“变革性技术”-揭示三维岩石圈物质架构的理论方法体系
样品名称: T140427-1 唯一ID:2018-0008 .
检索耗时: 0.019秒
| 经度 | 102.196000 |
|---|---|
| 纬度 | 24.720000 |
| 参考文献 | 高林志,张恒,张传恒,丁孝忠,尹崇玉,武振杰,宋彪.2018.滇东昆阳群地层序列的厘定及其在中国地层表的位置[J].地质论评,64(2):283-301 |
| 岩性 | 火山凝灰岩样品 |
| 分析矿物 | Zircon |
| 分析技术 | SHRIMP |
地质年龄
| Age | 2 σ | mswd | Interpretation | approach |
|---|---|---|---|---|
| 892.30 | 4.80 | 1.0 | 0 | 0 |
Spots list:15 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 2018-0008 | 1.1 | 0.38 | None | 126.0 | 110.0 | 0.9 | 913.7 | 0.92 | 0.0 | 0.0 | 980.0 | 3.2 | None | None | 7.0 |
| 2018-0008 | 2.1 | 0.01 | None | 169.0 | 115.0 | 0.7 | 903.7 | 0.81 | 0.0 | 0.0 | 884.0 | 1.5 | None | None | -2.0 |
| 2018-0008 | 3.1 | 0.07 | None | 550.0 | 276.0 | 0.52 | 852.8 | 0.6 | 0.0 | 0.0 | 888.0 | 0.84 | None | None | 4.0 |
| 2018-0008 | 4.1 | 0.33 | None | 602.0 | 428.0 | 0.73 | 669.2 | 1.1 | 0.0 | 0.0 | 770.0 | 1.5 | None | None | 15.0 |
| 2018-0008 | 5.1 | 0.04 | None | 118.0 | 105.0 | 0.92 | 895.7 | 0.94 | 0.0 | 0.0 | 902.0 | 2.4 | None | None | 1.0 |
| 2018-0008 | 6.1 | 0.1 | None | 211.0 | 123.0 | 0.6 | 888.6 | 0.74 | 0.0 | 0.0 | 878.0 | 1.8 | None | None | -1.0 |
| 2018-0008 | 7.1 | 0.23 | None | 161.0 | 143.0 | 0.92 | 899.0 | 1.2 | 0.0 | 0.0 | 921.0 | 2.3 | None | None | 2.0 |
| 2018-0008 | 8.1 | 0.73 | None | 89.0 | 69.0 | 0.8 | 864.7 | 1.1 | 0.0 | 0.0 | 745.0 | 9.2 | None | None | -14.0 |
| 2018-0008 | 9.1 | 0.22 | None | 840.0 | 644.0 | 0.79 | 563.6 | 0.52 | 0.0 | 0.0 | 817.0 | 1.1 | None | None | 45.0 |
| 2018-0008 | 10.1 | 0.0 | None | 102.0 | 70.0 | 0.71 | 886.0 | 1.4 | 0.0 | 0.0 | 923.0 | 1.8 | None | None | 4.0 |
| 2018-0008 | 11.1 | 0.2 | None | 202.0 | 181.0 | 0.93 | 885.3 | 0.77 | 0.0 | 0.0 | 895.0 | 1.8 | None | None | 1.0 |
| 2018-0008 | 12.1 | 0.1 | None | 261.0 | 185.0 | 0.73 | 892.2 | 0.69 | 0.0 | 0.0 | 907.0 | 1.3 | None | None | 2.0 |
| 2018-0008 | 13.1 | 0.36 | None | 153.0 | 110.0 | 0.75 | 893.4 | 0.85 | 0.0 | 0.0 | 844.0 | 2.4 | None | None | -6.0 |
| 2018-0008 | 14.1 | 0.33 | None | 109.0 | 67.0 | 0.63 | 888.0 | 0.96 | 0.0 | 0.0 | 822.0 | 2.5 | None | None | -7.0 |
| 2018-0008 | 15.1 | 0.02 | None | 651.0 | 541.0 | 0.86 | 843.0 | 0.54 | 0.0 | 0.0 | 884.0 | 0.78 | None | None | 5.0 |