## 1D Model for Northeast China, roughly covering the region ## within 110-130E in lon. and 35-45N in lat. ## ## Author: Juan Li ## Email: juanli@mail.iggcas.ac.cn ## ## We get the model from triplication waveform modeling of deep earthquakes. ## The velocity structure around mantle transition zone is well constrained. ## However, the shallow structure cannot be constrained well due to the depth ## distribution of earthquakes used, and we modified this part after ## Fukao et al. (1976) work. ## ## For details, please refer the following articles: ## 1. P and SH velocity structure in the upper mantle beneath Northeast China: ## Evidence for a stagnant slab in hydrous mantlet ransition zone, ## Juan Li, Xin Wang et al., 2013, Earth Plaent. Sci. Lett. 367: 71-81. ## 2. A stagnant slab in a water-bearing mantle transition zone beneath northeast China: ## implications from regional SH waveform modelling, ## Lingling Ye, Juan Li, et al, 2011, Geophys. J. Int. doi:10.1111/j.1365-246X.2011.05063.x ## ## The first 5 values are: No. Depth. Vp Vs Density ## 1 0 5.4 3.36 2.72 1340 600 2 20 5.4 3.36 2.72 1340 600 3 20 6.2 3.75 2.92 1340 600 4 35 6.2 3.75 2.92 1340 600 5 35 8.01 4.47 3.3198 1340 600 6 77.5 8.015 4.485 3.3455 1340 600 7 120 8.05 4.5 3.3713 1340 600 8 165 8.175 4.509 3.3985 250 100 9 210 8.25 4.518 3.4258 250 100 10 210 8.25 4.522 3.4258 360 150 11 260 8.361 4.5429 3.4561 360 150 12 320 8.47 4.61 3.4864 360 150 13 360 8.59 4.69 3.5167 360 150 14 410 8.81 4.80 3.547 360 150 15 410 9.36 5.00 3.7557 360 150 16 450 9.4944 5.07304 3.78678 360 150 17 460 9.5280 5.09130 3.792 360 150 18 500 9.6624 5.16434 3.8498 360 150 19 525 9.76 5.21 3.91282 360 150 20 550 9.89 5.29 3.9400 360 150 21 600 10.15 5.45 3.97584 360 150 22 665 10.24 5.50 4.0646 360 150 23 709 11.03 6.13 4.3714 780 300 24 760 11.06 6.21 4.4305 780 300 25 809.5 11.134 6.2474 4.4596 780 300 26 859 11.21 6.2841 4.4885 780 300 27 908.5 11.314 6.3199 4.5173 780 300 28 958 11.396 6.3546 4.5459 780 300 29 1007.5 11.4761 6.3883 4.5744 780 300 30 1057 11.5543 6.4211 4.6028 780 300 31 1106.5 11.6308 6.453 4.631 780 300 32 1156 11.7056 6.4841 4.6591 780 300 33 1205.5 11.7787 6.5143 4.687 780 300 34 1255 11.8504 6.5438 4.7148 780 300 35 1304.5 11.9205 6.5725 4.7424 780 300 36 1354 11.9893 6.6006 4.7699 780 300 37 1403.5 12.0568 6.628 4.7973 780 300 38 1453 12.1231 6.6547 4.8245 780 300 39 1502.5 12.1881 6.6809 4.8515 780 300 40 1552 12.2521 6.7066 4.8785 780 300 41 1601.5 12.3151 6.7317 4.9052 780 300 42 1651 12.3772 6.7564 4.9319 780 300 43 1700.5 12.4383 6.7807 4.9584 780 300 44 1750 12.4987 6.8046 4.9847 780 300 45 1799.5 12.5584 6.8282 5.0109 780 300 46 1849 12.6174 6.8514 5.037 780 300 47 1898.5 12.6759 6.8745 5.0629 780 300 48 1948 12.7339 6.8972 5.0887 780 300 49 1997.5 12.7915 6.9199 5.1143 780 300 50 2047 12.8487 6.9423 5.1398 780 300 51 2096.5 12.9057 6.9647 5.1652 780 300 52 2146 12.9625 6.987 5.1904 780 300 53 2195.5 13.0192 7.0093 5.2154 780 300 54 2245 13.0758 7.0316 5.2403 780 300 55 2294.5 13.1325 7.054 5.2651 780 300 56 2344 13.1892 7.0765 5.2898 780 300 57 2393.5 13.2462 7.0991 5.3142 780 300 58 2443 13.3034 7.1218 5.3386 780 300 59 2492.5 13.361 7.1449 5.3628 780 300 60 2542 13.419 7.1681 5.3869 780 300 61 2591.5 13.4774 7.1917 5.4108 780 300 62 2641 13.5364 7.2156 5.4345 780 300 63 2690.5 13.5961 7.2398 5.4582 780 300 64 2740 13.6564 7.2645 5.4817 780 300 65 2740 13.6564 7.2645 5.4817 780 300 66 2789.67 13.6679 7.2768 5.5051 780 300 67 2839.33 13.6793 7.2892 5.5284 780 300 68 2889 13.6908 7.3015 5.5515 780 300 69 2889 8.0088 0 9.9145 57822 0