Petrogenesis and Geodynamic Setting of Late Triassic Quartz Diorites in Zhiduo Area, Qinghai Province
-
摘要: 对羌塘地块东北缘甘孜-理塘缝合带南侧日啊日曲石英闪长岩进行了系统的锆石U-Pb年龄、主量-微量元素及Sr-Nd同位素分析, 以探讨其岩石成因及地球动力学意义.LA-ICP-MS锆石U-Pb定年结果表明, 石英闪长岩侵位年龄为218±1 Ma, 为晚三叠世岩浆活动的产物.岩石SiO2含量介于53.02%~62.06%之间, 富Al2O3(15.84%~17.00%)和CaO(6.71%~8.94%), 贫TiO2(0.49%~1.01%)和P2O5(0.04%~0.12%), 具有较高的MgO(3.31%~5.66%)和Mg#(50~62), 属准铝质钙碱性系列; 岩体稀土元素总量较低(38.05×10-6~61.58×10-6), 轻重稀土分馏不明显, LILE富集, HFSE亏损, 具有含量较高的Cr(33.45×10-6~176.64×10-6)和Ni(13.34×10-6~43.62×10-6).全岩(87Sr/86Sr)i比值较为一致(0.706 8~0.707 9), εNd(t)变化于-5.5~-1.6.主微量元素及同位素结果表明日啊日曲石英闪长岩具有高镁闪长岩的特征, 与赞岐岩地球化学特征类似, 为俯冲沉积物来源的熔体交代岩石圈地幔形成的尖晶石相金云母二辉橄榄岩低度(10%~15%)部分熔融的产物, 岩浆演化过程中经历了辉石、角闪石等矿物的分离结晶.微量元素构造判别图解表明岩石为俯冲环境下的弧岩浆岩, 结合区内蛇绿岩、研究区南部陆缘弧火山岩和义敦岛弧埃达克岩的发现, 认为古特提斯洋在晚三叠世时期可能仍处于消减状态, 日啊日曲高镁石英闪长岩形成于甘孜-理塘洋南西向俯冲过程中.Abstract: Zircon U-Pb age, major and trace elements and Sr, Nd isotope compositions of the Riariqu quartz diorites from the south of the Ganzi-Litang suture zone, northeastern Qiangtang terrane are studied to decipher its petrogenesis and geodynamic significance. LA-ICP-MS zircon U-Pb dating yields an emplacement age of 218±1 Ma for the intrusion. Bulk-rock analyses show that these rocks belong to the calc-alkaline series, with SiO2 contents ranging from 53.02% to 62.06%. They are enriched in Al2O3 (15.84%-17.00%) and CaO (6.71%-8.94%), depleted in TiO2 (0.49%-1.01%) and P2O5 (0.04%-0.12%), defining their metaluminous characteristics. All samples have high concentrations of MgO (3.31%-5.66%), Cr (33.45×10-6-176.64×10-6) and Ni (13.34×10-6-43.62×10-6), and resultant high Mg# (50-62). These rocks are enriched in LREE and LILE, and depleted in HFSE with low REE contents (38.05×10-6-61.58×10-6). The (87Sr/86Sr)i ratios range from 0.706 8 to 0.707 9, and εNd(t) values vary from -5.5 to -1.6. The geochemical and Sr-Nd isotopic compositions of the Riariqu quartz diorites are similar to those of high-Mg dioritoids/sanukitoids. We contend that the Riariqu quartz diorites were derived from low-degree partial melting (10%-15%) of a phlogopite-bearing spinel lherzolite mantle, which was metasomatized by sediment-derived melts. Fractional crystallization of pyroxene and amphibole might also occur during the magma evolution. The geochemical characteristics indicate that the Riariqu quartz diorites are arc-related magmatic rocks, and were generated in a subduction-related tectonic setting. Combined with the ophiolites and continental marginal arc lavas in the study area, and the regional adakites in the Yidun terrane, it is suggested that the Riariqu quartz diorites might be generated during the southwestward subduction of Ganzi-Litang Paleo-Tethys Ocean in the Late Triassic.
-
图 1 青藏高原构造轮廓及三叠纪岩浆岩时空分布(a)和羌塘地块东北缘治多地区地质简图(b)
1.新近纪-第四纪沉积物；2.晚三叠世巴塘群碳酸盐岩组；3.晚三叠世巴塘群火山岩组；4.晚三叠世巴塘群碎屑岩组；5.中三叠-晚三叠世巴颜喀拉山群砂岩组；6.三叠纪查涌蛇绿混杂岩带；7.石炭-早中二叠世多彩蛇绿混杂岩带；8.晚三叠世中酸性侵入岩体；9.断层；10.采样位置；a图据Yin and Harrison, 2000; Chung et al., 2005修改
Fig. 1. Simplified tectonic map of the Tibetan plateau showing the temporal-spatial distribution of Triassic arc magmatic rocks (a) and regional geological map of the Zhiduo area (b)
图 2 治多地区日啊日曲石英闪长岩显微照片(正交偏光)
Pl.斜长石；Amp.角闪石；Bi.黑云母；Q.石英
Fig. 2. Microphotographs of the Riariqu quartz diorite from Zhiduo area
图 3 治多地区日啊日曲石英闪长岩(GS2)中锆石阴极发光(CL)图像(a)、U-Pb年龄谐和图(b)和球粒陨石标准化稀土配分图(c)
图a中圆圈代表U-Pb年龄测试激光剥蚀点位；圈中数字为分析点号，编号同表 1，圈外年龄为206Pb/238U表面年龄
Fig. 3. Cathodoluminescence (CL) images (a), U-Pb concordia diagram (b) and Chondrite-normalized REE patterns (c) for zircons of Riariqu quartz diorite sample (GS2) from Zhiduo area
图 4 治多地区日啊日曲石英闪长岩(a)TAS分类图、(b)K2O-SiO2关系图、(c)A/NK-A/CNK关系图和(d)MgO-SiO2关系图
数据来源：日本岛弧Steouchi火山岩带新生代赞岐岩(Tatsumi and Ishizaka, 1982; Shimoda et al., 1998; Tatsumi et al., 2003)；可可西里晚三叠世高镁安山岩(Wang et al., 2011b)；义敦岛弧晚三叠世埃达克岩(Wang et al., 2011a)；a图据Wilson, 1989；b图据Rollinson, 1993；c图据Maniar and Piccoli, 1989；d图据McCarron and Smellie, 1998
Fig. 4. Major-element plots for the Riariqu quartz diorite from Zhiduo area (a) Total alkalis vs.silica (TAS) diagram, (b) K2O vs.SiO2 diagram, (c) A/NK vs.A/CNK diagram, (d) MgO vs.SiO2 diagram
图 5 治多地区日啊日曲石英闪长岩球粒陨石标准化稀土配分曲线(a)和原始地幔标准化微量元素蛛网图(b)
图中岩浆岩数据来源同图 4；球粒陨石和原始地幔标准化数据引自Sun and McDonough, 1989
Fig. 5. Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element patterns (b) for the Riariqu quartz diorite from Zhiduo area
图 6 治多地区日啊日曲石英闪长岩εNd(t)-(87Sr/86Sr)i
数据来源：MORB和海相沉积物(Plank and Langmuir, 1998)；义敦岛弧晚三叠世昌台玄武岩(Wang et al., 2013)；其他岩浆岩数据同图 4
Fig. 6. Initial 87Sr/86Sr vs. εNd(t) values for the Riariqu quartz diorite from Zhiduo area
图 7 治多地区日啊日曲石英闪长岩(a)Ba/La-La/Yb和(b)Th/Yb-Th/Sm
数据来源：MORB(N-MORB据Sun and McDonough, 1989)；沱沱河地区晚三叠世富Nb玄武岩(Wang et al., 2008)；其他岩浆岩数据同图 4和6；a图据Yogodzinski et al., 1995；b图据Zheng et al., 2014
Fig. 7. Trace-element plots for the Riariqu quartz diorite from Zhiduo area (a) Ba/La vs.La/Yb diagram and (b) Th/Yb vs.Th/Sm diagrams
图 8 治多地区日啊日曲石英闪长岩Rb/Sr-Ba/Rb(a)和Yb-La/Yb(b)
图a据Furman and Graham(1999)；图b中带短横线曲线为地幔岩浆熔融程度趋势线，两端元分别为含金云母尖晶石相二辉橄榄岩地幔源区和含金云母石榴石相二辉橄榄岩地幔源区.图中所有地幔成分参考数据Miller et al.(1999)及其文献；富集地幔源区组分La=0.648×10-6，Yb=0.347×10-6，Dy=0.578×10-6
Fig. 8. Rb/Sr vs.Ba/Rb (a) and Yb vs.La/Yb (b) diagrams for the Riariqu quartz diorite from Zhiduo area
图 9 治多地区日啊日曲石英闪长岩Nb-Y(a)和Rb-Y+Nb构造判别(b)
图中岩浆岩数据来源同图 4；syn-COLG.同碰撞花岗岩；WPG.板内花岗岩；VAG.火山弧花岗岩；ORG.洋中脊花岗岩；底图据Pearce et al., 1984
Fig. 9. Nb vs.Y and Rb vs.Y +Nb discrimination diagrams for the quartz diorite from Zhiduo area
图 10 晚三叠世甘孜-理塘古特提斯洋俯冲构造演化模式
Fig. 10. A suggested model for the evolution of Ganzi-Litang Paleo-Tethys Ocean during Late Triassic
表 1 治多地区日啊日曲石英闪长岩(GS2)锆石LA-ICP-MS U-Pb定年分析结果
Table 1. LA-ICP-MS zircon U-Pb dating results of the Riariqu quartz diorite sample (GS2) from Zhiduo area
测试点号 Pb(10-6) Th(10-6) U(10-6) Th/U U-Th-Pb同位素比值 年龄(Ma) 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 208Pb/232Th 1σ 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ GS2-1 281 906 850 1.07 0.050 1 0.001 3 0.235 1 0.006 3 0.034 0 0.000 4 0.010 8 0.000 3 198 29 214 5 216 2 GS2-2 267 821 843 0.97 0.051 4 0.001 3 0.242 5 0.006 1 0.034 1 0.000 3 0.010 7 0.000 2 257 59 220 5 216 2 GS2-3 199 622 894 0.70 0.052 4 0.001 3 0.246 5 0.006 1 0.033 9 0.000 3 0.010 3 0.000 2 302 49 224 5 215 2 GS2-4 289 873 868 1.01 0.050 9 0.001 3 0.242 0 0.006 1 0.034 4 0.000 3 0.010 9 0.000 2 235 64 220 5 218 2 GS2-5 202 631 711 0.89 0.050 6 0.001 5 0.240 6 0.007 3 0.034 5 0.000 4 0.010 7 0.000 3 233 70 219 6 219 2 GS2-6 203 630 764 0.82 0.050 3 0.001 3 0.239 6 0.006 2 0.034 4 0.000 4 0.010 5 0.000 3 209 92 218 5 218 2 GS2-7 253 780 1 096 0.71 0.050 8 0.001 3 0.242 7 0.006 4 0.034 6 0.000 4 0.010 8 0.000 4 232 64 221 5 219 2 GS2-8 442 1 378 1 315 1.05 0.051 0 0.001 1 0.244 3 0.004 7 0.034 7 0.000 3 0.010 0 0.000 4 243 48 222 4 220 2 GS2-9 147 419 638 0.66 0.050 6 0.001 3 0.241 8 0.006 4 0.034 6 0.000 4 0.010 9 0.000 7 233 61 220 5 219 2 GS2-10 99 295 442 0.67 0.050 2 0.001 6 0.240 1 0.007 8 0.034 8 0.000 4 0.010 0 0.000 7 211 76 218 6 220 3 GS2-11 255 721 1 036 0.70 0.049 0 0.001 2 0.255 9 0.006 6 0.037 7 0.000 4 0.011 2 0.000 8 146 62 231 5 238 2 GS2-12 117 357 435 0.82 0.050 8 0.002 6 0.234 8 0.010 6 0.033 9 0.000 4 0.009 8 0.000 6 232 112 214 9 215 3 GS2-13 285 890 872 1.02 0.051 3 0.001 3 0.247 2 0.006 5 0.034 8 0.000 3 0.010 0 0.000 5 257 64 224 5 220 2 GS2-14 178 509 614 0.83 0.050 4 0.001 5 0.259 3 0.008 1 0.037 2 0.000 4 0.012 4 0.000 7 213 72 234 7 235 3 GS2-15 514 1 673 1 287 1.30 0.049 5 0.001 6 0.233 7 0.005 9 0.034 3 0.000 4 0.010 2 0.000 3 172 81 213 5 217 2 GS2-16 196 621 709 0.88 0.049 7 0.001 6 0.237 1 0.007 7 0.034 4 0.000 4 0.010 4 0.000 3 189 76 216 6 218 2 GS2-17 126 384 512 0.75 0.050 3 0.001 4 0.239 9 0.006 5 0.034 6 0.000 3 0.010 6 0.000 3 209 65 218 5 219 2 GS2-18 179 572 601 0.95 0.050 9 0.001 5 0.243 7 0.006 9 0.034 6 0.000 3 0.010 4 0.000 3 235 65 221 6 219 2 GS2-19 87 271 389 0.70 0.050 6 0.001 5 0.244 2 0.007 5 0.034 8 0.000 4 0.010 5 0.000 3 233 73 222 6 220 2 
下载: 导出CSV
表 2 治多地区日啊日曲石英闪长岩(GS2)锆石微量元素分析结果(10-6)
Table 2. Zircon trace element data of the Riariqu quartz diorite sample (GS2) from Zhiduo area
测试点号 La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Eu/Eu* Hf Ta Y Ti Nb GS2-1 0.03 20.90 0.50 7.87 13.40 4.57 70.40 22.60 298 116.00 583 140.00 1 497 298 0.37 12 365 0.80 3 746 5.48 2.50 GS2-2 0.10 22.60 0.64 10.30 14.80 5.01 68.90 21.10 283 111.00 569 143.00 1 602 334 0.40 11 841 0.84 3 666 6.67 2.50 GS2-3 0.00 15.60 0.07 1.50 4.11 1.35 28.10 10.80 165 73.40 396 95.90 1 032 215 0.28 11 888 0.76 2 376 5.28 1.70 GS2-4 0.04 21.70 0.57 8.37 14.80 4.94 70.10 22.40 290 111.00 545 130.00 1 369 270 0.39 12 369 0.73 3 568 7.67 2.08 GS2-5 0.03 17.00 0.54 6.46 11.70 3.90 52.80 17.50 228 89.60 449 111.00 1 204 247 0.40 11 732 0.69 2 910 6.74 1.85 GS2-6 0.05 18.10 0.42 5.69 10.40 3.52 49.80 17.20 240 97.20 520 130.00 1 460 305 0.39 10 940 0.77 3 234 6.94 2.32 GS2-7 0.07 20.10 0.31 5.41 9.58 2.72 53.30 18.10 253 107.00 565 138.00 1 511 320 0.29 10 586 1.02 3 470 6.50 2.18 GS2-8 0.09 31.40 0.84 12.80 21.40 6.90 100.00 32.20 423 165.00 822 200.00 2 218 447 0.38 12 901 1.15 4 790 5.68 3.20 GS2-9 2.21 15.80 0.58 4.58 5.90 2.03 31.40 11.20 158 67.80 368 95.10 1 113 234 0.37 12 987 0.69 1 989 6.22 1.38 GS2-10 0.04 9.71 0.16 2.80 3.89 1.49 25.00 8.60 126 55.10 303 79.90 917 196 0.35 11 190 0.47 1 813 5.75 1.32 GS2-11 0.02 21.20 0.09 1.30 3.13 1.25 29.80 12.30 192 83.40 439 105.00 1 111 222 0.26 13 350 1.31 2 660 8.02 3.27 GS2-12 0.03 10.30 0.23 3.79 6.66 2.06 34.60 11.60 159 64.50 338 85.30 965 199 0.34 11 889 0.49 2 096 4.47 1.27 GS2-13 0.01 21.90 0.47 7.93 11.80 4.25 65.20 21.10 287 112.00 566 137.00 1 484 298 0.37 12 008 0.75 3 580 6.53 2.11 GS2-14 0.01 13.60 0.34 4.88 9.21 3.27 46.60 15.60 205 81.20 418 102.00 1 143 231 0.39 12 122 0.74 2 648 4.13 1.57 GS2-15 0.18 44.20 1.44 20.50 32.10 9.52 145.00 45.50 578 216.00 1 015 235.00 2 411 460 0.36 11 626 1.04 6 705 9.44 4.26 GS2-16 0.06 17.20 0.38 5.64 11.30 3.59 57.70 18.80 255 102.00 526 129.00 1 421 288 0.35 11 806 0.72 3 316 8.72 1.95 GS2-17 0.04 10.70 0.29 3.69 5.86 2.37 31.80 10.60 146 59.80 313 77.10 859 178 0.42 12 288 0.56 1 948 5.35 1.16 GS2-18 0.04 15.20 0.35 6.18 10.50 3.44 53.20 17.30 231 90.00 450 110.00 1 203 241 0.36 11 473 0.61 2 874 6.12 1.61 GS2-19 0.02 8.59 0.21 4.13 6.64 2.11 31.30 10.10 135 53.90 279 69.50 776 161 0.37 11 981 0.38 1 763 4.68 0.80
下载: 导出CSV
表 3 治多地区日啊日曲石英闪长岩主量元素(%)、微量及稀土元素(10-6)分析结果
Table 3. Major (%) and trace element (10-6) compositions of the Riariqu quartz diorites from Zhiduo area
样号 SC-2 SC-3 SC-4 SC-6 SC-8 SiO2 62.06 57.96 53.02 57.43 57.50 TiO2 0.59 0.51 1.01 0.49 0.69 Al2O3 15.93 15.84 16.94 17.00 16.75 Fe2O3T 6.56 6.81 9.36 6.30 7.13 MnO 0.13 0.14 0.18 0.14 0.14 MgO 3.31 5.66 5.06 5.06 4.55 CaO 6.71 8.54 8.94 7.91 8.07 Na2O 2.94 2.34 2.56 2.69 2.84 K2O 0.92 0.94 1.27 1.13 0.92 P2O5 0.07 0.06 0.04 0.05 0.12 LOI 0.60 1.36 1.58 1.18 1.43 Total 99.82 100.16 99.96 99.38 100.14 A/CNK 0.88 0.78 0.78 0.85 0.82 K2O/Na2O 0.31 0.40 0.50 0.42 0.32 Na2O+K2O 3.86 3.28 3.83 3.82 3.76 Mg# 50.00 62.00 52.00 61.00 55.00 La 8.70 8.40 8.80 7.30 11.20 Ce 20.40 16.70 14.10 13.60 21.90 Pr 2.78 2.07 1.70 1.56 2.70 Nd 11.70 8.60 6.70 6.10 10.40 Sm 3.12 2.16 1.56 1.50 2.31 Eu 0.75 0.62 0.55 0.59 0.74 Gd 3.34 2.32 1.64 1.66 2.35 Tb 0.60 0.41 0.30 0.31 0.42 Dy 3.80 2.66 1.95 2.01 2.8 Ho 0.85 0.56 0.41 0.42 0.58 Er 2.44 1.65 1.21 1.29 1.70 Tm 0.36 0.24 0.19 0.18 0.25 Yb 2.38 1.63 1.33 1.28 1.79 Lu 0.35 0.26 0.22 0.20 0.27 REE 61.58 48.33 40.72 38.05 59.31 Eu/Eu* 0.71 0.85 1.04 1.15 0.96 Cr 33.45 176.64 36.96 33.91 72.97 Co 17.40 23.78 30.66 20.84 21.92 Ni 13.34 43.62 15.87 18.69 23.76 Rb 33.90 38.00 48.00 44.80 35.40 Sr 168.90 157.00 186.50 190.00 197.00 Y 24.60 16.60 12.30 12.60 17.20 Zr 81.00 56.00 31.00 32.00 59.00 Nb 4.36 3.40 3.18 2.19 3.70 Ba 249.00 191.00 202.00 202.00 182.00 Hf 2.26 1.63 1.05 1.28 1.76 Ta 0.28 0.25 0.22 0.43 0.26 Pb 5.86 4.67 5.48 8.16 8.17 Th 1.07 2.83 2.09 5.26 1.98 U 0.40 0.75 0.55 1.53 0.66 注：LOI.烧失量；Mg#=100×Mg2+/(Mg2++0.9×Fe2O3T)；A/CNK=Al2O3/(CaO+Na2O+K2O)摩尔百分比.
下载: 导出CSV
表 4 治多地区日啊日曲石英闪长岩全岩Sr-Nd同位素分析结果
Table 4. Sr-Nd isotopic compositions of the Riariqu quartz diorites from Zhiduo area
样号 87Rb/86Sr 87Sr/86Sr ±2σ (87Sr/86Sr)i 147Sm/144Nd 143Nd/144Nd ±2σ εNd(t) TDM2(Ma) SC-2 0.580 7 0.709 209 4 0.707 408 0.160 9 0.512 332 2 -5.0 1 398 SC-3 0.702 4 0.710 082 6 0.707 904 0.151 6 0.512 290 2 -5.5 1 444 SC-4 0.740 9 0.709 431 5 0.707 134 0.140 1 0.512 343 3 -4.2 1 334 SC-6 0.680 2 0.708 998 4 0.706 889 0.149 5 0.512 437 14 -2.6 1 206 SC-8 0.519 6 0.708 445 6 0.706 834 0.134 9 0.512 469 3 -1.6 1 122 注：εNd(t)值计算采用(147Sm/144Nd)CHUR=0.196 7；(143Nd/144Nd)CHUR=0.512 638；t代表成岩年龄(218 Ma)；同位素亏损地幔模式年龄(TDM2)计算采用(147Sm/144Nd)DM=0.213 7；(143Nd/144Nd)DM=0.513 15.
下载: 导出CSV
-
Andersen, T., 2002. Correction of Common Lead in U-Pb Analyses That do not Report 204Pb. Chemical Geology, 192(1-2): 59-79. doi: 10.1016/S0009-2541(02)00195-X Chen, J.L., Xu, J.F., Ren, J.B., et al., 2013. Geochronology and Geochemical Characteristics of Late Triassic Porphyritic Rocks from the Zhongdian Arc, Eastern Tibet, and Their Tectonic and Metallogenic Implications. Gondwana Research, 26(2): 492-504. doi: 10.1016/j.gr.2013.07.022 Chung, S.L., Chu, M.F., Zhang, Y.Q., et al., 2005. Tibetan Tectonic Evolution Inferred from Spatial and Temporal Variations in Post-Collisional Magmatism. Earth-Science Reviews, 68(3-4): 173-196. doi: 10.1016/j.earscirev.2004.05.001 Condie, K.C., 2005. High Field Strength Element Ratios in Archean Basalts: A Window to Evolving Sources of Mantle Plumes? Lithos, 79(3-4): 491-504. doi: 10.1016/j.lithos.2004.09.014 Crawford, A.J., Falloon, T.J., Green, D.H., et al., 1989. Classification Petrogenesis and Tectonic Setting of Boninites. Academic Division of Unwin Hyaman Ltd., London. Deng, J.F., Liu, C., Feng, Y.F., et al., 2010. High Magnesian Andesitic/Dioritic Rocks (HMA) and Magnesian Andesitic/Dioritic Rocks (MA): Two Igneous Rock Types Related to Oceanic Subduction. Geology in China, 37(4): 1112-1118 (in Chinese with English abstract). http://www.cqvip.com/main/zcps.aspx?c=1&id=35237930 Elburg, M.A., van Bergen, M., Hoogewerff, J., et al., 2002. Geochemical Trends across an Arc-Continent Collision Zone: Magma Sources and Slab-Wedge Transfer Processes below the Pantar Strait Volcanoes, Indonesia. Geochimica et Cosmochimica Acta, 66(15): 2771-2789. doi: 10.1016/S0016-7037(02)00868-2 Furman, T., Graham, D., 1999. Erosion of Lithospheric Mantle beneath the East African Rift System: Geochemical Evidence from the Kivu Volcanic Province. Lithos, 48(1-4): 237-262. doi: 10.1016/S0419-0254(99)80014-7 Fu, X.G., Wang, J., Tan, F.W., et al., 2010. The Late Triassic Rift-Related Volcanic Rocks from Eastern Qiangtang, Northern Tibet (China): Age and Tectonic Implications. Gondwana Research, 17(1): 135-144. doi: 10.1016/j.gr.2009.04.010 Gao, S., Rudnick, R.L., Yuan, H.L., et al., 2004. Recycling Lower Continental Crust in the North China Craton. Nature, 432: 892-897. doi: 10.1038/nature03162 Griffin, W.L., Belousova, E.A., Shee, S.R., et al., 2004. Archean Crustal Evolution in the Northern Yilgarn Craton: U-Pb and Hf-Isotope Evidence from Detrital Zircons. Precambrian Research, 131(3-4): 231-282. doi: 10.1016/j.precamres.2003.12.011 Hawkesworth, C.J., Turner, S.P., Mcdermott, F., et al., 1997. U-Th Isotopes in Arc Magmas: Implications for Element Transfer from the Subducted Crust. Science, 276(5312): 551-555. doi: 10.1126/science.276.5312.551 Hoskin, P.W.O., Schaltegger, U., 2003. The Composition of Zircon and Igneous and Metamorphic Petrogenesis. Reviews in Mineralogy and Geochemistry, 53(1): 27-62. doi: 10.2113/0530027 Hou, Z.Q., Qu, X.M., Zhou, J.R., et al., 2001. Collision-Orogenic Processes of the Yidun Arc in the Sanjiang Region: Record of Granites. Acta Geologica Sinica, 75(4): 484-497 (in Chinese with English abstract). http://www.cqvip.com/qk/95080x/20014/5639608.html Hou, Z.Q., Yang, Y.Q., Qu, X.M., et al., 2004. Tectonic Evolution and Mineralization Systems of the Yidun Arc Orogen in Sanjiang Region, China. Acta Geologica Sinica, 78(1): 109-120 (in Chinese with English abstract). http://www.researchgate.net/publication/281547368_Tectonic_evolution_and_mineralization_systems_of_the_Yidun_Arc_Orogen_in_Sanjiang_Region_China Jian, P., Liu, D.Y., Kröner, A., et al., 2009a. Devonian to Permian Plate Tectonic Cycle of the Paleo-Tethys Orogen in Southwest China (I): Geochemistry of Ophiolites, Arc/Back-Arc Assemblages and Within-Plate Igneous Rocks. Lithos, 113(3-4): 748-766. doi: 10.1016/j.lithos.2009.04.004 Jian, P., Liu, D.Y., Kröner, A., et al., 2009b. Devonian to Permian Plate Tectonic Cycle of the Paleo-Tethys Orogen in Southwest China (II): Insights from Zircon Ages of Ophiolites, Arc/Back-Arc Assemblages and Within-Plate Igneous Rocks and Generation of the Emeishan CFB Province. Lithos, 113(3-4): 767-784. doi: 10.1016/j.lithos.2009.04.006 Kamei, A., Owada, M., Nagao, T., et al., 2004. High-Mg Diorites Derived from Sanukitic HMA Magmas, Kyushu Island, Southwest Japan Arc: Evidence from Clinopyroxene and Whole Rock Compositions. Lithos, 75(3-4): 359-371. doi: 10.1016/j.lithos.2004.03.006 Kapp, P., Yin, A., Manning, C.E., et al., 2000. Blueschist-Bearing Metamorphic Core Complexes in the Qiangtang Block Reveal Deep Crustal Structure of Northern Tibet. Geology, 28: 19-22. doi:10.1130/0091-7613(2000)28<19:BMCCIT>2.0.CO;2 Kapp, P., Yin, A., Manning, C.E., et al., 2003. Tectonic Evolution of the Early Mesozoic Blueschist-Bearing Qiangtang Metamorphic Belt, Central Tibet. Tectonics, 22(4): 1043. doi: 10.1029/2002TC001361 Kelemen, P.B., 1995. Genesis of High Mg# Andesites and the Continental Crust. Contributions to Mineralogy and Petrology, 120(1): 1-19. doi: 10.1007/BF00311004 Kelemen, P.B., Hanghøj, K., Greene, A.R., 2003. One View of the Geochemistry of Subduction-Related Magmatic Arcs, with an Emphasis on Primitive Andesite and Lower Crust. Treatise on Geochemistry, 3: 593-659. doi: 10.1016/B0-08-043751-6/03035-8 Liu, Y.S., Gao, S., Hu, Z.C., et al., 2010. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen: U-Pb Dating, Hf Isotopes and Trace Elements in Zircons of Mantle Xenoliths. Journal of Petrology, 51(1-2): 537-571. doi: 10.1093/petrology/egp082 Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008a. In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard. Chemical Geology, 257(1-2): 34-43. doi: 10.1016/j.chemgeo.2008.08.004 Liu, Y.S., Zong, K.Q., Kelemen, P.B., et al., 2008b. Geochemistry and Magmatic History of Eclogites and Ultramafic Rocks from the Chinese Continental Scientific Drill Hole: Subduction and Ultrahigh-Pressure Metamorphism of Lower Crustal Cumulates. Chemical Geology, 247(1-2): 133-153. doi: 10.1016/j.chemgeo.2008.08.004 Ludwig, K.R., 2003. User's Manual for Isoplot 3.0—A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publication, Berkeley. Luo, W.X., Qian, L.L., Li, D.W., et al., 2013. Petrogenesis of the Zhongzaohuo Ultramafic Pyroxenite Pluton, East Kunlun: Constraints from Petrology, Geochemistry and Genetic Mineralogy. Earth Science—Journal of China University of Geosciences, 38(6): 1214-1228 (in Chinese with English abstract). doi: 10.3799/dqkx.2013.119 Ma, L.Y., Niu, Z.J., Bai, Y.S., et al., 2007. Sr, Nd and Pb Isotopic Geochemistry of Permian Volcanic Rocks from Southern Qinghai and Their Geological Significance. Earth Science—Journal of China University of Geosciences, 32(1): 22-28 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200701002.htm Maniar, P.D., Piccoli, P.M., 1989. Tectonic Discrimination of Granitoids. Geological Society of America Bulletin, 101(5): 635-643. doi:10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2 Mao, J.W., Pirajno, F., Zhang, Z.H., et al., 2006. Late Variscan Post-Collisional Cu-Ni Sulfide Deposits in East Tianshan and Altay in China: Principal Characteristics and Possible Relationship with Mantle Plume. Acta Geologica Sinica, 80(7): 925-942 (in Chinese with English abstract). http://www.researchgate.net/publication/285865027_Late_Variscan_post-collisional_Cu-Ni_sulfide_deposits_in_East_Tianshan_and_Altay_in_China_Principal_characteristics_and_possible_relationship_with_mantle_plume McCarron, J.J., Smellie, J.L., 1998. Tectonic Implications of Fore-Arc Magmatism and Generation of High-Magnesian Andesites: Alexander Island, Antarctica. Journal of the Geological Society, 155(2): 269-280. doi: 10.1144/gsjgs.155.2.0269 Miller, C., Schuster, R., Klotzli, U., et al., 1999. Post-Collisional Potassic and Ultrapotassic Magmatism in SW Tibet: Geochemical and Sr-Nd-Pb-O Isotopic Constraints for Mantle Source Characteristics and Petrogenesis. Journal of Petrology, 40(9): 1399-1424. doi: 10.1093/petrology/40.9.1399 Mo, X.X., Deng, J.F., Dong, F.L., et al., 2001. Volcanic Petrotectonic Assemblages in Sanjiang Orogenic Belt, SW China and Implications for Tectonics. Geological Journal of China Universities, 7(2): 121-138 (in Chinese with English abstract). http://www.researchgate.net/publication/285844189_Volcanic_petrotectonic_assemblages_in_Sanjiang_orogenic_belt_SW_China_and_implication_for_tectonics Pan, G.T., Wang, L.Q., Li, R.S., et al., 2012. Tectonic Evolution of the Qinghai-Tibet Plateau. Journal of Asian Earth Sciences, 53: 3-14. doi: 10.1016/j.jseaes.2011.12.018 Pearce, J.A., Harris, N.B.W., Tindle, A.G., 1984. Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks. Journal of Petrology, 25(4): 956-983. doi: 10.1093/petrology/25.4.956 Pearce, J.A., Peate, D.W., 1995. Tectonic Implications of the Composition of Volcanic Arc Magmas. Annual Review of Earth and Planetary Sciences, 23: 251-286. doi: 10.1146/annurev.ea.23.050195.001343 Peng, T.P., Zhao, G.C., Fan, W.M., et al., 2014. Zircon Geochronology and Hf Isotopes of Mesozoic Intrusive Rocks from the Yidun Terrane, Eastern Tibetan Plateau: Petrogenesis and Their Bearings with Cu Mineralization. Journal of Asian Earth Sciences, 80: 18-33. doi: 10.1016/j.jseaes.2013.10.028 Plank, T., 2005. Constraints from Thorium/Lanthanum on Sediment Recycling at Subduction Zones and the Evolution of the Continents. Journal of Petrology, 46(5): 921-944. doi: 10.1093/petrology/egi005 Plank, T., Langmuir, C.H., 1998. The Chemical Composition of Subducting Sediment and Its Consequences for the Crust and Mantle. Chemical Geology, 145(3-4): 325-394. doi: 10.1016/S0009-2541(97)00150-2 Polat, A., Kerrich, R., 2001. Magnesian Andesites, Nb-Enriched Basalt-Andesites, and Adakites from Late-Archean 2.7 Ga Wawa Greenstone Belts, Superior Province, Canada: Implications for Late Archean Subduction Zone Petrogenetic Processes. Contributions to Mineralogy and Petrology, 141(1): 36-52. doi: 10.1007/s004100000223 Pullen, A., Kapp, P., Gehrels, G.E., et al., 2008. Triassic Continental Subduction in Central Tibet and Mediterranean-Style Closure of the Paleo-Tethys Ocean. Geology, 36(5): 351-354. doi: 10.1130/G24435A.1 Rapp, R.P., Shimizu, N., Norman, M.D., et al., 1999. Reaction between Slab-Derived Melts and Peridotite in the Mantle Wedge: Experimental Constraints at 3.8 GPa. Chemical Geology, 160(4): 335-356. doi: 10.1016/S0009-2541(99)00106-0 Rollinson, H.R., 1993. Using Geochemical Data: Evaluation, Presentation, Interpretation. Longman Group UK Ltd., New York. Shimoda, G., Tatsumi, Y., Nohda, S., et al., 1998. Setouchi High-Mg Andesites Revisited: Geochemical Evidence for Melting of Subducting Sediments. Earth and Planetary Science Letters, 160(3-4): 479-492. doi: 10.1016/S0012-821X(98)00105-8 Shirey, S.B., Hanson, G.N., 1984. Mantle-Derived Archaean Monozodiorites and Trachyandesites. Nature, 310: 222-224. doi: 10.1038/310222a0 Smithies, R.H., Champion, D.C., 1999. Late Archaean Felsic Alkaline Igneous Rocks in the Eastern Goldfields, Yilgarn Craton, Western Australia: A Result of Lower Crustal Delamination? Journal of the Geological Society, 156(3): 561-576. doi: 10.1144/gsjgs.156.3.0561 Smithies, R.H., Champion, D.C., 2000. The Archaean High-Mg Diorite Suite: Links to Tonalite-Trondhjemite-Granodiorite Magmatism and Implications for Early Archaean Crustal Growth. Journal of Petrology, 41(12): 1653-1671. doi: 10.1093/petrology/41.12.1653 Smithies, R.H., van Kranendonk, M.J., Champion, D.C., 2007. The Mesoarchean Emergence of Modern-Style Subduction. Gondwana Research, 11(1-2): 50-68. doi: 10.1016/j.gr.2006.02.001 Sun, S.S., McDonough, W.F., 1989. Chemical and Isotopic Systematics of Oceanic Basalt: Implications for Mantle Composition and Processes. In: Saunders, A.D., Norry, M.J., eds., Magmatism in the Ocean Basins. Geological Society Special Publications, London, 42: 313-345. Tatsumi, Y., 1995. Subduction Zone Magmatism. Blackwell Publishing House, Boston. Tatsumi, Y., 2001. Geochemical Modeling of Partial Melting of Subducting Sediments and Subsequent Melt-Mantle Interaction: Generation of High-Mg Andesites in the Setouchi Volcanic Belt, Southwest Japan. Geology, 29(4): 323-326. doi:10.1130/0091-7613(2001)029<0323:GMOPMO>2.0.CO;2 Tatsumi, Y., Hanyu, T., 2003. Geochemical Modeling of Dehydration and Partial Melting of Subducting Lithosphere: Toward a Comprehensive Understanding of High-Mg Andesite Formation in the Setouchi Volcanic Belt, SW Japan. Geochemistry, Geophysics, Geosystems, 4(9): 1081. doi: 10.1029/2003GC000530 Tatsumi, Y., Ishizaka, K., 1981. Existence of Andesitic Primary Magma: An Example from Southwest Japan. Earth and Planetary Science Letters, 53(1): 124-130. doi: 10.1016/0012-821X(81)90033-9 Tatsumi, Y., Ishizaka, K., 1982. Origin of High-Magnesian Andesites in the Setouchi Volcanic Belt, Southwest Japan, I. Petrographical and Chemical Characteristics. Earth and Planetary Science Letters, 60(2): 293-304. doi: 10.1016/0012-821X(82)90008-5 Tatsumi, Y., Shukuno, H., Sato, K., et al., 2003. The Petrology and Geochemistry of High-Magnesium Andesites at the Western Tip of the Setouchi Volcanic Belt, SW Japan. Journal of Petrology, 44(9): 1561-1578. doi: 10.1093/petrology/egg049 Wang, B.Q., Zhou, M.F., Chen, W.T., et al., 2013. Petrogenesis and Tectonic Implications of the Triassic Volcanic Rocks in the Northern Yidun Terrane, Eastern Tibet. Lithos, 175-176: 285-301. doi: 10.1016/j.lithos.2013.05.013 Wang, B.Q., Zhou, M.F., Li, J.W., et al., 2011a. Late Triassic Porphyritic Intrusions and Associated Volcanic Rocks from the Shangri-La Region, Yidun Terrane, Eastern Tibetan Plateau: Adakitic Magmatism and Porphyry Copper Mineralization. Lithos, 127(1-2): 24-38. doi: 10.1016/j.lithos.2011.07.028 Wang, Q., Li, Z.X., Chung, S.L., et al., 2011b. Late Triassic High-Mg Andesite/Dacite Suites from Northern Hohxil, North Tibet: Geochronology, Geochemical Characteristics, Petrogenetic Processes and Tectonic Implications. Lithos, 126(1-2): 54-67. doi: 10.1016/j.lithos.2011.06.002 Wang, Q., Wyman, D.A., Xu, J.F., et al., 2008. Triassic Nb-Enriched Basalts, Magnesian Andesites, and Adakites of the Qiangtang Terrane (Central Tibet): Evidence for Metasomatism by Slab-Derived Melts in the Mantle Wedge. Contributions to Mineralogy and Petrology, 155(4): 473-490. doi: 10.1007/s00410-007-0253-1 Wang, Q., Zhao, Z.H., Xu, J.F., et al., 2006. Carboniferous Adakite-High-Mg Andesite-Nb-Enriched Basaltic Rocks Suites in the Northern Tianshan Area: Implications for Phanerozoic Crustal Growth in the Central Asia Orogenic Belt and Cu-Au Mineralization. Acta Petrologica Sinica, 22(1): 11-30 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200601002.htm Wilson, M., 1989. Igneous Petrogenesis. Unwim Hyman, London. Woodhead, J.D., Hergt, J.M., Davidson, J.P., et al., 2001. Hafnium Isotope Evidence for 'Conservative' Element Mobility during Subduction Zone Processes. Earth and Planetary Science Letters, 192(3): 331-346. doi: 10.1016/S0012-821X(01)00453-8 Xu, Z.Q., Yang, J.S., Li, W.C., et al., 2013. Paleo-Tethys System and Accretionary Orogen in the Tibet Plateau. Acta Petrologica Sinica, 29(6): 1847-1860 (in Chinese with English abstract). http://www.cqvip.com/QK/94579X/20136/46670152.html Yan, Q.R., Wang, Z.Q., Liu, S.W., et al., 2005. The Tethys Expansion and the Gondwana Cleavage in West-Northern Sanjiang: The SHRIMP Chronological Evidence from Ganzi Ophiolite Gabbro. Chinese Science Bulletin, 50(2): 158-166 (in Chinese). doi: 10.1360/csb2005-50-2-158 Yi, L.W., Ma, C.Q., Wang, L.X., et al., 2014. Discovery of Late Ordovician Subvolcanic Rocks in South China: Existence of Subduction-Related Dacite from Early Paleozoic? Earth Science—Journal of China University of Geosciences, 39(6): 637-653 (in Chinese with English abstract). doi: 10.3799/dqkx.2014.061 Yin, A., Harrison, T.M., 2000. Geologic Evolution of the Himalayan-Tibetan Orogen. Annual Review Earth and Planetary Science Letters, 28: 211-280. doi: 10.1146/annurev.earth.28.1.211 Yin, J.Y., Yuan, C., Sun, M., et al., 2012. Age, Geochemical Features and Possible Petrogenesis Mechanism of Early Permian Diorite in Hatu, Xinjiang. Acta Petrologica Sinica, 28(7): 2171-2182 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-YSXB201207019.htm Yogodzinski, G.M., Key, R.W., Volynets, O.N., et al., 1995. Magnesian Andesite in the Western Aleutian Komandorsky Region: Implications for Slab Melting and Processes in the Mantle Wedge. Geological Society of America Bulletin, 107(5): 505-519. doi:10.1130/0016-7606(1995)107<0505:MAITWA>2.3.CO;2 Yogodzinski, G.M., Volynets, O.N., Koloskov, A.V., et al., 1994. Magnesian Andesites and the Subduction Component in a Strongly Calcalkaline Series at Piip Volcano, Far Western Aleutians. Journal of Petrology, 35(1): 163-204. doi: 10.1093/petrology/35.1.163 Zhai, Q.G., Jahn, B.M., Su, L., et al., 2013. Triassic Arc Magmatism in the Qiangtang Area, Northern Tibet: Zircon U-Pb Ages, Geochemical and Sr-Nd-Hf Isotopic Characteristics, and Tectonic Implications. Journal of Asian Earth Sciences, 63(1): 162-178. doi: 10.1016/j.jseaes.2012.08.025 Zhai, Q.G., Jahn, B.M., Zhang, R.Y., et al., 2011. Triassic Subduction of the Paleo-Tethys in Northern Tibet, China: Evidence from the Geochemical and Isotopic Characteristics of Eclogites and Blueschists of the Qiangtang Block. Journal of Asian Earth Sciences, 42(6): 1356-1370. doi: 10.1016/j.jseaes.2011.07.023 Zhang, Q., Qian, Q., Zhai, M.G., et al., 2005. Geochemistry, Petrogenesis and Geodynamic Implications of Sanukite. Acta Petrologica et Mineralogica, 24(2): 117-125 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW200502004.htm Zhang, Q., Wang, Y., Qian, Q., et al., 2004. Sanukite of Late Archaean and Early Earth Evolution. Acta Petrologica Sinica, 20(6): 1355-1362 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB200406004.htm Zhang, Z.M., Dong, X., Santosh, M., et al., 2014. Metamorphism and Tectonic Evolution of the Lhasa Terrane, Central Tibet. Gondwana Research, 25(1): 170-189. doi: 10.1016/j.gr.2012.08.024 Zhao, Z.H., Wang, Q., Xiong, X.L., et al., 2007. Magnesian Igneous Rocks in Northern Xinjiang. Acta Petrologica Sinica, 23(7): 1696-1707 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200707014.htm Zheng, Y.C., Hou, Z.Q., Gong, Y.L., et al., 2014. Petrogenesis of Cretaceous Adakite-Like Intrusions of the Gangdese Plutonic Belt, Southern Tibet: Implications for Mid-Ocean Ridge Subduction and Crustal Growth. Lithos, 190-191: 240-263. doi: 10.1016/j.lithos.2013.12.013 Zhu, D.C., Zhao, Z.D., Niu, Y.L., et al., 2013. The Origin and Pre-Cenozoic Evolution of the Tibetan Plateau. Gondwana Research, 23(4): 1429-1454. doi: 10.1016/j.gr.2012.02.002 Zi, J.W., Cawood, P.A., Fan, W.M., et al., 2012. Contrasting Rift and Subduction-Related Plagiogranites in the Jinshajiang Ophiolitic Melange, Southwest China, and Implications for the Paleo-Tethys. Tectonics, 31: 1-18. doi: 10.1029/2011TC002937 邓晋福, 刘翠, 冯艳芳, 等, 2010. 高镁安山岩/闪长岩类(HMA)和镁安山岩/闪长岩类(MA): 与洋俯冲作用相关的两类典型的火成岩类. 中国地质, 37(4): 1112-1118. doi: 10.3969/j.issn.1000-3657.2010.04.025 侯增谦, 曲晓明, 周继荣, 等, 2001. 三江地区义敦岛弧碰撞造山过程: 花岗岩记录. 地质学报, 75(4): 484-497. doi: 10.3321/j.issn:0001-5717.2001.04.008 侯增谦, 杨岳清, 曲晓明, 等, 2004. 三江地区义敦岛弧造山带演化和成矿系统. 地质学报, 78(1): 109-120. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200401013.htm 罗文行, 钱莉莉, 李德威, 等, 2013. 东昆仑中灶火地区超镁铁质辉石岩的成因. 地球科学——中国地质大学学报, 38(6): 1214-1228. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201306006.htm 马丽艳, 牛志军, 白云山, 等, 2007. 青海南部二叠纪火山岩Sr、Nd、Pb同位素特征及地质意义. 地球科学——中国地质大学学报, 32(1): 22-28. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200701002.htm 毛景文, Pirajno, F., 张作衡, 等, 2006. 天山-阿尔泰东部地区海西晚期后碰撞铜镍硫化物矿床: 主要特点及可能与地幔柱的关系. 地质学报, 80(7): 925-942. doi: 10.3321/j.issn:0001-5717.2006.07.001 莫宣学, 邓晋福, 董方浏, 等, 2001. 西南三江造山带火山岩-构造组合及其意义. 高校地质学报, 7(2): 121-138. doi: 10.3969/j.issn.1006-7493.2001.02.001 王强, 赵振华, 许继峰, 等, 2006. 天山北部石炭纪埃达克岩-高镁安山岩-富Nb岛弧玄武质岩: 对中亚造山带显生宙地壳增生与铜金成矿的意义. 岩石学报, 22(1): 11-30. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200601002.htm 许志琴, 杨经绥, 李文昌, 等, 2013. 青藏高原中的古特提斯体制与增生造山作用. 岩石学报, 29(6): 1847-1860. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201306002.htm 闫全人, 王宗起, 刘树文, 等, 2005. 西南三江特提斯洋扩张与晚古生代东冈瓦纳裂解: 来自甘孜蛇绿岩辉长岩的SHRIMP年代学证据. 科学通报, 50(2): 158-166. doi: 10.3321/j.issn:0023-074X.2005.02.010 易立文, 马昌前, 王连训, 等, 2014. 华南晚奥陶世次火山岩的发现: 早古生代与俯冲有关的英安岩? 地球科学——中国地质大学学报, 39(6): 637-653. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201406001.htm 尹继元, 袁超, 孙敏, 等, 2012. 新疆哈图早二叠世富镁闪长岩的时代、地球化学特征和可能的成因机制. 岩石学报, 28(7): 2171-2182. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201207019.htm 张旗, 钱青, 翟明国, 等, 2005. Sanukite(赞岐岩) 的地球化学特征、成因及其地球动力学意义. 岩石矿物学杂志, 24(2): 117-125. doi: 10.3969/j.issn.1000-6524.2005.02.005 张旗, 王焰, 钱青, 等, 2004. 晚太古代Sanukite(赞岐岩)与地球早期演化. 岩石学报, 20(6): 1355-1362. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200406004.htm 赵振华, 王强, 熊小林, 等, 2007. 新疆北部的富镁火成岩. 岩石学报, 23(7): 1696-1707. doi: 10.3969/j.issn.1000-0569.2007.07.015 -
点击查看大图
图(10) / 表(4)
计量
- 文章访问数: 4397
- HTML全文浏览量: 703
- PDF下载量: 534
- 被引次数: 0
