Data Services Products: EMC-EARA2024 A new radially anisotropic seismic velocity model for the crust and upper mantle beneath east asia and northwestern pacific subduction zones.

Summary

EARA2024 is a new radially anisotropic seismic velocity model for the crust and upper mantle beneath east asia and northwestern pacific subduction zones.

Description

Name EARA2024
Title Full-waveform tomography model of East Asia (EARA2024)
Type 3-D Tomography Earth Model
Sub Type Radial anisotropic (in the crust and upper mantle) P and S velocities
Year 2024
Data Revision r0.0 (revision history)
 
Short Description   EARA2024 is a new radially anisotropic seismic velocity model for the crust and upper mantle beneath east asia and northwestern pacific subduction zones.
 
Authors: Ziyi Xi (xiziyi@msu.edu), Department of Computational Mathematics, Science and Engineering, Michigan State University, East Lansing, MI, USA

Min Chen, Department of Computational Mathematics, Science and Engineering, Michigan State University, East Lansing, MI, USA; Department of Earth and Environmental Sciences, Michigan State University, East Lansing, MI, USA

Songqiao Shawn Wei (swei@msu.edu), Department of Earth and Environmental Sciences, Michigan State University, East Lansing, MI, USA; Department of Computational Mathematics, Science and Engineering, Michigan State University, East Lansing, MI, USA

Jiaqi Li, Department of Computational Mathematics, Science and Engineering, Michigan State University, East Lansing, MI, USA; Department of Earth and Environmental Sciences, Michigan State University, East Lansing, MI, USA

Tong Zhou, Department of Computational Mathematics, Science and Engineering, Michigan State University, East Lansing, MI, USA

Baoshan Wang, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China; Mengcheng National Geophysical Observatory, University of Science and Technology of China, Hefei, China

YoungHee Kim, School of Earth and Environmental Sciences, Seoul National University, Seoul, Republic of Korea

 
Reference Model In the crust, we utilize CRUST1.0, and in the mantle, we use STW105 during the inversion process. This approach allows us to focus on updating model perturbations rather than absolute model parameter values. For plotting and final illustration purposes, we employ the EARA2024_AVG, an averaged 1D model derived from EARA2024, which is provided by the _ref parameters in the model file.
 
Prior Model EARA2014 doi: 10.1002/2014JB011638
 
Model Download EARA2024.r0.0.nc (see metadata) is the model in netCDF 3 Classic format.
EARA2024.r0.0-n4.nc (see metadata) is the model in netCDF 4 Classic format.
 
Model Home Page None
 
Depth Coverage 0 to 1000 km
 
Area East Asia (10° N to 60° N and 80° E to 160° E)
 
Data Set Description We present a new 3-D radially anisotropic seismic velocity model EARA2024 of the crust and mantle beneath East Asia and the northwestern Pacific using adjoint full-waveform inversion tomography. We construct the EARA2024 model by iteratively minimizing the waveform similarity misfit between the synthetic and observed waveforms from 142 earthquakes recorded by about 2,000 broadband stations in East Asia. Compared to previous studies, this new model renders significantly improved images of the subducted oceanic plate in the upper mantle, mantle transition zone, and uppermost lower mantle along the Kuril, Japan, Izu-Bonin, and Ryukyu Trenches. Complex slab deformation and break-offs are observed at different depths. Moreover, our model provides new insights into the origins of intraplate volcanoes in East Asia, including the Changbaishan, Datong-Fengzhen, Tengchong, and Hainan volcanic fields.
 
 

EARA2024
Map views of Vs perturbation at various depths. The reference model is the 1-D average of the 3-D model. Regions with low resolution, based on the point spread function resolution test, are masked out. Magenta curves represent the slab depth contour at each depth, based on the Slab2 model (Hayes et al. 2018). The tectonic units and plate boundaries from the NUVEL-1 model (DeMets et al. 1990) are outlined by green curves, and intraplate volcanoes are marked with red triangles.

Citations and DOIs

To cite the original work behind this Earth model:

  • Ziyi Xi, Min Chen, Songqiao Shawn Wei, Jiaqi Li, Tong Zhou, Baoshan Wang, YoungHee Kim, EARA2024: A New Radially Anisotropic Seismic Velocity Model for the Crust and Upper Mantle beneath East Asia and Northwestern Pacific Subduction Zones, Geophysical Journal International, 2024;, ggae302, https://doi.org/10.1093/gji/ggae302

To cite IRIS DMC Data Products effort:

  • Trabant, C., A. R. Hutko, M. Bahavar, R. Karstens, T. Ahern, and R. Aster (2012), Data Products at the IRIS DMC: Stepping Stones for Research and Other Applications, Seismological Research Letters, 83(5), 846–854, https://doi.org/10.1785/0220120032.

DOI for this EMC webpage: https://doi.org/10.17611/dp/emc.2024.eara2024.1

References

  • Hayes, G. P., Moore, G. L., Portner, D. E., Hearne, M., Flamme, H., Furtney, M., & Smoczyk, G. M., 2018. Slab2, a comprehensive subduction zone geometry model, Science, 362(6410), 58–61. https://doi.org/10.1126/science.aat4723
  • DeMets, C., Gordon, R. G., Argus, D. F., & Stein, S., 1990. Current plate motions, Geophysical Journal International, 101(2), 425–478. https://academic.oup.com/gji/article/101/2/425/561883

Credits

  • r0.0 model provided by Ziyi Xi.

Revision History

revision r0.0: uploaded August 29, 2024.

Timeline

2024-08-29
r0.0 online

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