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Items: 2

1.

Shallow deformation of the San Andreas fault 5 years following the 2004 Parkfield earthquake (Mw6) combining ERS2 and Envisat InSAR.

Bacques G, de Michele M, Raucoules D, Aochi H, Rolandone F.

Sci Rep. 2018 Apr 16;8(1):6032. doi: 10.1038/s41598-018-24447-3.

2.

Areas prone to slow slip events impede earthquake rupture propagation and promote afterslip.

Rolandone F, Nocquet JM, Mothes PA, Jarrin P, Vallée M, Cubas N, Hernandez S, Plain M, Vaca S, Font Y.

Sci Adv. 2018 Jan 31;4(1):eaao6596. doi: 10.1126/sciadv.aao6596. eCollection 2018 Jan.

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