Crustal architecture of the oblique collision belt: Insights of the spatial variation in U-Pb ages and Hf isotope of inherited zircons from the Eocene to Oligocene magmatic rocks
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摘要:
在通过锆石U-Pb方法测定岩浆活动时代的过程中总会获取或多或少的继承锆石年龄数据, 这些数据对于揭示岩浆岩所处构造单元的构造-岩浆事件序列具有独特优势。本文选择印度-欧亚大陆侧向碰撞带内NEE走向的始-渐新世岩浆岩带作为研究对象, 详细收集、梳理该岩浆岩带内现有测年结果中的继承锆石U-Pb年代学和Hf同位素数据, 采用统计分析方法, 尝试探讨被该岩浆岩带穿越的扬子、印支、保山、腾冲地块的构造-岩浆事件及其序列, 对比分析其大地构造亲缘性和地块拼贴历史。继承锆石U-Pb年龄频率分布和Hf同位素数据统计结果显示, 扬子与印支地块记录了相同的晋宁期、加里东期、印支期构造-岩浆事件, 而腾冲与保山地块则记录了相同的加里东期、印支期构造-岩浆事件。结合现有地层学、古生物和古地磁等方面数据, 我们提出扬子-印支与腾冲-保山地块作为两个具有不同结晶基底的独立地块, 分别就位于古生代-早中生代古大洋(原、古特提斯洋)的两侧, 该大洋板块双向俯冲于这两个地块之下, 在两个地块内留下了可高度对比的构造-岩浆事件。由此提出, 正向碰撞带班公湖-怒江缝合带内完备的地质记录与侧向碰撞带之间的关联、哀牢山洋的构造属性等是值得深入探究的重大问题。
Abstract:Most igneous rocks contain some inherited zircons whose age-data are valuable to reveal tectonothermal history of the continental block with these igneous rocks as a by-product of them. A huge NEE-trending Eocene to Oligocene magmatic zone developed in the oblique collision belt in southeastern Tibetan Plateau, where numerous magmatic rocks occurred in the Yangtze, Indochina, Baoshan and Tengchong blocks. This paper collected the available U-Pb dating results and Hf isotopic data of the inherited zircons from the igneous rocks of this magmatic zone. Statistics of these data revealed three tectonothermal events happened in the Yangtze and Indochina blocks during the Neoproterozoic, the Early Paleozoic, and the Late Plaeozoic to Early Mesozoic, respectively; while only two tectonothermal events of the Early Paleozoic and the Late Paleozoic to Early Mesozoic occurred in the Baoshan and Tengchong blocks. These data, combined with the previously published stratigraphic, paleontological and paleomagnetic data, suggest that the Yangtze and Indochina blocks are likely a single block, while the Tengchong and Baoshan blocks belong to another single block. Between them, a long-lived paleo-ocean should exist from the Early Paleozoic to the Early Mesozoic. Two directions subduction of the plaeo-oceanic plate under the Yangtze-Indochina and Tengchong-Baoshan blocks resulted in the highly comparable magmatism histories of the two blocks. Therefore, the geological relationships of the Bangong-Nujiang suture between the orthogonal and oblique collision belts, and the tectonic properties of the Ailaoshan ocean are major issues worthy further studying.
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Key words:
- Statistic analysis /
- Inherited zircons /
- U-Pb ages /
- Hf isotope /
- Tectonothermal events /
- SE Tibetan Plateau
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图 1
青藏高原及其周边地区构造框架图(据任纪舜等, 1999修改)
Figure 1.
Tectonic sketch map of the Tibetan Plateau and its surrounding areas (modified after Ren et al., 1999)
图 2
藏东及藏东南地区构造框架图，示新生代岩浆岩的时-空分布(据Yang et al., 2021修改)
Figure 2.
Tectonic sketch map of the eastern and southeastern Tibetan Plateau, showing the temporal-spatial distribution of Cenozoic magmatic rocks (modified after Yang et al., 2021)
图 3
青藏高原东南缘NEE向岩浆岩带构造简图，示始-渐新世岩浆岩的分布
Figure 3.
Tectonic sketch map of the NEE-trending magmatic zone in the SE Tibetan Plateau, showing the spatial distribution of the Eocene to Oligocene magmatic rocks
图 4
青藏高原东南缘NEE向岩浆岩带内始-渐新世岩浆岩继承锆石U-Pb年龄的频率分布图
Figure 4.
Diagrams showing the frequency distribution of inherited zircon U-Pb ages from the Eocene to Oligocene magmatic rocks in the SE Tibetan Plateau
图 5
青藏高原东南缘NEE向岩浆岩带内始-渐新世岩浆岩继承锆石Hf同位素组成(数据来源于附表 1)
Figure 5.
εHf(t) vs. Age diagram of inherited zircons from the Eocene to Oligocene magmatic rocks of the NEE-trending magmatic zone in the SE Tibetan Plateau (see Appendix Table 1 for data)
图 6
扬子-印支和腾冲-保山地块内始-渐新世岩浆岩继承锆石U-Pb年代学频率分布图
Figure 6.
Diagrams showing frequency distribution of inherited zircon U-Pb ages from the Eocene to Oligocene magmatic rocks in the Yangtze-Indochina blocks (a) and Tengchong-Baoshan blocks (b), respectively
表 附表 1
NEE向岩浆岩带内始-渐新世岩浆岩继承锆石Hf同位素数据
Table 附表 1.
Hf isotope data of inherited zircons from the Eocene to Oligocene magmatic rocks in the NEE-trending magmatic zone
点号 年龄(Ma) 176Yb/177Hf 176Lu/177Hf 176Hf/177Hf (176Hf/177Hf)i εHf(t) tDM(Ma) tDMC(Ma) fLu/Hf 参考文献 扬子地块 1 112.7 0.01552 0.00068 0.28217 0.28216 -19.05 1519 2380 -0.98 Wang et al., 2018 2 113.9 0.02107 0.00082 0.28234 0.28234 -12.84 1281 1989 -0.98 Wang et al., 2018 3 275.6 0.05052 0.00164 0.28276 0.28275 5.19 715 966 -0.95 Wang et al., 2018 4 757.5 0.06523 0.00239 0.28278 0.28275 15.93 690 654 -0.93 Wang et al., 2018 5 762.3 0.03284 0.00128 0.28168 0.28166 -22.51 2220 3075 -0.96 Wang et al., 2018 6 764.8 0.04264 0.00165 0.28175 0.28172 -20.24 2147 2936 -0.95 Wang et al., 2018 7 214.8 0.01361 0.00050 0.28248 0.28248 -5.58 1073 1605 -0.98 Wang et al., 2018 8 207.6 0.06485 0.00243 0.28241 0.28240 -8.65 1239 1794 -0.93 Wang et al., 2018 9 209.8 0.00229 0.00009 0.28229 0.28229 -12.31 1320 2028 -1.00 Wang et al., 2018 10 210.7 0.01203 0.00040 0.28216 0.28216 -17.19 1519 2335 -0.99 Wang et al., 2018 11 213.6 0.00918 0.00034 0.28225 0.28225 -13.93 1393 2132 -0.99 Wang et al., 2018 12 243.1 0.03325 0.00116 0.28238 0.28237 -8.78 1240 1829 -0.97 Wang et al., 2018 13 837.3 0.00538 0.00030 0.28244 0.28244 6.64 1125 1306 -0.99 Wang et al., 2018 14 843.7 0.01395 0.00053 0.28210 0.28209 -5.57 1608 2080 -0.98 Wang et al., 2018 15 112.1 0.03616 0.00144 0.28208 0.28208 -22.05 1667 2567 -0.96 Wang et al., 2018 16 244.7 0.05349 0.00199 0.28268 0.28267 1.73 835 1163 -0.94 Wang et al., 2018 17 629.3 0.01385 0.00050 0.28206 0.28205 -11.63 1660 2299 -0.99 Wang et al., 2018 18 748.4 0.05521 0.00221 0.28218 0.28215 -5.42 1556 1998 -0.93 Wang et al., 2018 19 751.2 0.07920 0.00264 0.28290 0.28287 19.93 517 394 -0.92 Wang et al., 2018 20 897.2 0.03516 0.00136 0.28159 0.28157 -22.90 2351 3198 -0.96 Wang et al., 2018 21 1002 0.00899 0.00031 0.28192 0.28191 -8.36 1845 2374 -0.99 Wang et al., 2018 22 118.9 0.03838 0.00156 0.28230 0.28230 -14.14 1361 2074 -0.95 Wang et al., 2018 23 208 0.00738 0.00027 0.28242 0.28242 -7.92 1154 1749 -0.99 Wang et al., 2018 24 211.2 0.00823 0.00032 0.28224 0.28223 -14.40 1409 2160 -0.99 Wang et al., 2018 25 214.7 0.00236 0.00009 0.28232 0.28232 -11.39 1289 1973 -1.00 Wang et al., 2018 26 258.2 0.05988 0.00254 0.28300 0.28299 13.35 371 430 -0.92 Wang et al., 2018 27 778.5 0.04002 0.00161 0.28212 0.28209 -6.82 1625 2109 -0.95 Wang et al., 2018 28 84.7 0.02721 0.00108 0.28254 0.28253 -6.55 1015 1569 -0.97 Wang et al., 2018 29 217.7 0.00328 0.00011 0.28237 0.28237 -9.49 1218 1855 -1.00 Wang et al., 2018 30 218 0.00477 0.00017 0.28228 0.28228 -12.57 1339 2050 -0.99 Wang et al., 2018 31 218.3 0.03539 0.00139 0.28223 0.28222 -14.65 1459 2181 -0.96 Wang et al., 2018 32 220 0.02396 0.00095 0.28227 0.28226 -13.17 1388 2089 -0.97 Wang et al., 2018 33 363.8 0.02785 0.00113 0.28224 0.28223 -11.20 1437 2072 -0.97 Wang et al., 2018 34 614 0.02599 0.00107 0.28245 0.28244 1.68 1137 1449 -0.97 Wang et al., 2018 35 725.7 0.02390 0.00097 0.28210 0.28209 -8.12 1617 2151 -0.97 Wang et al., 2018 36 660 0.01556 0.00058 0.28243 0.28242 2.14 1152 1455 -0.98 蒋成竹, 2014 37 760 0.05481 0.00198 0.28242 0.28240 3.48 1201 1447 -0.94 蒋成竹, 2014 38 714 0.05309 0.00187 0.28259 0.28256 8.27 966 1108 -0.94 蒋成竹, 2014 39 512 0.04047 0.00127 0.28222 0.28220 -8.86 1473 2036 -0.96 蒋成竹, 2014 40 596 0.03470 0.00120 0.28232 0.28230 -3.51 1330 1762 -0.96 蒋成竹, 2014 41 565 0.04613 0.00158 0.28242 0.28241 -0.45 1188 1546 -0.95 蒋成竹, 2014 42 346 0.01910 0.00075 0.28239 0.28239 -6.04 1208 1733 -0.98 蒋成竹, 2014 43 900 0.01324 0.00053 0.28259 0.28258 13.10 928 946 -0.98 蒋成竹, 2014 44 2427 0.05130 0.00156 0.28120 0.28112 -3.88 2906 3181 -0.95 蒋成竹, 2014 45 788 0.00679 0.00020 0.28218 0.28217 -3.82 1487 1928 -0.99 蒋成竹, 2014 46 587 0.00907 0.00030 0.28214 0.28214 -9.51 1537 2134 -0.99 蒋成竹, 2014 47 677 0.03175 0.00125 0.28242 0.28241 2.03 1179 1475 -0.96 蒋成竹, 2014 48 503 0.01510 0.00048 0.28211 0.28210 -12.65 1592 2268 -0.99 蒋成竹, 2014 49 485 0.06029 0.00208 0.28241 0.28240 -2.65 1219 1624 -0.94 蒋成竹, 2014 50 840 0.03064 0.00095 0.28217 0.28215 -3.27 1523 1933 -0.97 蒋成竹, 2014 51 588 0.01906 0.00063 0.28219 0.28218 -7.88 1483 2032 -0.98 蒋成竹, 2014 52 836 0.03921 0.00117 0.28235 0.28233 2.80 1283 1548 -0.96 蒋成竹, 2014 53 972 0.02015 0.00062 0.28203 0.28202 -5.22 1705 2156 -0.98 蒋成竹, 2014 54 254 0.03303 0.00105 0.28260 0.28259 -0.82 930 1333 -0.97 蒋成竹, 2014 55 1043 0.03269 0.00106 0.28202 0.28200 -4.18 1733 2144 -0.97 蒋成竹, 2014 56 502 0.01159 0.00038 0.28219 0.28218 -9.81 1478 2088 -0.99 蒋成竹, 2014 57 814 0.01922 0.00069 0.28258 0.28257 10.80 945 1025 -0.98 蒋成竹, 2014 58 524 0.01860 0.00063 0.28225 0.28224 -7.14 1400 1937 -0.98 蒋成竹, 2014 59 418 0.03144 0.00104 0.28232 0.28231 -7.04 1315 1851 -0.97 蒋成竹, 2014 60 481 0.01669 0.00062 0.28194 0.28193 -19.12 1828 2657 -0.98 蒋成竹, 2014 61 481 0.01501 0.00051 0.28178 0.28178 -24.61 2036 2999 -0.98 蒋成竹, 2014 62 812 0.09772 0.00343 0.28261 0.28256 10.48 967 1043 -0.90 蒋成竹, 2014 63 285 0.01304 0.00052 0.28170 0.28170 -31.80 2149 3303 -0.98 蒋成竹, 2014 64 735 0.02928 0.00128 0.28261 0.28259 9.81 918 1026 -0.96 蒋成竹, 2014 65 150 0.06099 0.00223 0.28293 0.28293 8.80 466 638 -0.93 蒋成竹, 2014 66 275 0.03850 0.00152 0.28289 0.28288 10.02 517 657 -0.95 蒋成竹, 2014 67 466 0.04816 0.00173 0.28239 0.28237 -3.93 1247 1691 -0.95 蒋成竹, 2014 68 850 0.06714 0.00218 0.28256 0.28252 10.00 1014 1103 -0.93 蒋成竹, 2014 69 793 0.02772 0.00096 0.28243 0.28242 5.02 1156 1374 -0.97 蒋成竹, 2014 70 404 0.04405 0.00161 0.28247 0.28246 -2.29 1126 1540 -0.95 蒋成竹, 2014 71 826 0.01841 0.00069 0.28201 0.28200 -8.95 1727 2279 -0.98 蒋成竹, 2014 72 821 0.06006 0.00222 0.28185 0.28181 -15.75 2035 2698 -0.93 蒋成竹, 2014 73 733 0.01482 0.00055 0.28224 0.28224 -2.80 1406 1822 -0.98 蒋成竹, 2014 74 489 0.06619 0.00228 0.28267 0.28264 6.25 860 1062 -0.93 蒋成竹, 2014 75 850 0.02413 0.00078 0.28188 0.28186 -13.37 1921 2572 -0.98 蒋成竹, 2014 76 642 0.02485 0.00087 0.28242 0.28240 1.16 1179 1503 -0.97 蒋成竹, 2014 77 1517 0.02360 0.00084 0.28179 0.28177 -1.86 2043 2361 -0.97 蒋成竹, 2014 78 333 0.04326 0.00149 0.28267 0.28266 3.25 841 1134 -0.96 蒋成竹, 2014 79 419 0.01489 0.00051 0.28200 0.28199 -18.42 1746 2567 -0.98 蒋成竹, 2014 80 422.4 0.01659 0.00053 0.28230 0.28229 -7.69 1333 1895 -0.98 严清高等, 2019 81 782 0.01634 0.00070 0.28286 0.28285 20.15 547 404 -0.98 沈阳等, 2019 82 210 0.01590 0.00070 0.28265 0.28265 0.20 846 1234 -0.98 韩美芝, 2017 83 856.9 0.03954 0.00127 0.28236 0.28233 3.47 1276 1521 -0.96 Zhou et al., 2019 84 656 0.05183 0.00159 0.28210 0.28208 -9.90 1643 2209 -0.95 Zhou et al., 2019 85 222.8 0.01823 0.00049 0.28268 0.28267 1.39 806 1168 -0.99 Zhou et al., 2019 86 222.8 0.02579 0.00087 0.28285 0.28285 7.56 566 774 -0.97 Zhou et al., 2019 87 1160.3 0.04444 0.00153 0.28207 0.28204 -0.23 1685 1986 -0.95 Zhou et al., 2019 88 293.7 0.00443 0.00012 0.28234 0.28233 -9.03 1265 1883 -1.00 Zhou et al., 2019 89 502.1 0.04104 0.00114 0.28274 0.28272 9.38 735 873 -0.97 Zhou et al., 2019 90 842 0.02412 0.00078 0.28274 0.28272 16.96 725 655 -0.98 Zhou et al., 2019 91 1389.4 0.05991 0.00171 0.28216 0.28212 7.75 1564 1663 -0.95 Zhou et al., 2019 92 241.5 0.01794 0.00062 0.28246 0.28246 -5.90 1111 1646 -0.98 Zhou et al., 2019 93 234 0.03781 0.00115 0.28268 0.28268 1.78 811 1152 -0.97 Zhou et al., 2019 94 245 0.00714 0.00025 0.28277 0.28276 5.13 675 946 -0.99 Zhou et al., 2019 95 260.6 0.02579 0.00087 0.28285 0.28285 8.38 566 751 -0.97 Zhou et al., 2019 96 299.4 0.00443 0.00012 0.28234 0.28233 -8.90 1265 1879 -1.00 Zhou et al., 2019 97 637.6 0.05991 0.00171 0.28216 0.28214 -8.21 1564 2090 -0.95 Zhou et al., 2019 98 777.3 0.03455 0.00099 0.28244 0.28242 4.74 1154 1380 -0.97 Zhou et al., 2019 99 703.5 0.02353 0.00077 0.28240 0.28239 1.94 1199 1500 -0.98 Zhou et al., 2019 100 839.7 0.02248 0.00072 0.28247 0.28246 7.59 1093 1248 -0.98 Zhou et al., 2019 101 806.5 0.02908 0.00092 0.28249 0.28247 7.26 1079 1244 -0.97 Zhou et al., 2019 102 234 0.03190 0.00099 0.28290 0.28290 9.52 499 657 -0.97 Zhou et al., 2019 103 340.8 0.06263 0.00167 0.28227 0.28225 -10.82 1417 2031 -0.95 Zhou et al., 2019 104 1206.6 0.05280 0.00160 0.28219 0.28215 4.93 1519 1699 -0.95 Zhou et al., 2019 105 319 0.04340 0.00045 0.28272 0.28272 5.08 743 1006 -0.99 吴鹏等, 2020 106 760 0.03207 0.00093 0.28231 0.28230 -0.03 1327 1668 -0.97 吴鹏等, 2020 107 757.5 0.09660 0.00056 0.28233 0.28232 0.81 1287 1613 -0.98 吴鹏等, 2020 108 765.8 0.08500 0.00052 0.28230 0.28229 -0.05 1327 1674 -0.98 吴鹏等, 2020 109 773.2 0.03867 0.00220 0.28210 0.28207 -7.84 1675 2168 -0.93 吴鹏等, 2020 印支地块 1 107 0.06218 0.00124 0.28257 0.28256 -4.99 975 1486 -0.96 Miao et al., 2021 2 97 0.05453 0.00115 0.28257 0.28256 -5.27 976 1496 -0.97 Miao et al., 2021 3 99 0.06010 0.00128 0.28258 0.28258 -4.56 953 1453 -0.96 Miao et al., 2021 4 97 0.06514 0.00140 0.28258 0.28258 -4.61 956 1455 -0.96 Miao et al., 2021 5 101 0.11731 0.00233 0.28260 0.28260 -3.95 954 1415 -0.93 Miao et al., 2021 6 93 0.06791 0.00143 0.28256 0.28256 -5.44 986 1504 -0.96 Miao et al., 2021 7 606 0.03317 0.00137 0.28243 0.28241 0.64 1176 1508 -0.96 Li et al., 2021 8 590 0.02807 0.00110 0.28239 0.28238 -0.83 1217 1589 -0.97 Li et al., 2021 9 638 0.04310 0.00174 0.28219 0.28217 -7.29 1528 2033 -0.95 Li et al., 2021 腾冲地块 1 60 0.04021 0.00158 0.28258 0.28258 -5.43 961 1479 -0.95 Xu et al., 2012 2 60.5 0.01808 0.00076 0.28282 0.28282 3.07 606 937 -0.98 Ma et al., 2014 3 78.6 0.02016 0.00072 0.28288 0.28288 5.54 522 793 -0.98 Ma et al., 2014 4 123.2 0.02555 0.00093 0.28291 0.28290 7.33 491 712 -0.97 Ma et al., 2014 5 67.2 0.05215 0.00187 0.28292 0.28292 6.63 482 714 -0.94 Ma et al., 2014 6 230 0.02926 0.00104 0.28275 0.28275 4.12 712 1000 -0.97 Ma et al., 2014 7 120.9 0.02455 0.00100 0.28259 0.28259 -3.76 933 1418 -0.97 Ma et al., 2014 8 447.2 0.02649 0.00099 0.28269 0.28268 6.48 803 1016 -0.97 Ma et al., 2014 9 144 0.02610 0.00080 0.28245 0.28245 -8.34 1129 1727 -0.98 Cao et al., 2017 10 58 0.14458 0.00249 0.28260 0.28260 -4.77 955 1435 -0.93 张诗启等, 2017 11 71 0.05291 0.00089 0.28258 0.28258 -5.31 950 1480 -0.97 张诗启等, 2017 12 71 0.07203 0.00123 0.28255 0.28255 -6.39 1001 1548 -0.96 张诗启等, 2017 13 75 0.11632 0.00196 0.28255 0.28255 -6.27 1018 1543 -0.94 张诗启等, 2017 14 62 0.09345 0.00149 0.28261 0.28260 -4.57 926 1426 -0.96 张诗启等, 2017 15 73 0.07743 0.00128 0.28260 0.28260 -4.44 925 1425 -0.96 张诗启等, 2017 16 69 0.13853 0.00213 0.28255 0.28254 -6.54 1028 1556 -0.94 张诗启等, 2017 17 55 0.15515 0.00245 0.28262 0.28262 -4.22 929 1398 -0.93 张诗启等, 2017 18 73 0.18737 0.00283 0.28261 0.28261 -4.16 951 1407 -0.91 张诗启等, 2017 19 54 0.18896 0.00313 0.28265 0.28265 -3.28 905 1337 -0.91 张诗启等, 2017 20 75 0.09269 0.00157 0.28253 0.28253 -6.85 1031 1580 -0.95 张诗启等, 2017 21 69 0.08452 0.00133 0.28262 0.28262 -3.92 903 1390 -0.96 张诗启等, 2017 22 78.7 0.04411 0.00164 0.28286 0.28286 4.68 568 848 -0.95 Chen et al., 2022a 23 58.2 0.05828 0.00204 0.28280 0.28280 2.33 653 982 -0.94 Chen et al., 2022a 24 69 0.01900 0.00073 0.28293 0.28293 7.07 453 687 -0.98 Chen et al., 2022a 25 364.4 0.00855 0.00031 0.28286 0.28285 10.88 553 671 -0.99 Chen et al., 2022a 26 57 0.04340 0.00156 0.28278 0.28278 1.37 683 1043 -0.95 Chen et al., 2022a 27 98.5 0.03417 0.00117 0.28284 0.28284 4.49 587 875 -0.96 Chen et al., 2022a 
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