Article ID Journal Published Year Pages File Type
4693043 Tectonophysics 2011 12 Pages PDF
Abstract
►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.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Authors
, , , , , , , ,