Fig. 7From: Late Quaternary eruption of the Ranau Caldera and new geological slip rates of the Sumatran Fault Zone in Southern Sumatra, IndonesiaExposures of the distal Ranau Tuff near Muaradua (Lat,Lon: −4.53182, 104.06358), 40 km from the eruptive center, where samples RAN-14A,B were collected. The tuff is separated from tilted sedimentary rocks by a thick, organic-rich paleosolBack to article page