“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: J01-TW1 唯一ID:2018-0003 .
检索耗时: 0.020秒
| 经度 | 116.479500 |
|---|---|
| 纬度 | 23.740000 |
| 参考文献 | 范飞鹏,肖惠良,陈乐柱,李海立,蔡逸涛,康丛轩,朱意萍,刘建雄,邓中林,李少斌,林耿伟,周霞,肖凡.2018.粤东鸿沟山金矿区流纹斑岩锆石ZirconSHRIMPU-Pb定年、Lu-Hf同位素组成及其地质意义[J].地质论评,64(1):213-226 |
| 岩性 | 流纹斑岩 |
| 分析矿物 | Zircon |
| 分析技术 | SHRIMP |
地质年龄
| Age | 2 σ | mswd | Interpretation | approach |
|---|---|---|---|---|
| 169.10 | 1.50 | 1.3 | 0 | 0 |
Spots list:20 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 2018-0003 | 1.1 | 2.59 | None | 112.0 | 42.0 | 0.38 | 0.02688 | 1.7 | 0.0 | 0.0 | 168.9 | 6.2 | None | None | 98.95 |
| 2018-0003 | 2.1 | 9.0 | None | 386.0 | 161.0 | 0.43 | 0.02716 | 1.3 | 0.0 | 0.0 | 166.9 | 2.5 | None | None | 96.75 |
| 2018-0003 | 3.1 | 6.5 | None | 284.0 | 66.0 | 0.24 | 0.02657 | 1.9 | 0.0 | 0.0 | 177.1 | 2.9 | None | None | 104.55 |
| 2018-0003 | 4.1 | 3.72 | None | 147.0 | 73.0 | 0.51 | 0.02723 | 1.5 | 0.0 | 0.0 | 183.5 | 5.7 | None | None | 106.93 |
| 2018-0003 | 5.1 | 5.24 | None | 225.0 | 71.0 | 0.33 | 0.02707 | 1.4 | 0.0 | 0.0 | 138.8 | 3.3 | None | None | 81.6 |
| 2018-0003 | 6.1 | 10.4 | None | 457.0 | 133.0 | 0.3 | 0.02638 | 1.3 | 0.0 | 0.0 | 158.2 | 2.3 | None | None | 94.73 |
| 2018-0003 | 7.1 | 3.57 | None | 159.0 | 68.0 | 0.44 | 0.02603 | 1.6 | 0.0 | 0.0 | 151.5 | 3.7 | None | None | 92.15 |
| 2018-0003 | 8.1 | 6.29 | None | 311.0 | 95.0 | 0.31 | 0.02344 | 1.6 | 0.0 | 0.0 | 160.9 | 3.8 | None | None | 107.2 |
| 2018-0003 | 9.1 | 3.41 | None | 148.0 | 64.0 | 0.45 | 0.02674 | 2.1 | 0.0 | 0.0 | 195.3 | 4.2 | None | None | 113.48 |
| 2018-0003 | 10.1 | 5.26 | None | 231.0 | 71.0 | 0.32 | 0.0265 | 1.4 | 0.0 | 0.0 | 179.9 | 6.8 | None | None | 106.45 |
| 2018-0003 | 11.1 | 11.6 | None | 507.0 | 222.0 | 0.45 | 0.02666 | 1.3 | 0.0 | 0.0 | 167.8 | 2.1 | None | None | 99.0 |
| 2018-0003 | 12.1 | 5.31 | None | 231.0 | 95.0 | 0.42 | 0.02669 | 1.9 | 0.0 | 0.0 | 170.0 | 3.2 | None | None | 100.06 |
| 2018-0003 | 13.1 | 4.84 | None | 140.0 | 66.0 | 0.49 | 0.04029 | 1.5 | 0.0 | 0.0 | 263.2 | 3.4 | None | None | 103.01 |
| 2018-0003 | 14.1 | 3.37 | None | 149.0 | 48.0 | 0.33 | 0.02621 | 1.6 | 0.0 | 0.0 | 130.6 | 5.7 | None | None | 79.49 |
| 2018-0003 | 15.1 | 3.49 | None | 355.0 | 113.0 | 0.33 | 0.02779 | 1.4 | 0.0 | 0.0 | 174.8 | 2.6 | None | None | 99.04 |
| 2018-0003 | 16.1 | 7.15 | None | 308.0 | 115.0 | 0.39 | 0.02704 | 1.4 | 0.0 | 0.0 | 165.3 | 2.7 | None | None | 96.5 |
| 2018-0003 | 17.1 | 7.39 | None | 313.0 | 122.0 | 0.4 | 0.02757 | 1.4 | 0.0 | 0.0 | 178.5 | 2.6 | None | None | 102.0 |
| 2018-0003 | 18.1 | 3.55 | None | 157.0 | 71.0 | 0.47 | 0.02618 | 1.6 | 0.0 | 0.0 | 143.9 | 4.3 | None | None | 86.79 |
| 2018-0003 | 19.1 | 3.63 | None | 164.0 | 73.0 | 0.46 | 0.02564 | 1.5 | 0.0 | 0.0 | 203.6 | 4.3 | None | None | 122.65 |
| 2018-0003 | 20.1 | 6.74 | None | 296.0 | 119.0 | 0.41 | 0.0265 | 1.4 | 0.0 | 0.0 | 187.8 | 2.8 | None | None | 111.19 |