样品名称: 112PII14 唯一ID:2018-0026 .
检索耗时: 0.021秒
经度 | 115.974700 |
---|---|
纬度 | 30.320000 |
参考文献 | 李远,刘贻灿,杨阳,等.大别山宿松变质带花岗片麻岩的锆石U-Pb年龄和Hf同位素成分[J].地球科学与环境学报,2018,40(01):61-75. |
岩性 | 花岗片麻岩样品 |
分析矿物 | Zircon |
分析技术 | SHRIMP |
地质年龄
Age | 2 σ | mswd | Interpretation | approach |
---|---|---|---|---|
740.00 | 8.00 | 1.0 | 0 | 0 |
Spots list:19 items
# | spot_no | Pbc | Pb* | U | Th | Th/U | 206Pb/238U Age | 1δ Error | 207Pb/235U Age | 1δ Error | 207Pb/206Pb Age | 1δ Error | 208Pb/232Th Age | 1δ Error | Disconcordance |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2018-0026 | 1112PII14-1.1 | 103.17 | None | 81.79 | 41.6 | 0.82 | 2471.0 | 0.0061 | 0.0 | 0.0 | 2480.0 | 0.0023 | None | None | None |
2018-0026 | 1112PII14-2.1 | 281.65 | None | 144.55 | 97.7 | 0.53 | 2184.0 | 0.0033 | 0.0 | 0.0 | 2433.0 | 0.0015 | None | None | None |
2018-0026 | 1112PII14-3.1 | 305.77 | None | 161.43 | 23.2 | 0.55 | 544.0 | 0.0009 | 0.0 | 0.0 | 727.0 | 0.002 | None | None | None |
2018-0026 | 1112PII14-4.1 | 493.38 | None | 459.38 | 56.6 | 0.96 | 807.0 | 0.001 | 0.0 | 0.0 | 911.0 | 0.0011 | None | None | None |
2018-0026 | 1112PII14-5.1 | 18.2 | None | 152.98 | 219.92 | 1.49 | 827.0 | 0.0021 | 0.0 | 0.0 | 720.0 | 0.003 | None | None | None |
2018-0026 | 1112PII14-6.1 | 59.4 | None | 537.75 | 459.14 | 0.88 | 778.0 | 0.001 | 0.0 | 0.0 | 779.0 | 0.0014 | None | None | None |
2018-0026 | 1112PII14-7.1 | 25.6 | None | 243.36 | 208.26 | 0.88 | 740.0 | 0.0015 | 0.0 | 0.0 | 889.0 | 0.0029 | None | None | None |
2018-0026 | 1112PII14-8.1 | 63.6 | None | 626.55 | 642.45 | 1.06 | 716.0 | 0.0009 | 0.0 | 0.0 | 738.0 | 0.0017 | None | None | None |
2018-0026 | 1112PII14-9.1 | 50.8 | None | 471.64 | 385.99 | 0.85 | 757.0 | 0.001 | 0.0 | 0.0 | 729.0 | 0.0021 | None | None | None |
2018-0026 | 1112PII14-10.1 | 3.62 | None | 86.82 | 9.4 | 0.11 | 305.0 | 0.0013 | 0.0 | 0.0 | 987.0 | 0.0051 | None | None | None |
2018-0026 | 1112PII14-11.1 | 8.34 | None | 72.9 | 59.89 | 0.85 | 757.0 | 0.0027 | 0.0 | 0.0 | 589.0 | 0.0089 | None | None | None |
2018-0026 | 1112PII14-12.1 | 53.8 | None | 470.57 | 374.08 | 0.82 | 804.0 | 0.0009 | 0.0 | 0.0 | 742.0 | 0.001 | None | None | None |
2018-0026 | 1112PII14-13.1 | 25.5 | None | 226.22 | 108.8 | 0.5 | 792.0 | 0.0018 | 0.0 | 0.0 | 819.0 | 0.0027 | None | None | None |
2018-0026 | 1112PII14-14.1 | 80.8 | None | 617.44 | 507.88 | 0.85 | 909.0 | 0.0009 | 0.0 | 0.0 | 903.0 | 0.0014 | None | None | None |
2018-0026 | 1112PII14-15.1 | 27.1 | None | 71.66 | 43.05 | 0.62 | 2344.0 | 0.0061 | 0.0 | 0.0 | 2349.0 | 0.003 | None | None | None |
2018-0026 | 1112PII14-16.1 | 13.0 | None | 130.74 | 149.42 | 1.18 | 685.0 | 0.0017 | 0.0 | 0.0 | 822.0 | 0.008 | None | None | None |
2018-0026 | 1112PII14-17.1 | 20.1 | None | 169.33 | 173.09 | 1.06 | 831.0 | 0.0015 | 0.0 | 0.0 | 943.0 | 0.0021 | None | None | None |
2018-0026 | 1112PII14-18.1 | 10.7 | None | 136.88 | 129.54 | 0.98 | 559.0 | 0.0012 | 0.0 | 0.0 | 608.0 | 0.0032 | None | None | None |
2018-0026 | 1112PII14-19.1 | 43.9 | None | 367.56 | 286.09 | 0.8 | 838.0 | 0.001 | 0.0 | 0.0 | 855.0 | 0.0015 | None | None | None |