“…3 and 4). Immediately north of the basin, the fault zone is accompanied by exposures of Upper Neogene tholeiitic basalts (Hoang et al, 1996a,b;Lee et al, 1998), thermal springs, and emanations of radon, methane and carbon dioxide (Hung and Vinh, 2001), and is marked by epicentres of relatively strong earthquakes. Young basalts have been drilled in the basin bottom, some 2 km west of Dien Bien city (borehole LK-3D; cf.…”