Reflection imaging of the crust and the lithospheric mantle in the Lützow-Holm complex, Eastern Dronning Maud Land, Antarctica, derived from the SEAL transects

►The deep structure and tectonic evolution of the Lützow-Holm Complex (LHC), East Antarctica were derived from Deep Seismic Surveys (DSS) by SEAL transects. ►The imaged repetitive crust-mantle transition zone suggests the compression stress during the Pan-African orogeny, in contrast, successive break-up processes of Gondowana in mid-Mesozoic may account for the formation of the stretched reflection structure above the Moho beneath the LHC.