LARGE SCALE CONTINENTAL EXTENSION IN WEST ANTARCTICA
The disadvantageous situation is being addressed through a new aerogeophysics acquisition over a vast under-explored sector of the rift, the Ross Ice Shelf. The multi-institution, multidisciplinary program in 2015 to 2017 is called ROSETTA-Ice, for Ross Ocean and ice Shelf Environment, and Tectonic setting Through Aerogeophysical surveys and modeling. The investigation of crustal geology combines new gravity data with magnetics to model bathymetry, then delineate sediments, bedrock geological units, and faults beneath the Ross Ice Shelf. The results are being used to interpret the locations and characteristics of faults and tectonic basins, and thereby achieve a greater understanding of Mesozoic large-scale extension across the West Antarctic rift system, active volcanism from Oligocene to present, and ongoing narrow extensional to wrench deformation in the province.
This contribution aims to provide an overview of the tectonic evolution of the West Antarctic extensional province, reexamine ‘legacy’ geophysical data within the context of 21st century datasets, and introduce new hypotheses about large scale continental extension in Antarctica, based on analysis of ROSETTA-Ice data.