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Chronology and geochemical characteristics of trachytes in the Tiaojishan Formation, Xuanhua Basin, northwestern Hebei Province, and their geological implications |
YANG Ji-Yuan1(), HU Xin-Zhuo2(), ZHOU Jing1, QI Peng-Chao3, LI Ze-Yang1, MENG Jia-Bao1, XU Fan1, ZHANG Hui-Bin1, QI Hui-Yun1 |
1. Hebei Institute of Regional Geological Survey(Geotourism Research Center of Hebei Province), Langfang 065000, China 2. Langfang Natural Resources Comprehensive Survey Center, China Geological Survey, Langfang 065000, China 3. No. 6 Geological Team of Hebei Bureau of Geology and Mineral Resources Exploration, Shijiazhuang 050000, China |
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Abstract The Tiaojishan Formation in northwestern Hebei Province is home to volcanic-sedimentary strata. Due to the lack of fossil organisms, insufficient isotopic dating data, and outdated dating methods, the formation epochs of these strata have been controversial. To accurately determine their formation epochs and examine their regional geotectonic setting, this study conducted a detailed field investigation of the lithologic assemblage of the Tiaojishan Formation in the Xuanhua Basin. Petrological, petrogeochemical, and high-precision isotopic dating studies were conducted on the trachytic volcanic rocks in the upper segment of the formation, obtaining the LA-ICP-MS-based zircon U-Pb isotopic ages, which were 161.1±1.2 Ma and 162.5±1.3Ma. As indicated by the petrological and petrogeochemical characteristics, these trachytic volcanic rocks belong to the shoshonite series, exhibiting enriched light rare earth elements, relatively enriched elements including Rb, K, Th, Ce, Zr, and Hf, and relatively depleted Ba, Nb, Sr, P, and Ti. According to the comparison of principal parameters and graphical discrimination, the magma originated primarily from the melting of continental crustal materials and formed in the tectonic setting of compressional continental margin volcanic arcs. The comprehensive research reveals that the Tiaojishan Formation formed primarily during the Middle Jurassic and continued to the Late Jurassic, and the trachytic volcanic rocks in its upper segment formed in the intraplate compressional tectonic setting. The results of this study provide new data for the division and correlation of Mesozoic volcanic-sedimentary strata and the analysis of their formation environment.
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Received: 08 October 2022
Published: 26 February 2024
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31])and geological sketch (b) of the Xuanhua Basin (simplified according to Bai C D,et al[32]) 1—Quaternary;2—Zhangjiakou Formation;3—Tuchengzi Formation;4—the second section of Tiaojishan Formation;5—the first section of Tiaojishan Formation;6—Jiulongshan Formation;7—Wumishan Formation;8—Gaoyuzhuang Formation;9—granite porphyry;10—angle unconformity contact boundary;11—normal fault and dip;12—fault of unknown nature;13—Feilaifeng structure;14—formation occurrrence;15—volcanic crater;16—sampling position ">
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Sketch map of the regional structure (a) (simplified according to Zhen S M, et al. [31])and geological sketch (b) of the Xuanhua Basin (simplified according to Bai C D,et al[32]) 1—Quaternary;2—Zhangjiakou Formation;3—Tuchengzi Formation;4—the second section of Tiaojishan Formation;5—the first section of Tiaojishan Formation;6—Jiulongshan Formation;7—Wumishan Formation;8—Gaoyuzhuang Formation;9—granite porphyry;10—angle unconformity contact boundary;11—normal fault and dip;12—fault of unknown nature;13—Feilaifeng structure;14—formation occurrrence;15—volcanic crater;16—sampling position
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Field outcrops(a~d) and photomicrographs(e~f) of trachytes in the Tiaojishan Formation, Xuanhua Basin (Kfs: potassium feldspar)
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样品号 | 含量/10-6 | 同位素比值 | 年龄/Ma | Pb | 232Th | 238U | Th/U | 207Pb/ 235U | 2σ | 206Pb/ 238U | 2σ | 207Pb/ 206Pb | 2σ | 208Pb/ 232Th | 2σ | 206Pb/ 238U | 2σ | 207Pb/ 235U | 2σ | 208Pb/ 232Th | 2σ | D2022-1 | 3.0 | 62.5 | 94.0 | 0.66 | 0.177 | 0.021 | 0.0251 | 0.0007 | 0.0515 | 0.006 | 0.0081 | 0.0007 | 159.7 | 4.5 | 162.0 | 18.0 | 162.0 | 14.0 | D2022-2 | 2.6 | 66.1 | 77.4 | 0.85 | 0.181 | 0.028 | 0.0253 | 0.0008 | 0.0530 | 0.009 | 0.0086 | 0.0007 | 161.0 | 5.3 | 162.0 | 24.0 | 174.0 | 14.0 | D2022-3* | 6.0 | 57.2 | 82.9 | 0.69 | 1.490 | 0.190 | 0.0305 | 0.0014 | 0.3230 | 0.034 | 0.0399 | 0.0043 | 193.6 | 8.5 | 829.0 | 73.0 | 784.0 | 82.0 | D2022-4 | 2.3 | 46.0 | 74.5 | 0.62 | 0.179 | 0.029 | 0.0254 | 0.0011 | 0.0504 | 0.008 | 0.0079 | 0.0010 | 161.9 | 6.8 | 160.0 | 25.0 | 160.0 | 21.0 | D2022-5 | 3.2 | 63.3 | 100.8 | 0.63 | 0.164 | 0.021 | 0.0251 | 0.0007 | 0.0478 | 0.006 | 0.0086 | 0.0007 | 159.7 | 4.6 | 149.0 | 18.0 | 173.0 | 13.0 | D2022-6 | 2.8 | 58.3 | 85.7 | 0.68 | 0.165 | 0.021 | 0.0253 | 0.0007 | 0.0485 | 0.006 | 0.0083 | 0.0007 | 161.3 | 4.7 | 149.0 | 19.0 | 167.0 | 13.0 | D2022-7 | 2.8 | 58.7 | 84.6 | 0.69 | 0.178 | 0.024 | 0.0254 | 0.0008 | 0.0513 | 0.007 | 0.0085 | 0.0007 | 161.8 | 4.7 | 161.0 | 21.0 | 170.0 | 13.0 | D2022-8 | 2.7 | 48.8 | 88.6 | 0.55 | 0.166 | 0.019 | 0.0251 | 0.0008 | 0.0477 | 0.006 | 0.0083 | 0.0009 | 159.7 | 4.7 | 151.0 | 17.0 | 166.0 | 18.0 | D2022-9 | 2.1 | 36.3 | 67.6 | 0.54 | 0.162 | 0.025 | 0.0255 | 0.0008 | 0.0458 | 0.007 | 0.0093 | 0.0009 | 162.0 | 5.1 | 145.0 | 22.0 | 187.0 | 17.0 | D2022-10 | 2.6 | 45.8 | 81.0 | 0.56 | 0.175 | 0.021 | 0.0253 | 0.0007 | 0.0531 | 0.007 | 0.0089 | 0.0008 | 161.0 | 4.4 | 158.0 | 18.0 | 180.0 | 15.0 | D2022-11 | 2.9 | 57.3 | 82.9 | 0.69 | 0.201 | 0.037 | 0.0253 | 0.0009 | 0.0610 | 0.011 | 0.0093 | 0.0013 | 161.1 | 5.4 | 176.0 | 31.0 | 187.0 | 27.0 | D2022-12 | 2.4 | 46.6 | 80.6 | 0.58 | 0.175 | 0.033 | 0.0251 | 0.0009 | 0.0498 | 0.009 | 0.0084 | 0.0010 | 160.0 | 5.7 | 157.0 | 28.0 | 169.0 | 20.0 | D2022-13 | 2.4 | 39.9 | 73.2 | 0.55 | 0.163 | 0.035 | 0.0250 | 0.0010 | 0.0500 | 0.010 | 0.0097 | 0.0013 | 159.3 | 6.5 | 148.0 | 31.0 | 194.0 | 27.0 | D2022-14 | 2.1 | 39.8 | 64.9 | 0.61 | 0.175 | 0.026 | 0.0251 | 0.0008 | 0.0500 | 0.008 | 0.0080 | 0.0008 | 159.7 | 4.9 | 154.0 | 22.0 | 162.0 | 17.0 | D2022-15 | 1.6 | 30.2 | 53.4 | 0.57 | 0.169 | 0.040 | 0.0257 | 0.0012 | 0.0500 | 0.012 | 0.0080 | 0.0012 | 163.6 | 7.5 | 154.0 | 36.0 | 161.0 | 23.0 | D2022-16 | 2.9 | 56.6 | 83.5 | 0.68 | 0.191 | 0.025 | 0.0256 | 0.0009 | 0.0552 | 0.007 | 0.0088 | 0.0009 | 163.0 | 5.8 | 174.0 | 22.0 | 177.0 | 18.0 | D2022-17 | 3.3 | 88.8 | 92.9 | 0.96 | 0.201 | 0.046 | 0.0261 | 0.0014 | 0.0570 | 0.014 | 0.0084 | 0.0013 | 166.0 | 8.7 | 181.0 | 39.0 | 169.0 | 26.0 | D2022-18 | 1.7 | 30.1 | 52.8 | 0.57 | 0.166 | 0.035 | 0.0254 | 0.0011 | 0.0480 | 0.010 | 0.0091 | 0.0013 | 161.3 | 6.9 | 148.0 | 30.0 | 182.0 | 26.0 | D2022-19 | 1.9 | 32.8 | 59.8 | 0.55 | 0.180 | 0.032 | 0.0250 | 0.0010 | 0.0540 | 0.010 | 0.0084 | 0.0013 | 159.2 | 6.6 | 160.0 | 27.0 | 169.0 | 26.0 | D2022-20 | 2.0 | 39.1 | 62.4 | 0.63 | 0.174 | 0.025 | 0.0257 | 0.0009 | 0.0502 | 0.008 | 0.0088 | 0.0010 | 163.7 | 5.6 | 158.0 | 22.0 | 176.0 | 20.0 |
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Chronological analysis results of trachyte (D2022) zircon by LA-ICP-MS
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样品号 | 含量/10-6 | 同位素比值 | 年龄/Ma | Pb | 232Th | 238U | Th/U | 207Pb/ 235U | 2σ | 206Pb/ 238U | 2σ | 207Pb/ 206Pb | 2σ | 208Pb/ 232Th | 2σ | 206Pb/ 238U | 2σ | 207Pb/ 235U | 2σ | 208Pb/ 232Th | 2σ | D3511-1* | 7.7 | 151.8 | 187.0 | 0.81 | 0.24 | 0.035 | 0.0326 | 0.0008 | 0.05 | 0.0075 | 0.0112 | 0.0010 | 206.9 | 4.8 | 217.0 | 29.0 | 226.0 | 21.0 | D3511-2 | 64.9 | 2168.0 | 1695.0 | 1.28 | 0.18 | 0.007 | 0.0256 | 0.0005 | 0.05 | 0.0016 | 0.0080 | 0.0002 | 162.8 | 2.8 | 167.0 | 5.7 | 161.3 | 3.4 | D3511-3* | 29.8 | 509.0 | 455.0 | 1.12 | 0.33 | 0.016 | 0.0452 | 0.0008 | 0.05 | 0.0026 | 0.0142 | 0.0004 | 285.1 | 4.8 | 285.0 | 12.0 | 285.8 | 7.3 | D3511-4* | 105.9 | 100.7 | 462.0 | 0.22 | 2.07 | 0.072 | 0.1869 | 0.0037 | 0.08 | 0.0028 | 0.0629 | 0.0033 | 1104.0 | 20.0 | 1136.0 | 24.0 | 1232.0 | 62.0 | D3511-5* | 15.6 | 117.4 | 206.1 | 0.57 | 0.46 | 0.044 | 0.0593 | 0.0013 | 0.06 | 0.0055 | 0.0186 | 0.0013 | 371.5 | 7.9 | 378.0 | 31.0 | 372.0 | 25.0 | D3511-6* | 19.1 | 331.2 | 498.0 | 0.67 | 0.21 | 0.017 | 0.0282 | 0.0008 | 0.05 | 0.0049 | 0.0087 | 0.0006 | 179.1 | 4.9 | 193.0 | 14.0 | 174.0 | 12.0 | D3511-7* | 15.7 | 207.2 | 241.0 | 0.86 | 0.34 | 0.026 | 0.0459 | 0.0010 | 0.05 | 0.0041 | 0.0149 | 0.0007 | 289.2 | 6.1 | 292.0 | 20.0 | 299.0 | 14.0 | D3511-8* | 13.2 | 250.8 | 190.6 | 1.32 | 0.35 | 0.033 | 0.0458 | 0.0013 | 0.06 | 0.0054 | 0.0138 | 0.0008 | 288.6 | 8.0 | 299.0 | 25.0 | 277.0 | 16.0 | D3511-9* | 34.1 | 490.0 | 486.0 | 1.01 | 0.37 | 0.016 | 0.0494 | 0.0009 | 0.05 | 0.0024 | 0.0153 | 0.0004 | 311.0 | 5.2 | 315.0 | 12.0 | 307.3 | 7.7 | D3511-10 | 22.4 | 600.0 | 647.0 | 0.93 | 0.18 | 0.007 | 0.0255 | 0.0004 | 0.05 | 0.0021 | 0.0083 | 0.0002 | 162.4 | 2.4 | 165.8 | 6.3 | 166.7 | 4.4 | D3511-11 | 16.6 | 351.7 | 503.4 | 0.70 | 0.18 | 0.010 | 0.0255 | 0.0005 | 0.05 | 0.0029 | 0.0078 | 0.0003 | 162.2 | 2.9 | 166.7 | 8.9 | 157.5 | 6.5 | D3511-12* | 29.2 | 502.0 | 441.0 | 1.14 | 0.35 | 0.033 | 0.0447 | 0.0013 | 0.06 | 0.0048 | 0.0141 | 0.0007 | 281.7 | 7.9 | 303.0 | 24.0 | 282.0 | 13.0 | D3511-13 | 9.0 | 221.6 | 265.0 | 0.84 | 0.18 | 0.012 | 0.0257 | 0.0005 | 0.05 | 0.0032 | 0.0082 | 0.0003 | 163.5 | 3.1 | 164.0 | 10.0 | 165.5 | 6.4 | D3511-14* | 198.1 | 109.7 | 304.0 | 0.36 | 11.80 | 0.190 | 0.4927 | 0.0073 | 0.17 | 0.0022 | 0.1374 | 0.0028 | 2581.0 | 32.0 | 2586.0 | 15.0 | 2601.0 | 50.0 | D3511-15 | 3.5 | 90.1 | 96.1 | 0.94 | 0.19 | 0.027 | 0.0253 | 0.0008 | 0.05 | 0.0074 | 0.0086 | 0.0006 | 161.1 | 4.7 | 168.0 | 23.0 | 174.0 | 13.0 | D3511-16* | 39.3 | 493.0 | 591.0 | 0.83 | 0.35 | 0.035 | 0.0473 | 0.0012 | 0.05 | 0.0056 | 0.0155 | 0.0008 | 297.6 | 7.2 | 303.0 | 26.0 | 310.0 | 16.0 | D3511-17 | 45.6 | 699.0 | 596.0 | 1.17 | 0.65 | 0.028 | 0.0488 | 0.0009 | 0.10 | 0.0046 | 0.0192 | 0.0005 | 307.2 | 5.7 | 500.0 | 17.0 | 384.0 | 10.0 | D3511-18* | 234.3 | 342.3 | 311.5 | 1.10 | 11.59 | 0.190 | 0.4840 | 0.0074 | 0.17 | 0.0028 | 0.1335 | 0.0022 | 2543.0 | 32.0 | 2573.0 | 15.0 | 2532.0 | 40.0 |
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Chronological analysis results of trachyte (D3511) zircon by LA-ICP-MS
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样品号 | PM17-38-1 | PM17-41-1 | PM17-44-1 | D2022 | D3511 | D4021-1 | D4021-2 | D4022-1 | SiO2 | 64.60 | 65.62 | 63.35 | 68.96 | 63.18 | 62.72 | 61.19 | 63.96 | TiO2 | 0.90 | 0.97 | 0.99 | 0.34 | 0.99 | 1.04 | 1.02 | 0.96 | Al2O3 | 13.76 | 14.52 | 14.64 | 15.46 | 14.55 | 15.34 | 15.24 | 14.47 | Fe2O3 | 5.83 | 4.42 | 6.66 | 1.43 | 5.40 | 6.50 | 8.63 | 7.72 | FeO | 0.33 | 0.55 | 1.14 | 0.49 | 0.63 | 0.18 | 0.18 | 0.12 | MnO | 0.137 | 0.076 | 0.12 | 0.040 | 0.130 | 0.042 | 0.066 | 0.043 | MgO | 0.45 | 0.50 | 0.55 | 0.87 | 1.34 | 0.39 | 0.51 | 0.32 | CaO | 2.26 | 1.55 | 0.90 | 2.35 | 1.57 | 1.07 | 1.20 | 1.11 | Na2O | 4.00 | 4.37 | 4.39 | 3.45 | 4.31 | 4.18 | 3.79 | 3.20 | K2O | 5.45 | 5.75 | 5.81 | 4.34 | 5.63 | 6.10 | 5.86 | 5.74 | P2O5 | 0.282 | 0.312 | 0.32 | 0.149 | 0.330 | 0.337 | 0.324 | 0.306 | 灼失量 | 1.87 | 1.19 | 0.89 | 1.83 | 1.77 | 2.00 | 1.88 | 1.97 | Total | 99.91 | 99.89 | 99.88 | 99.76 | 99.90 | 99.89 | 99.89 | 99.91 | A/NK | 1.10 | 1.08 | 1.08 | 1.49 | 1.10 | 1.14 | 1.21 | 1.26 | A/CNK | 0.87 | 0.94 | 1.02 | 1.08 | 0.95 | 1.05 | 1.09 | 1.13 | La | 51.90 | 55.50 | 53.70 | 43.20 | 52.70 | 45.40 | 54.00 | 53.20 | Ce | 96.10 | 105.00 | 108.00 | 74.30 | 99.60 | 93.70 | 109.00 | 112.00 | Pr | 12.90 | 13.50 | 13.60 | 7.86 | 12.70 | 12.00 | 13.30 | 13.60 | Nd | 49.70 | 51.50 | 52.40 | 27.50 | 49.40 | 47.40 | 51.70 | 53.00 | Sm | 9.57 | 9.16 | 9.03 | 4.04 | 9.14 | 9.17 | 9.34 | 9.80 | Eu | 2.74 | 2.84 | 2.81 | 1.30 | 2.68 | 3.41 | 3.09 | 2.95 | Gd | 8.57 | 7.86 | 8.16 | 3.47 | 7.83 | 8.33 | 8.29 | 8.73 | Tb | 1.37 | 1.26 | 1.30 | 0.48 | 1.30 | 1.40 | 1.38 | 1.47 | Dy | 7.96 | 7.07 | 7.09 | 2.30 | 7.69 | 6.84 | 7.09 | 7.74 | Ho | 1.50 | 1.34 | 1.40 | 0.44 | 1.46 | 1.24 | 1.35 | 1.51 | Er | 4.05 | 3.65 | 4.07 | 1.39 | 4.15 | 3.43 | 3.87 | 4.34 | Tm | 0.60 | 0.54 | 0.68 | 0.22 | 0.65 | 0.49 | 0.58 | 0.68 | Yb | 3.66 | 3.17 | 4.18 | 1.60 | 3.98 | 2.85 | 3.57 | 4.20 | Lu | 0.57 | 0.48 | 0.63 | 0.26 | 0.64 | 0.42 | 0.53 | 0.61 | Y | 38.70 | 34.50 | 37.80 | 13.20 | 38.60 | 31.80 | 33.90 | 41.10 | Rb | 101.00 | 106.00 | 108.00 | 101.00 | 90.10 | 92.90 | 101.00 | 103.00 | Ba | 356.00 | 386.00 | 370.00 | 1255.00 | 340.00 | 377.00 | 312.00 | 267.00 | Th | 7.99 | 8.21 | 7.84 | 7.84 | 7.45 | 8.24 | 9.05 | 8.80 | U | 1.62 | 1.69 | 1.62 | 1.23 | 1.88 | 1.53 | 1.51 | 1.71 | Nb | 19.70 | 21.00 | 20.90 | 13.80 | 19.80 | 18.90 | 19.80 | 19.90 | Sr | 36.90 | 31.00 | 32.20 | 433.00 | 54.80 | 74.40 | 38.80 | 46.60 | Zr | 325.00 | 358.00 | 375.00 | 147.00 | 336.00 | 369.00 | 379.00 | 385.00 | Hf | 8.44 | 8.69 | 8.86 | 4.05 | 8.25 | 9.27 | 9.26 | 9.02 | Ga | 23.00 | 24.70 | 24.50 | 16.00 | 24.00 | 23.80 | 24.50 | 24.60 | Ta | 1.12 | 1.13 | 1.35 | 1.00 | 1.09 | 1.21 | 1.21 | 1.14 | V | 12.00 | 7.02 | 6.62 | 28.40 | 5.12 | 51.80 | 24.40 | 35.50 | Co | 2.11 | 1.09 | 1.25 | 3.26 | 2.38 | 1.84 | 1.29 | 0.91 | Ni | 3.33 | 1.97 | 2.87 | 2.46 | 3.02 | 1.13 | 0.98 | 1.26 | ∑REE | 251.16 | 262.49 | 267.08 | 168.47 | 253.92 | 236.10 | 267.00 | 273.96 | LREE | 222.90 | 237.13 | 239.57 | 158.30 | 226.22 | 21110.00 | 240.34 | 244.68 | HREE | 28.27 | 25.36 | 27.52 | 10.16 | 27.69 | 25.00 | 26.65 | 29.29 | LREE/ HREE | 7.89 | 9.35 | 8.71 | 15.57 | 8.17 | 8.45 | 9.02 | 8.35 | La/Yb | 10.19 | 12.54 | 9.22 | 19.34 | 9.51 | 11.46 | 10.87 | 9.08 | δEu | 0.92 | 1.02 | 1.00 | 1.06 | 0.97 | 1.19 | 1.07 | 0.97 | δCe | 0.91 | 0.94 | 0.98 | 0.99 | 0.94 | 0.99 | 0.99 | 1.02 |
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Analysis results of major elements (%), trace elements and rare earth elements (10-6) of trachytes in the Tiaojishan Formation
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Zircon cathodoluminescence images of trachytes in the Tiaojishan Formation, Xuanhua Basin
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Consonance map and weighted average age of U-Pb ages of trachytes in the Tiaojishan Formation, Xuanhua Basin a—D2022;b—D3511
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39] and w(K2O)-w(SiO2) diagram (b)[40-41]of trachytes in the Tiaojishan Formation, Xuanhua Basin 1—picrite basalt;2—basalt;3—basaltic andesite;4—andesite;5—dacite;6—rhyolite; 7—trachybasalt;8—basaltic trachyandesite;9—trachyandesite;10—trachyte,trachyte dacite; 11—phonolite;12—alkalinite phonolite;13—phonolitic alkali basalt;14—alkali basalt, basalt; 15—subfeldspar rock ">
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TAS diagram (a) [39] and w(K2O)-w(SiO2) diagram (b)[40-41]of trachytes in the Tiaojishan Formation, Xuanhua Basin 1—picrite basalt;2—basalt;3—basaltic andesite;4—andesite;5—dacite;6—rhyolite; 7—trachybasalt;8—basaltic trachyandesite;9—trachyandesite;10—trachyte,trachyte dacite; 11—phonolite;12—alkalinite phonolite;13—phonolitic alkali basalt;14—alkali basalt, basalt; 15—subfeldspar rock
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42],primitive mantle normalized values according to Sun and McDonough[43]) ">
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Chondrite-normalized rare earth element distribution map (a) and spider diagram of primitive mantle normalized trace elements (b) of trachytes in the Tiaojishan Formation, Xuanhua Basin(standardized values for chondrites according to Bounton[42],primitive mantle normalized values according to Sun and McDonough[43])
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Harker diagram of major elements of trachytes in the Tiaojishan Formation, Xuanhua Basin
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53] and Sr/Y—Y diagram (b)[54] of trachytes in the Tiaojishan Formation,Xuanhua Basin ">
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A/FM—C/FM diagram (a)[53] and Sr/Y—Y diagram (b)[54] of trachytes in the Tiaojishan Formation,Xuanhua Basin
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64?-66] WPG—intraplate granite; VAG—volcanic arc granite; syn-COLG—syncolliding granite; ORG—mid-ocean ridge plagiogranite;1—mantle plagioclase granite; 2 —destructive active plate margin (pre-plate collision) granite; 3—post-plate collision uplift granite; 4—late orogenic granite; 5—A-type granite in non-orogenic mountains; 6—syncollision S-type granite; 7—post-orogenic A-type granite ">
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Discrimination map of trachytes in the Tiaojishan Formation, Xuanhua Basin[64?-66] WPG—intraplate granite; VAG—volcanic arc granite; syn-COLG—syncolliding granite; ORG—mid-ocean ridge plagiogranite;1—mantle plagioclase granite; 2 —destructive active plate margin (pre-plate collision) granite; 3—post-plate collision uplift granite; 4—late orogenic granite; 5—A-type granite in non-orogenic mountains; 6—syncollision S-type granite; 7—post-orogenic A-type granite
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