/235U ±1δ 207Pb/206Pb ±1δ 206Pb/238U ±1δ 207Pb/235U ±1δ DH2011RZ11：安粗岩 DH2011RZ11_3 0.67 0.058 1 0.003 4 0.031 0 0.000 8 0.227 3 0.014 8 532 123 197 5 208 12 DH2011RZ11_5 0.75 0.049 7 0.001 7 0.032 8 0.000 7 0.230 4 0.008 6 180 78 208 4 211 7 DH2011RZ11_7 0.85 0.051 8 0.002 1 0.033 4 0.000 7 0.239 0 0.011 0 277 92 212 5 218 9 DH2011RZ11_9 0.84 0.051 5 0.001 6 0.032 7 0.000 7 0.235 7 0.008 1 264 71 208 4 215 7 DH2011RZ11_10 0.96 0.052 1 0.001 5 0.033 2 0.000 7 0.233 0 0.006 9 288 62 211 4 213 6 DH2011RZ11_12 0.69 0.054 0 0.002 1 0.035 3 0.000 8 0.243 2 0.010 2 371 83 223 5 221 8 DH2011RZ11_13 0.80 0.051 6 0.001 4 0.036 0 0.000 7 0.254 6 0.007 1 267 59 228 4 230 6 DH2011RZ11_15 1.59 0.051 4 0.001 3 0.031 3 0.000 6 0.224 5 0.006 1 261 58 199 4 206 5 DH2011RZ11_17 0.76 0.053 7 0.002 3 0.031 3 0.000 7 0.222 0 0.010 5 360 93 199 4 204 9 DH2011RZ11_18 0.89 0.049 6 0.001 9 0.032 9 0.000 7 0.225 1 0.009 7 177 88 208 4 206 8 DH2011RZ11_19 0.97 0.051 5 0.001 7 0.034 2 0.000 7 0.255 2 0.009 4 265 75 217 4 231 8 DH2011RZ11_20 0.88 0.048 0 0.001 8 0.033 2 0.000 7 0.214 6 0.008 8 97 88 211 4 197 7 DH2011RZ11_22 0.65 0.052 9 0.001 7 0.034 0 0.000 7 0.243 3 0.008 3 323 70 216 4 221 7 DH2011RZ11_23 0.89 0.049 4 0.001 7 0.033 8 0.000 7 0.228 9 0.008 5 165 78 215 4 209 7 DH2011RZ11_24 1.24 0.050 8 0.001 8 0.032 3 0.000 7 0.236 3 0.009 2 231 80 205 4 215 8 DH2011RZ11_26 0.79 0.055 0 0.001 4 0.032 1 0.000 6 0.233 7 0.006 4 410 57 204 4 213 5 DH2011RZ11_27 0.85 0.051 4 0.001 4 0.033 2 0.000 7 0.234 0 0.006 6 259 61 210 4 214 5 DH2011RZ11_28 0.77 0.050 7 0.001 6 0.034 1 0.000 7 0.239 9 0.008 3 226 72 216 4 218 7 DH2011RZ11_29 0.94 0.048 9 0.001 4 0.033 0 0.000 7 0.223 8 0.006 8 143 66 209 4 205 6 DH2011RZ11_30 0.82 0.049 6 0.001 4 0.033 2 0.000 7 0.230 0 0.007 1 178 66 211 4 210 6 DH2011RZ11_34 0.57 0.049 4 0.001 8 0.034 3 0.000 7 0.227 2 0.009 0 166 82 218 4 208 7 DH2011RZ11_35 0.70 0.050 4 0.001 6 0.035 1 0.000 7 0.244 3 0.008 2 212 71 223 4 222 7 DH2011RZ17：安山岩 DH2011RZ17_1 0.74 0.051 0 0.001 4 0.033 6 0.000 7 0.242 3 0.007 2 242 63 213 4 220 6 DH2011RZ17_2 0.87 0.052 6 0.001 6 0.034 4 0.000 7 0.246 4 0.008 2 313 68 218 4 224 7 DH2011RZ17_3 0.77 0.052 2 0.001 5 0.034 8 0.000 7 0.252 3 0.008 1 293 66 221 4 228 7 DH2011RZ17_4 0.87 0.051 6 0.001 7 0.034 5 0.000 7 0.236 7 0.008 4 267 73 219 4 216 7 DH2011RZ17_5 0.81 0.051 0 0.001 5 0.035 5 0.000 7 0.252 4 0.008 1 239 66 225 5 229 7 DH2011RZ17_6 0.77 0.050 2 0.002 2 0.032 1 0.000 7 0.218 3 0.010 9 205 101 204 5 201 9 DH2011RZ17_7 0.81 0.049 7 0.001 6 0.033 2 0.000 7 0.233 6 0.008 4 181 75 211 4 213 7 DH2011RZ17_8 1.14 0.052 4 0.001 2 0.032 4 0.000 6 0.229 8 0.005 7 301 53 206 4 210 5 DH2011RZ17_9 0.95 0.050 2 0.001 3 0.032 9 0.000 7 0.230 6 0.006 5 206 61 209 4 211 5 DH2011RZ17_11 0.79 0.050 3 0.001 3 0.035 7 0.000 7 0.251 2 0.006 8 209 58 226 4 228 5 DH2011RZ17_13 0.66 0.050 0 0.001 6 0.034 3 0.000 7 0.240 3 0.008 4 195 73 218 4 219 7 DH2011RZ17：安山岩 DH2011RZ17_15 0.88 0.049 8 0.001 3 0.033 4 0.000 7 0.232 9 0.006 4 188 60 212 4 213 5 DH2011RZ17_17 0.78 0.051 6 0.001 4 0.036 3 0.000 7 0.255 6 0.007 1 268 59 230 4 231 6 DH2011RZ17_18 0.72 0.052 0 0.001 7 0.032 8 0.000 7 0.231 6 0.008 0 284 71 208 4 212 7 DH2011RZ17_19 0.77 0.049 9 0.001 8 0.033 6 0.000 7 0.236 8 0.009 1 191 80 213 4 216 8 DH2011RZ17_20 0.68 0.052 9 0.001 5 0.035 2 0.000 7 0.248 7 0.007 7 323 64 223 4 226 6 DH2011RZ17_22 0.78 0.051 4 0.001 4 0.034 1 0.000 7 0.244 3 0.007 0 259 61 216 4 222 6 DH2011RZ17_23 0.63 0.048 6 0.003 1 0.033 7 0.000 9 0.228 2 0.016 4 127 142 214 6 209 14 DH2011RZ17_24 0.67 0.051 2 0.001 8 0.034 8 0.000 7 0.249 7 0.009 6 249 78 221 5 226 8 DH2011RZ17_25 0.76 0.053 8 0.001 8 0.036 9 0.000 8 0.256 9 0.009 2 363 72 233 5 232 7 DH2011RZ17_26 0.78 0.049 3 0.001 7 0.033 8 0.000 7 0.225 1 0.008 5 162 79 214 4 206 7 DH2011RZ17_29 0.94 0.054 9 0.001 8 0.033 7 0.000 7 0.244 2 0.008 8 408 71 214 4 222 7 DH2011RZ17_30 0.87 0.050 1 0.001 8 0.035 1 0.000 8 0.244 0 0.009 8 201 82 222 5 222 8 DH2011RZ17_32 0.79 0.049 5 0.001 6 0.034 3 0.000 7 0.237 6 0.008 3 171 73 217 4 216 7 TW04：石英粗安岩 TW04_3 1.94 0.050 5 0.001 3 0.035 0 0.000 8 0.246 3 0.006 6 217 57 222 5 224 5 TW04_5 2.37 0.053 9 0.002 3 0.034 5 0.000 8 0.270 0 0.012 9 368 92 219 5 243 10 TW04_6 3.18 0.054 7 0.003 1 0.034 5 0.000 9 0.267 8 0.017 5 400 122 218 6 241 14 TW04_7 2.15 0.051 0 0.001 5 0.035 3 0.000 8 0.247 3 0.007 8 238 65 224 5 224 6 TW04_8 2.13 0.052 5 0.002 0 0.034 4 0.000 8 0.244 0 0.010 3 309 85 218 5 222 8 TW04_9 2.39 0.051 8 0.002 8 0.034 0 0.000 8 0.245 5 0.014 8 275 120 216 5 223 12 TW04_10 2.18 0.051 9 0.002 8 0.035 4 0.000 9 0.247 8 0.015 1 283 121 224 5 225 12 TW04_12 1.98 0.054 4 0.001 6 0.034 6 0.000 8 0.264 7 0.008 3 388 62 219 5 239 7 TW04_13 2.07 0.052 3 0.001 3 0.033 9 0.000 8 0.247 4 0.006 7 300 57 215 5 224 5 TW04_14 2.29 0.056 9 0.002 0 0.033 9 0.000 8 0.266 0 0.010 3 487 76 215 5 240 8 TW04_16 2.30 0.051 8 0.002 0 0.035 6 0.000 9 0.263 6 0.011 4 274 86 225 5 238 9 TW04_17 1.86 0.050 8 0.001 2 0.033 8 0.000 8 0.241 4 0.006 0 229 54 215 5 220 5 TW04_19 2.29 0.055 6 0.001 5 0.033 2 0.000 8 0.261 7 0.007 6 435 59 210 5 236 6 TW04_21 2.13 0.052 2 0.002 0 0.035 7 0.000 8 0.259 1 0.011 0 292 83 226 5 234 9 TW04_22 1.64 0.050 5 0.001 3 0.034 5 0.000 8 0.246 2 0.006 6 219 57 219 5 224 5 TW04_23 1.89 0.050 8 0.001 4 0.033 8 0.000 8 0.245 0 0.007 1 230 61 214 5 223 6 TW04_24 2.27 0.054 2 0.001 6 0.033 7 0.000 8 0.263 5 0.008 5 379 64 214 5 238 7 TW04_25 2.61 0.052 2 0.001 7 0.033 9 0.000 8 0.252 2 0.009 2 295 73 215 5 228 7 TW04_26 1.86 0.051 3 0.001 3 0.033 4 0.000 8 0.245 3 0.006 7 253 58 212 5 223 5 TW04_27 2.41 0.051 1 0.001 5 0.033 3 0.000 8 0.238 3 0.007 6 246 66 211 5 217 6 TW04_28 1.40 0.051 3 0.001 2 0.034 3 0.000 8 0.250 4 0.006 1 255 53 218 5 227 5 TW04：石英粗安岩 TW04_29 1.74 0.028 1 0.001 8 0.033 4 0.000 8 0.137 6 0.008 9 212 53 212 5 131 8 TW13：流纹岩 TW13_1 2.60 0.051 1 0.002 6 0.036 6 0.001 0 0.274 9 0.016 4 244 115 231 6 247 13 TW13_2 2.74 0.052 2 0.001 8 0.036 8 0.001 0 0.260 7 0.010 5 296 78 233 6 235 8 TW13_3 3.46 0.056 6 0.004 3 0.036 7 0.001 1 0.278 9 0.024 5 477 160 232 7 250 19 TW13_4 1.91 0.051 5 0.002 6 0.036 7 0.001 0 0.259 7 0.015 0 264 111 232 6 234 12 TW13_5 2.23 0.053 5 0.003 9 0.035 7 0.001 1 0.261 9 0.021 7 348 155 226 7 236 17 TW13_6 2.47 0.051 3 0.003 0 0.038 2 0.001 1 0.266 5 0.017 7 256 130 242 7 240 14 TW13_7 2.00 0.050 9 0.003 0 0.038 2 0.001 1 0.269 3 0.018 0 235 129 242 7 242 14 TW13_8 1.82 0.054 6 0.002 4 0.038 1 0.001 0 0.286 6 0.014 6 396 95 241 6 256 12 TW13_9 3.51 0.053 2 0.003 7 0.036 8 0.001 1 0.278 8 0.023 0 336 151 233 7 250 18 TW13_10 2.19 0.053 7 0.002 7 0.037 1 0.001 0 0.275 1 0.015 8 357 109 235 6 247 13 TW13_11 2.04 0.068 1 0.001 9 0.036 4 0.001 0 0.341 4 0.011 2 871 57 231 6 298 8 TW13_12 2.60 0.050 4 0.001 7 0.036 3 0.001 0 0.254 6 0.010 0 211 77 230 6 230 8 TW13_13 3.02 0.064 8 0.002 4 0.036 6 0.001 0 0.326 7 0.014 2 766 75 232 6 287 11 TW13_14 2.45 0.054 1 0.002 8 0.035 3 0.001 0 0.272 8 0.016 0 375 110 224 6 245 13 TW13_15 2.66 0.051 9 0.002 8 0.036 8 0.001 0 0.259 7 0.016 0 279 119 233 6 234 13 TW13_16 1.73 0.052 5 0.002 9 0.035 6 0.001 0 0.259 8 0.016 8 309 122 226 6 235 14 TW13_17 3.38 0.050 9 0.001 9 0.036 6 0.001 0 0.263 9 0.011 2 238 83 232 6 238 9 TW13_18 2.29 0.055 7 0.004 7 0.035 4 0.001 1 0.274 0 0.026 6 442 176 224 7 246 21 TW13_19 3.73 0.051 7 0.002 9 0.036 0 0.001 0 0.264 5 0.017 2 270 123 228 6 238 14 TW13_20 1.87 0.050 8 0.001 4 0.037 1 0.001 0 0.257 8 0.007 9 232 61 235 6 233 6 TW13_21 2.76 0.055 1 0.003 5 0.036 6 0.001 1 0.279 0 0.020 0 417 135 232 7 250 16 TW13_22 2.22 0.051 0 0.001 8 0.036 8 0.001 0 0.257 9 0.010 2 239 78 233 6 233 8 TW13_23 3.14 0.050 1 0.002 6 0.036 1 0.001 0 0.252 6 0.014 4 199 114 229 6 229 12 TW13_24 1.96 0.049 5 0.001 5 0.037 4 0.001 0 0.261 0 0.008 7 170 67 236 6 236 7 TW13_25 3.01 0.055 2 0.002 2 0.035 1 0.001 0 0.267 1 0.012 1 419 85 222 6 240 10 TW13_26 2.89 0.053 2 0.001 9 0.035 7 0.001 0 0.257 0 0.010 4 336 79 226 6 232 8 TW13_27 1.92 0.049 7 0.001 3 0.036 2 0.001 0 0.247 4 0.007 5 182 62 229 6 225 6 TW13_28 1.94 0.052 0 0.001 5 0.035 3 0.000 9 0.259 0 0.008 2 285 63 224 6 234 7 TW13_29 2.34 0.055 1 0.002 3 0.034 8 0.000 9 0.282 0 0.013 4 417 89 220 6 252 11 TW13_30 2.12 0.053 1 0.001 7 0.035 4 0.000 9 0.259 7 0.009 4 333 71 224 6 234 8
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