The definition and geological significance of tuffs about 1.85Ga in Yimen area, central Yunnan Province
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摘要:
在滇中易门-罗茨断裂带以西前人划分的昆阳群美党组中发现了大量的中酸性凝灰岩。采用锆石激光剥蚀法(LAICP-MS)对易门县铜厂一带的英安质凝灰岩、石英晶屑凝灰岩进行了年龄测定,获得锆石U-Pb年龄加权平均值为1842±26Ma(MSWD=7.6,n=29)和1860±25Ma(MSWD=2.5,n=11)。2件样品的锆石Th/U值为0.2~1.0,且均具清晰的振荡环带结构,为岩浆成因锆石。该套凝灰岩产于一套厚度超过1000m的火山-细碎屑岩组合中,其下发育厚约800m的黑色板岩-碳酸盐岩组合,表明滇中易门地区存在厚度超过2000m的古元古界。此年龄值与全球性的Columbia超大陆事件一致,所以,在进行Columbia超大陆重建时需要充分考虑扬子陆块的位置及意义。
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关键词:
- 古元古界 /
- 锆石U-Pb年龄 /
- 滇中易门地区 /
- Columbia超大陆重建
Abstract:Medium-acid tuff was extensively found in Meidang Formation of Kunyang Group, which was determined by previous researchers in the west of Yimen-Luoci faults belt. Using the zircon laser denudation method (LA-ICP-MS), the authors obtained weighted average ages of 1842±26Ma (MSWD=7.6, n=29) and 1860±25Ma (MSWD=2.5, n=11) from dacitic tuff and quartz crystal tuff in Tongchang area, Yimen County, central Yunnan Province. Th/U ratios of zircon, which was of magmatic origin and with clear vibration band, were obtained from two samples (0.2~1.0). The tuff was found from a volcanic-microclastic rock assembly, which is over 1000m in thickness. There is a black slate-carbonate rock assembly, which is about 800m in thickness, under the volcanic-microclastic rock assembly. It is thus inferred that there is a large area of Paleoproterozoic strata, which are over 2000m in thickness in Yimen area of central Yunnan Province. The ages coincide with Columbia Supercontinent, and hence Yangtze block's location and significance ought to be taken into account in the reconstruction process of Columbia Supercontinent.
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致谢: 锆石LA-ICP-MS分析和阴极发光照片得到南京宏创地质勘查技术服务有限公司袁秋云及湖北省地质实验室测试中心岩石矿物研究室朱丹、潘诗洋的帮助,审稿专家提出了宝贵的修改意见,在此一并表示衷心感谢。
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表 1 LA-ICP-MS锆石U-Th-Pb同位素分析数据
Table 1 LA-ICP-MS zircon U-Th-Pb data
测号 Th/U 同位素比值 年龄/Ma 207Pb/206Pb 1σ 207Pb/235Pb 1σ 206Pb/238Pb 1σ 207Pb/206Pb 1σ 207Pb/235Pb 1σ 206Pb/238Pb 1σ 1 0.6 0.1382 0.0016 8.3694 0.1011 0.4363 0.0027 2206 20.4 2272 11.1 2334 12.2 2 0.8 0.1352 0.0016 7.7280 0.0937 0.4124 0.0027 2169 20.8 2200 11.0 2226 12.2 3 0.3 0.1118 0.0012 5.2939 0.0553 0.3407 0.0018 1829 19.6 1868 9.0 1890 8.7 4 0.8 0.1388 0.0016 8.1023 0.0943 0.4202 0.0025 2213 19.8 2243 10.6 2261 11.6 5 1.0 0.1548 0.0017 10.3969 0.1136 0.4833 0.0028 2400 18.5 2471 10.3 2542 12.4 6 0.5 0.1134 0.0014 5.4495 0.0648 0.3462 0.0022 1854 21.8 1893 10.3 1916 10.7 7 0.9 0.1343 0.0017 7.5660 0.095 0.4053 0.0026 2155 21.9 2181 11.4 2194 12.2 8 0.4 0.1207 0.0017 6.1097 0.0841 0.3643 0.0025 1966 24.2 1992 12.1 2003 11.8 9 0.7 0.1335 0.0019 7.4084 0.1053 0.4002 0.003 2144 24.5 2162 12.8 2170 13.7 10 0.4 0.1110 0.0014 5.2606 0.0658 0.3409 0.0022 1816 22.1 1862 10.7 1891 10.4 11 0.3 0.1132 0.0015 5.3696 0.0694 0.3418 0.0021 1851 24.2 1880 11.1 1895 10.3 12 0.4 0.1265 0.0016 6.6901 0.0870 0.3816 0.0026 2050 22.4 2071 11.6 2084 12 13 0.3 0.1157 0.0016 5.4813 0.0748 0.3415 0.0022 1891 25.2 1898 11.8 1894 10.6 14 0.7 0.1385 0.0021 7.9141 0.1187 0.4127 0.0030 2209 25.9 2221 13.6 2227 13.7 15 0.5 0.1282 0.0019 6.8340 0.1042 0.3850 0.0028 2074 26.5 2090 13.6 2099 13.0 16 1.0 0.1394 0.0026 7.8294 0.1435 0.4073 0.0035 2220 31.8 2212 16.6 2202 16.1 17 0.3 0.1257 0.0020 6.7690 0.1124 0.3889 0.0029 2039 34.1 2082 14.8 2118 13.7 18 0.9 0.1181 0.0020 5.8035 0.0989 0.3549 0.0028 1928 29.8 1947 14.8 1958 13.3 19 0.3 0.1142 0.0017 5.4429 0.0801 0.3437 0.0023 1933 25.9 1892 12.7 1904 11.1 20 1.0 0.1171 0.0017 5.7942 0.0878 0.3570 0.0026 1922 25.8 1946 13.2 1968 12.6 21 0.7 0.1190 0.0018 6.0879 0.0972 0.3687 0.0027 1940 27.9 1989 14.0 2023 12.8 22 0.4 0.1110 0.0018 5.3492 0.0882 0.3475 0.0026 1817 28.6 1877 14.2 1923 12.4 23 0.6 0.1288 0.0023 7.1069 0.1268 0.3982 0.0033 2081 36.3 2125 15.9 2161 15.2 24 0.3 0.1251 0.0023 6.4311 0.1210 0.3704 0.0031 2031 31.9 2037 16.6 2031 14.6 25 0.2 0.1181 0.0018 5.9243 0.0915 0.3610 0.0026 1928 26.7 1965 13.5 1987 12.2 26 0.4 0.1136 0.0017 5.3546 0.0812 0.3398 0.0024 1857 27.5 1878 13.0 1886 11.5 27 0.3 0.1253 0.0018 6.6377 0.0977 0.3815 0.0027 2035 25.9 2064 13.1 2083 12.6 28 0.7 0.1338 0.0019 7.5402 0.1080 0.4056 0.0028 2150 25.0 2178 12.9 2195 12.7 29 0.6 0.1296 0.0020 7.1867 0.1101 0.3999 0.0029 2092 27.9 2135 13.7 2168 13.6 30 0.9 0.1605 0.0025 10.6557 0.1636 0.4780 0.0035 2461 25.9 2494 14.3 2518 15.4 31 0.5 0.1223 0.0018 6.1429 0.0859 0.3622 0.0026 1991 25.9 1996 12.3 1993 12.2 32 0.7 0.1119 0.0018 5.1603 0.0827 0.3331 0.0027 1831 25.0 1846 13.7 1853 13.1 33 0.7 0.1358 0.0017 7.5805 0.0954 0.4018 0.0028 2176 21.1 2183 11.4 2178 12.9 34 0.5 0.1397 0.0018 7.9728 0.1031 0.4114 0.0030 2233 22.2 2228 11.8 2221 13.7 35 0.5 0.1158 0.0014 5.4629 0.0686 0.3393 0.0021 1892 22.5 1895 10.9 1883 10.1 36 0.3 0.1161 0.0014 5.5639 0.0667 0.3446 0.0021 1898 22.2 1911 10.4 1909 10.1 样品D002(英安质凝灰岩) 1 0.7 0.1409 0.0021 8.0011 0.1425 0.4123 0.0061 2239 25.9 2231 16.1 2225 27.7 2 0.8 0.1135 0.0019 5.0138 0.0992 0.3212 0.0053 1857 31.2 1822 16.8 1796 26.0 3 0.7 0.1119 0.0019 5.2508 0.1093 0.3413 0.0062 1831 31.2 1861 17.8 1893 30.0 4 0.5 0.1180 0.0015 5.8548 0.1007 0.3600 0.0057 1928 23.3 1955 15.0 1982 27.2 5 0.5 0.1106 0.0018 4.9070 0.0999 0.3220 0.0053 1809 25.0 1803 17.2 1799 26.1 6 0.5 0.1137 0.0019 5.3428 0.1229 0.3401 0.0055 1858 36.1 1876 19.7 1887 26.3 7 0.5 0.1107 0.0017 5.2445 0.1053 0.3439 0.0063 1813 27.9 1860 17.2 1906 30.4 8 0.6 0.1125 0.0019 5.0557 0.1008 0.3262 0.0056 1840 30.2 1829 16.9 1820 27.3 9 0.9 0.1180 0.0018 5.8482 0.1163 0.3596 0.0065 1928 27.6 1954 17.3 1980 30.8 10 0.5 0.1121 0.0021 5.1119 0.1224 0.3311 0.0065 1833 67.4 1838 20.4 1844 31.7 11 0.7 0.1116 0.0015 5.1392 0.0868 0.3344 0.0057 1828 19.9 1843 14.4 1860 27.5 12 0.5 0.1497 0.0018 8.8076 0.1652 0.4256 0.0070 2343 19.3 2318 17.2 2286 31.7 13 0.6 0.1104 0.0018 5.4049 0.1133 0.3563 0.0076 1806 29.8 1886 18.0 1965 36.0 14 0.8 0.1091 0.0015 5.3071 0.0985 0.3527 0.006 1784 25.5 1870 15.9 1947 28.6 15 1.1 0.1503 0.0017 9.3232 0.1306 0.4498 0.0063 2349 18.7 2370 12.9 2395 28.1 16 0.5 0.1094 0.0017 5.0522 0.0882 0.3354 0.0053 1791 27.5 1828 14.8 1864 25.4 17 1.0 0.1188 0.0017 5.6021 0.1180 0.3423 0.0062 1939 27.0 1916 18.2 1898 29.8 18 1.1 0.1197 0.0020 5.8455 0.1253 0.3532 0.0052 1951 29.6 1953 18.6 1950 24.8 19 0.7 0.1299 0.0044 5.9000 0.2902 0.3236 0.0066 2098 65.3 1961 42.7 1807 32.0 20 0.6 0.1149 0.0018 5.6593 0.1031 0.3570 0.0052 1880 28.4 1925 15.8 1968 24.9 21 0.9 0.1165 0.0016 5.7564 0.0970 0.3573 0.0046 1903 24.1 1940 14.6 1969 22.1 22 0.6 0.1081 0.0015 4.9254 0.0944 0.3291 0.0047 1769 25.9 1807 16.2 1834 23.1 23 0.7 0.1090 0.0018 4.9367 0.1036 0.3288 0.0066 1783 29.6 1809 17.8 1832 32.2 24 0.7 0.1096 0.0018 5.2081 0.1064 0.3437 0.0061 1794 34.3 1854 17.5 1904 29.1 25 0.6 0.1106 0.0016 4.8923 0.0953 0.3201 0.0054 1809 26.1 1801 16.5 1790 26.2 26 0.7 0.1090 0.0016 4.8577 0.0814 0.3227 0.0048 1784 21.5 1795 14.2 1803 23.3 27 0.6 0.1114 0.0018 4.9448 0.0994 0.3212 0.0052 1821 27.6 1810 17.0 1796 25.2 28 0.5 0.1100 0.0015 5.0148 0.0811 0.3303 0.0048 1800 25.3 1822 13.7 1840 23.5 29 0.6 0.1097 0.0019 4.8976 0.1133 0.3227 0.0055 1795 31.5 1802 19.5 1803 26.7 30 0.5 0.1447 0.0019 8.8696 0.1294 0.4437 0.0057 2284 22.5 2325 13.4 2367 25.3 31 1.6 0.1413 0.0019 7.9721 0.1326 0.4084 0.0061 2244 56.6 2228 15.1 2208 28.2 32 0.6 0.1109 0.0016 4.8997 0.0913 0.3193 0.0046 1815 25.6 1802 15.8 1786 22.5 33 0.5 0.1150 0.0017 5.0421 0.0956 0.3170 0.0047 1880 26.4 1826 16.1 1775 23.1 34 1.5 0.1524 0.0024 9.3652 0.1780 0.4471 0.0089 2373 26.9 2374 17.5 2382 39.6 35 0.6 0.1374 0.0019 7.6226 0.1373 0.4017 0.0061 2195 23.0 2188 16.2 2177 28.1 36 0.8 0.1216 0.0012 6.0853 0.0853 0.3617 0.0041 1981 18.2 1988 12.3 1990 19.6 37 0.8 0.1181 0.0013 5.5635 0.0811 0.3408 0.0040 1928 19.8 1910 12.6 1891 19.4 -
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