China Seismological Reference Model (CSRM) - Models and Datasets
- 1. University of Science and Technology of China (中国科学技术大学)
Description
Reference Models:
- CSRM-1.0 [Link]
Pre-CSRM and CSRM-derived models:
- Seismic model of the shallow crust in continental China [Link]
- An uppermost mantle seismic Pn-velocity in continental China [Link]
- Crustal average Vp/Vs model in continental China [Link]
- A composition model of crust beneath continental China [Link]
Database (Level 2):
Level 2 database contains processed seismic data and seismic constraints used for the construction of the "China Seismological Reference Model". The Level 2 data are for personal use only. They should not be redistributed and should not be used for any commercial purposes.
- P-wave polarization angle [Link]
- Short-period Rayleigh wave ellipticity (4 - 8 s) [Link]
- Stacked receiver function [Link]
- Pn travel time [Link]
- Pn travel time in the crust beneath station [Link]
- Pn travel time in the crust beneath seismic event [Link]
- Epicenter location of event initiation point [Link]
- Long-period Rayleigh wave ellipticity (20 - 80 s) [Link]
- Isotropic receiver function (2 - 12 s) [Link]
- Inter-station empirical Green's functions [Link]
- Event-station Rayleigh wave phase and group velocity dispersion curves [Link]
- Rayleigh wave phase/group velocity maps (8 - 70 s) [Link]
- Raw receiver functions (0 - 35 s) [Link]
- Seismometer orientation measurements [Link]
Database (Level 1) [Policy of data usage]
Level 1 database contains the original seismic data that Level 2 datasets were derived from.
- P-wave polarization angle [Link]
- Short-period Rayleigh wave ellipticity (4 - 8 s) [Link]
- Stacked receiver function [Link]
- Pn travel time [Link]
- Pn travel time in the crust beneath station [Link]
- Pn travel time in the crust beneath seismic event [Link]
- Epicenter location of event initiation point [Link]
- Long-period Rayleigh wave ellipticity (20 - 80 s) [Link]
- Isotropic receiver function (2 - 12 s) [Link]
- Inter-station empirical Green's functions [Link]
- Event-station Rayleigh wave phase and group velocity dispersion curves [Link]
- Rayleigh wave phase/group velocity maps (8 - 70 s) [Link]
- Raw receiver functions (0 - 35 s) [Link]
- Seismometer orientation measurements [Link]
Citation of the Level 2 database:
Wen, L. X., and Yu, S. (2023). The China Seismological Reference Model project. Earth Planet. Phys., 7(5), 521–532. doi: 10.26464/epp2023078
_______________________________________________________________________________________________________________________
参考模型:
- CSRM-1.0 [链接]
预构建模型和导出模型:
Level 2 数据库:
Level 2 数据库包含经过处理的地震数据和用于构建 “中国区域地震学参考模型” 的地震学约束。Level 2 数据库仅限于个人使用,不得分发和用于任何商业目的。
- P 波偏振角度 [链接]
- 短周期瑞利波椭率 (4 - 8 s) [链接]
- 叠加接收函数 [链接]
- Pn 走时 [链接]
- 台站下方壳内 Pn 波走时 [链接]
- 震源下方壳内 Pn 波走时 [链接]
- 地震起破点水平位置 [链接]
- 长周期瑞利波椭率 (20 - 80 s) [链接]
- 各向同性接收函数 (2 - 12 s) [链接]
- 台站间经验格林函数 [链接]
- 事件-台站间瑞利波相/群速度频散曲线 [链接]
- 瑞利波相/群速度图 (8 - 70 s) [链接]
- 原始接收函数 (0 - 35 s) [链接]
- 地震计方位测量 [链接]
Level 1 数据库 [数据使用政策]
Level 1 数据库包含 Level 2 数据库中用到的原始地震数据。
- P 波偏振角度 [链接]
- 短周期瑞利波椭率 (4 - 8 s) [链接]
- 叠加接收函数 [链接]
- Pn 走时 [链接]
- 台站下方壳内 Pn 波走时 [链接]
- 震源下方壳内 Pn 波走时 [链接]
- 地震起破点水平位置 [链接]
- 长周期瑞利波椭率 (20 - 80 s) [链接]
- 各向同性接收函数 (2 - 12 s) [链接]
- 台站间经验格林函数 [链接]
- 事件-台站间瑞利波相/群速度频散曲线 [链接]
- 瑞利波相/群速度图 (8 - 70 s) [链接]
- 原始接收函数 (0 - 35 s) [链接]
- 地震计方位测量 [链接]
Level 2 数据库引用:
Wen, L. X., and Yu, S. (2023). The China Seismological Reference Model project. Earth Planet. Phys., 7(5), 521–532. doi: 10.26464/epp2023078
Notes
Files
ContactUs.md
Files
(848 Bytes)
Name | Size | Download all |
---|---|---|
md5:2dbe872f7c84fe6188d64fa4c28aad8c
|
848 Bytes | Preview Download |
Additional details
References
- Wen, L. X., and Yu, S. (2023). The China Seismological Reference Model project. Earth Planet. Phys., 7(5), 521–532. doi: 10.26464/epp2023078