Figure 9
(a) SW-NE seismic profile showing crater C5 and underlying magmatic sills at a depth between 3300 ms and 5500 ms TWTT. Most of the shallow sills in the Solsikke area are interconnected saucer-shaped sills. N.B: An uninterpreted seismic profile is provided in the appendix. (b) 3D view showing the spatial relationship between C5 and underlying magmatic sills. In the study area, the interpreted magmatic sills are classified into shallow sills at depths < 4000 ms TWTT, intermediate sills occurring at a depth of 4000–5000 ms TWTT, and deeper sills occurring at depth > 5000 ms TWTT.
