No. 28 · Frontiers in Earth Science · 11 May 2023

The crust-mantle transition beneath Northeast China from P-wave receiver functions

Nita Sebastian, Hrvoje Tkalčić, Christian Sippl, Seongryong Kim, Anya M. Reading, Youlin Chen, Fabrice R. Fontaine

DOI 10.3389/feart.2023.1144819 Publisher page Cite Geodynamics and Earth structure Seismological methods

Representative figure

Four maps compare crustal thickness and uncertainty beneath Northeast China from Bayesian inversion and H-kappa stacking. — Crust is ≤32 km beneath the craton and Songliao Basin and 35–40 km beneath the orogen and Changbaishan; Vp/Vs is ~1.65 at Changbaishan and mostly >1.75 elsewhere.

Figure 6 · Sebastian et al. (2023), Frontiers in Earth Science, Figure 6. · CC BY 4.0

Citation

Nita Sebastian, Hrvoje Tkalčić, Christian Sippl, Seongryong Kim, Anya M. Reading, Youlin Chen, and Fabrice R. Fontaine (2023), The crust-mantle transition beneath Northeast China from P-wave receiver functions, Frontiers in Earth Science, 11:1144819, doi: https://doi.org/10.3389/feart.2023.1144819.