Figure 11From: Geological and tectonic implications obtained from first seismic activity investigation around Lembang fault A modified geological map from Sunardi& Kimura [ 17 ] and Horspool et al . (2011). The Lembang fault line was identified by Horspool et al. (2011) based on morphological features on SRTM digital elevation model of ca. 90 m grid, showing a length of more than 30 km excluding the segment identified in this study. The schematic north–south longitudinal stratigraphic profile of the Bandung basin and its adjacent area inferred from geological map, showing Quaternary and pre-Quaternary rock units and their boundary at about 1 km depth.Back to article page