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Co- and postseismic subaquatic evidence for prehistoric fault activity near Coyhaique, Aysén Region, Chile - Vervoort, Morgan et al - published in NHESS, 24 issue 10, pp. 3401–3421 (2024) - SCART-2024-0032
 
additional file(s):
      nhess-24-3401-2024-f02-web
    version 1
    nhess-24-3401-2024-f02-web.gif (icon) [25.25 KB] 08 Nov 2024, 11:06 (a) Bathymetry of Lago Pollux with an indication of subbasins and location of the two pinger seismic profiles (white lines). (b, c) Pinger seismic profiles of Lago Pollux with interpretations: acoustic basement (in grey), all seismic (sub)units (numbers) and mass transport deposits (MTDs) are indicated
    nhess-24-3401-2024-f02-web.jpg (icon-180) [16.76 KB] 08 Nov 2024, 11:06 (a) Bathymetry of Lago Pollux with an indication of subbasins and location of the two pinger seismic profiles (white lines). (b, c) Pinger seismic profiles of Lago Pollux with interpretations: acoustic basement (in grey), all seismic (sub)units (numbers) and mass transport deposits (MTDs) are indicated
    nhess-24-3401-2024-f02-web.png [1.32 MB] 08 Nov 2024, 11:06 (a) Bathymetry of Lago Pollux with an indication of subbasins and location of the two pinger seismic profiles (white lines). (b, c) Pinger seismic profiles of Lago Pollux with interpretations: acoustic basement (in grey), all seismic (sub)units (numbers) and mass transport deposits (MTDs) are indicated
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