Mantle Transition Zone Beneath Hainan Island and Its Surrounding Areas Revealed by Receiver Function Analysis
Authors/Creators
- 1. National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing, China
- 2. Department of Geophysics, Graduate School of Science, Tohoku University, Sendai, Japan
Description
1. RFevlist.lst:
Teleseismic events uesd in this study.
2. staHNV-132.lst:
Broadband seismic stations used in this study.
3. good_410_660_1D_IASP91.lst:
The depths of the D410 and D660, and MTZ thickness derived by 1D IASP91 model in bins. This table shows the results of D410 and D660 depths in bins have more than 80 RFs and positive amplitudes with lower boundaries at the 95% confidence intervals above zero from bootstrapping method.
4. good_410_660_3D_FWEA18.lst:
The depths of the D410 and D660, and MTZ thickness derived by 3D FWEA18 model in bins. This table shows the results of D410 and D660 depths in bins have more than 80 RFs and positive amplitudes with lower boundaries at the 95% confidence intervals above zero from bootstrapping method.
5. good_410_660_3D_EARA2024.lst:
The depths of the D410 and D660, and MTZ thickness derived by 3D EARA2024 model in bins. This table shows the results of D410 and D660 depths in bins have more than 80 RFs and positive amplitudes with lower boundaries at the 95% confidence intervals above zero from bootstrapping method.
Files
Files
(16.1 kB)
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md5:ee9647019901b515280a2982369a60a1
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