Fig. 7: Depth profiles of seismic and elastic attributes at SI-Seis and JP-Seis.
From: Seawater softening of suture zones inhibits fracture propagation in Antarctic ice shelves
a P-wave and S-wave velocities. b Bulk and shear moduli. In both a and b, the shaded bounds represent possible ranges of seismic velocity models derived from Monte Carlo analysis, considering the median plus the interquartile range (see ‘Methods’).
