Supplemental material: Hidden intrabasin extension: Evidence for dike-fault interaction from magnetic, gravity, and seismic reflection data in Surprise Valley, northeastern California

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.