Crustal properties of the northern Scandinavian mountains and Fennoscandian shield from analysis of teleseismic receiver functions
2018
Supplementary data are available at GJ I online. https://academic.oup.com/gji/article-lookup/doi/10.1093/gji/ggy140#supplementary-data
Figure S1. (a) Teleseismic events (Mw > 5.8) recorded by SCANLIPS2 between July 2007 and September 2009 for P-receiver function study. (b) Teleseismic events (Mw > 5.8) recorded by SCANLIPS3D between July 2013 and September 2014 for P-receiver
function study. In both cases the blue star corresponds to the centre
of the seismic array.
Figure S2. (a) Synthetic P-receiver functions for a Moho depth
of 43 km and Vp/Vs of 1.73 from three crustal models. In red, a
model with two layers (upper and lower crust) for the crust and step
discontinues. In green, a model with three layers (upper, lower crust
and transitional Moho with highVp) and step discontinuities. In blue,
a gradual model between upper crust and Moho. (b) Sensibility
of amplitude of direct P arrival and Ps conversion for different
slowness and for two crustal model (on the left a step Moho model
and on the right a gradual Moho model).
Table S1. Informations about seismic stations and number of events
used in this study for each instruments (70XX: SCANLIPS2 -13XX:
SCANLIPS3D).
Table S2. Compilation of P-RFs analysis and previous works (Ottemoller & Midzi ¨ 2003; Olsson et al. 2008; Silvennoinen et al.
2014).
Keywords:
- Correction
- Source
- Cite
- Save
- Machine Reading By IdeaReader
86
References
5
Citations
NaN
KQI