Comptes Rendus Géoscience

Chuansong He

M. Santosh

Handled by Michel Campillo

Intraplate earthquakes and their link with mantle dynamics: insights from P-wave teleseismic tomography along northern part of the North-South Tectonic Zone in China

Chuansong He1[footnoteRef:1], M. Santosh2, 3  [1:  Corresponding author. Tel.: 86-10-68729303; Fax: 86-10-83534760.
Email address: hechuansong@aliyun.com] 

1Institute of Geophysics, China Earthquake Administration, Beijing 100081, China
2 Centre for Tectonics, Exploration and Resources, Department of Earth Sciences, University of Adelaide, SA 5005, Australia
3School of Earth Sciences and Resources, China University of Geosciences Beijing, 29 Xueyuan Road, Beijing 100083, China









Fig. S1 Distribution of the relative travel-time residuals, data of great than 2s and less then -2s were used for tomographic inversion.

Fig. S2 The damping parameter 15 (red circle) is taken to invert final model after a series of tests.

Fig. S3 Check board resolution test at 70, 100, 200, 300, 400, 500, 600, 700 and 800 km depth sections respectively relative to the iasp91 1-D Earth model (Kennett and Engdahl, 1991). The model was run using the same raypaths as the main inversion, with the same damping parameter.

Fig. S4 CRT along the west-east profiles (see Fig. 1 for profile location). a, b, c and d are at 39 degree, 37 degree, 35 degree and 33 degree along latitudinal direction.

Fig. S5 CRT along the north-south profiles (see Fig. 1 for profile location), e and f are at 103 degree and 105 degree along meridians of longitude. 



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Volume 349 (2017) – No. 8 – December 
Cover illustration: A view of the Dead Sea seen from the Israeli shore. © David Shankbone. This fi le is licensed under 
the Creative Commons Attribution-Share Alike 3.0 Unported license. For further details, see Michael G. Ezersky 
and Amos Frumkin, C. R. Geoscience 349(1), 2017, pp. 1–11.
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