Figure 3
From: Giant rhyolite lava dome formation after 7.3 ka supereruption at Kikai caldera, SW Japan
MCS profiles along the lines 1 and 2 (Fig. 1). Topographical and/or structural caldera rims (open and solid arrows for inner and outer rims, respectively), post-caldera sediment cover layers, and possible 7.3-ka syn-caldera ignimbrite layers (blue stars) are highlighted. Central lava dome intruded and upwarped the caldera floor at its margin. Several intrusions are distributed along caldera rims.
