Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4693043 | Tectonophysics | 2011 | 12 Pages |
Abstract
âºThe deep structure and tectonic evolution of the Lützow-Holm Complex (LHC), East Antarctica were derived from Deep Seismic Surveys (DSS) by SEAL transects. âºThe 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
M. Kanao, A. Fujiwara, H. Miyamachi, S. Toda, K. Ito, M. Tomura, T. Ikawa, The SEAL Geotransect Group The SEAL Geotransect Group,