Pitsanupong Kanjanapayont

TL;DR: The tsunami left behind a sand sheet as much as 25 cm thick that contains parallel, inclined, landward and seaward lamina in addition to the normal grading commonly reported from tsunami deposits as discussed by the authors.

TL;DR: The 2004 Indian Ocean tsunami deposited a sheet of sand with surficial bedforms at the Andaman coast of Thailand as discussed by the authors, and the recognition of bedforms and the key internal sedimentary structures as criteria of the tsunami supercritical flow condition.

TL;DR: In this paper, the authors used erosional and depositional features to infer the main processes that acted during inundation from the tsunami, including ripples from inflow and outflow, graded bedding, parallel lamination, and double-layered deposits.

TL;DR: In situ U-Pb ages of inherited zircon cores from all zircons in the Khlong Marui shear zone indicate that they have the same material from the Archean as mentioned in this paper.