Dataset and 3D Vs Model for "Crustal velocity images of north-western Türkiye along the North Anatolian Fault Zone from transdimensional Bayesian ambient seismic noise tomography"
Creators
- 1. Research School of Earth Sciences, Australian National University, Canberra, Australia & Department of Geophysical Engineering, The Faculty of Mines, Istanbul Technical University, Istanbul, Türkiye
- 2. Department of Geophysical Engineering, The Faculty of Mines, Istanbul Technical University, Istanbul, Türkiye
- 3. School of Earth Sciences, Zhejiang University, Hangzhou, 310027, China
- 4. School of Earth and Environment, The University of Leeds, Leeds, LS29JT, United Kingdom
- 5. Deep Earth Imaging Future Science Platform, CSIRO, Perth, Australia & Department of Physics, School of Physics, Mathematics and Computing, University of Western Australia, Perth, Australia
Contributors
Supervisors:
- 1. Department of Geophysical Engineering, The Faculty of Mines, Istanbul Technical University, Istanbul, Türkiye
- 2. Deep Earth Imaging Future Science Platform, CSIRO, Perth, Australia & Department of Physics, School of Physics, Mathematics and Computing, University of Western Australia, Perth, Australia
Description
Final 3D Vs model and dispersion data for the paper entitled "Crustal velocity images of north-western Türkiye along the North Anatolian Fault Zone from transdimensional Bayesian ambient seismic noise tomography".
In the vel_files folder, there are 10 files for each depth for 1-15 km. The format of each velocity file is as follows:
Column Value
1 Lattitude (°)
2 Longitude (°)
3 Vs (km/s)
The format of the dispersion data is as follows (See Computer Programs in Seismology Tutorials - do_mft for more information on the format):
Column Value
1 Type of file, MFT96
2 Wave type: R for Rayleigh
3 Dispersion type: U for group velocity
4 Mode: 0 represents the fundamental mode
5 Filter period, T, in seconds
6 Dispersion value, either group or phase
7 Error in dispersion. This is just a place holder since there is no way to estimate an error from a single trace. The group velocity error is determined from the ratio of the filter period to travel time
8 Distance in km
9 Azimuth from the source to the receiver
10 Spectral amplitude.
11 Epicenter latitude
12 Epicenter longitude
13 Station latitude
14 Station longitude
15 control flag
16 control flag
17 Instantaneous period if this is preferred. This differs from the ilter period because the signal spectram is not flat.
18 Comment: keyword
19 Station
20 Component
21 Year
22 Day of year
23 Hour
24 Minute - these identify the event origin time
Files
Files
(4.3 MB)
Name | Size | Download all |
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md5:7440a58fdb8e84920ed0a5828195c064
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4.1 MB | Download |
md5:892bb14c09a195781a43ad4b526833bc
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182.5 kB | Download |