“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: JD03-7 唯一ID:2018-0010 .
检索耗时: 0.020秒
| 经度 | 118.102600 |
|---|---|
| 纬度 | 40.310000 |
| 参考文献 | 耿元生,杨崇辉,杜利林,任留东,宋会侠.2018.冀东地区新太古代晚期的岩浆事件与地壳增生:来自岩石地球化学和锆石年龄及Hf同位素的制约.岩石学报,34(4):1058-1082 |
| 岩性 | 含榴角闪斜长片麻岩 |
| 分析矿物 | Zircon |
| 分析技术 | SHRIMP |
地质年龄
| Age | 2 σ | mswd | Interpretation | approach |
|---|---|---|---|---|
| 2493.00 | 11.00 | 1.0 | 0 | 0 |
Spots list:30 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 2018-0010 | -1.1 | 0.0 | None | 551.0 | 8.0 | 0.02 | 2525.0 | 1.9 | 0.0 | 0.0 | 2482.0 | 0.4 | None | None | -2.0 |
| 2018-0010 | -1.2 | 0.0 | None | 125.0 | 103.0 | 0.85 | 2571.0 | 2.1 | 0.0 | 0.0 | 2462.0 | 1.0 | None | None | -4.0 |
| 2018-0010 | -2.1 | 0.0 | None | 315.0 | 4.0 | 0.01 | 2499.0 | 2.0 | 0.0 | 0.0 | 2505.0 | 0.53 | None | None | 0.0 |
| 2018-0010 | -2.2 | 0.0 | None | 11.0 | 3.0 | 0.33 | 2688.0 | 4.5 | 0.0 | 0.0 | 2438.0 | 5.2 | None | None | -10.0 |
| 2018-0010 | -3.1 | 0.0 | None | 28.0 | 4.0 | 0.14 | 2489.0 | 3.0 | 0.0 | 0.0 | 2436.0 | 2.3 | None | None | -2.0 |
| 2018-0010 | -4.1 | 0.0 | None | 312.0 | 11.0 | 0.03 | 2424.0 | 2.0 | 0.0 | 0.0 | 2485.0 | 0.62 | None | None | 2.0 |
| 2018-0010 | -4.2 | 0.0 | None | 34.0 | 29.0 | 0.89 | 2324.0 | 2.7 | 0.0 | 0.0 | 2499.0 | 2.0 | None | None | 7.0 |
| 2018-0010 | -5.1 | 0.0 | None | 325.0 | 41.0 | 0.13 | 2479.0 | 2.1 | 0.0 | 0.0 | 2460.0 | 0.53 | None | None | -1.0 |
| 2018-0010 | -5.2 | 0.0 | None | 55.0 | 63.0 | 1.18 | 2299.0 | 2.7 | 0.0 | 0.0 | 2374.0 | 1.5 | None | None | 3.0 |
| 2018-0010 | -6.1 | 0.0 | None | 185.0 | 109.0 | 0.61 | 2623.0 | 2.1 | 0.0 | 0.0 | 2511.0 | 1.1 | None | None | -4.0 |
| 2018-0010 | -7.1 | 0.0 | None | 275.0 | 13.0 | 0.05 | 2350.0 | 2.0 | 0.0 | 0.0 | 2332.0 | 0.61 | None | None | -1.0 |
| 2018-0010 | -8.1 | 0.0 | None | 444.0 | 29.0 | 0.07 | 2550.0 | 2.0 | 0.0 | 0.0 | 2512.0 | 0.47 | None | None | -2.0 |
| 2018-0010 | -8.2 | 0.0 | None | 13.0 | 2.0 | 0.18 | 2537.0 | 4.0 | 0.0 | 0.0 | 2569.0 | 3.8 | None | None | 1.0 |
| 2018-0010 | -9.1 | 0.0 | None | 264.0 | 9.0 | 0.03 | 2439.0 | 2.0 | 0.0 | 0.0 | 2445.0 | 0.6 | None | None | 0.0 |
| 2018-0010 | -9.2 | 0.0 | None | 465.0 | 10.0 | 0.02 | 2634.0 | 2.0 | 0.0 | 0.0 | 2492.0 | 0.56 | None | None | -6.0 |
| 2018-0010 | -10.1 | 0.0 | None | 1065.0 | 4.0 | 0.0 | 2463.0 | 1.9 | 0.0 | 0.0 | 2486.0 | 0.35 | None | None | 1.0 |
| 2018-0010 | -11.1 | 0.0 | None | 562.0 | 27.0 | 0.05 | 2497.0 | 1.9 | 0.0 | 0.0 | 2465.0 | 0.41 | None | None | -1.0 |
| 2018-0010 | -11.2 | 0.0 | None | 23.0 | 9.0 | 0.4 | 2420.0 | 3.3 | 0.0 | 0.0 | 2408.0 | 2.5 | None | None | -1.0 |
| 2018-0010 | -12.1 | 0.0 | None | 11.0 | 3.0 | 0.31 | 2391.0 | 6.0 | 0.0 | 0.0 | 1896.0 | 7.3 | None | None | -26.0 |
| 2018-0010 | -13.1 | 0.0 | None | 214.0 | 31.0 | 0.15 | 2579.0 | 2.1 | 0.0 | 0.0 | 2495.0 | 0.66 | None | None | -3.0 |
| 2018-0010 | -13.2 | 0.0 | None | 33.0 | 12.0 | 0.38 | 2553.0 | 2.8 | 0.0 | 0.0 | 2547.0 | 1.9 | None | None | 0.0 |
| 2018-0010 | -14.1 | 0.0 | None | 715.0 | 11.0 | 0.02 | 2558.0 | 1.9 | 0.0 | 0.0 | 2512.0 | 0.35 | None | None | -2.0 |
| 2018-0010 | -15.1 | 0.0 | None | 2417.0 | 307.0 | 0.13 | 2294.0 | 1.9 | 0.0 | 0.0 | 2512.0 | 0.33 | None | None | 9.0 |
| 2018-0010 | -15.2 | 0.0 | None | 48.0 | 5.0 | 0.11 | 2400.0 | 4.2 | 0.0 | 0.0 | 2368.0 | 1.7 | None | None | -1.0 |
| 2018-0010 | -16.1 | 0.0 | None | 427.0 | 6.0 | 0.01 | 2607.0 | 2.0 | 0.0 | 0.0 | 2511.0 | 0.71 | None | None | -4.0 |
| 2018-0010 | -17.1 | 0.0 | None | 487.0 | 25.0 | 0.05 | 2558.0 | 2.0 | 0.0 | 0.0 | 2470.0 | 0.47 | None | None | -4.0 |
| 2018-0010 | -17.2 | 0.0 | None | 115.0 | 7.0 | 0.07 | 2324.0 | 2.2 | 0.0 | 0.0 | 2515.0 | 1.6 | None | None | 8.0 |
| 2018-0010 | -18.1 | 0.0 | None | 19.0 | 10.0 | 0.56 | 2486.0 | 3.5 | 0.0 | 0.0 | 2484.0 | 2.7 | None | None | 0.0 |
| 2018-0010 | -19.1 | 0.0 | None | 624.0 | 42.0 | 0.07 | 2315.0 | 2.1 | 0.0 | 0.0 | 2417.0 | 0.41 | None | None | 4.0 |
| 2018-0010 | -20.1 | 0.0 | None | 22.0 | 24.0 | 1.12 | 2465.0 | 3.2 | 0.0 | 0.0 | 2363.0 | 4.1 | None | None | -4.0 |