Supplemental material: Hidden intrabasin extension: Evidence for dike-fault interaction from magnetic, gravity, and seismic reflection data in Surprise Valley, northeastern California
journal contributionposted on 25.11.2015, 00:00 by Noah D. Athens, Jonathan M.G. Glen, Simon L. Klemperer, Anne E. Egger, Valentina C. Fontiveros
Geosphere, February 2016, v. 12, p. 15-25, doi:10.1130/GES01173.1, Supplemental Figure 1 - Unmigrated common midpoint stack. The high-amplitude reflection (B in Fig. 3A) is clearly homoclinal rather than synformal. Depth conversion is based on the velocity model of Figure 3A.