Unique geological structures of the Law Dome and Vanderford and Totten glaciers region (Wilkes Land) distinguished by geophysical data

Wilkes Land is a key region for Gondwana reconstruction, however it remains one of the largest regions on Earth with poorest knowledge of geology. This study comprehensively reviews the ICECAP/ IceBridge geophysical data for the Law Dome region including Vanderford and Totten adjacent glaciers over Wilkes Land and their role in obtaining new insight on the East Antarctic geology hidden under the ice cover. We analyzed more than 100,000 line kilometers of new magnetic, gravity and subglacial bedrock topography data that are available through the National Snow and Ice Data Center (USA). The newly acquired data supports our previous idea of the continuous rift structure existence at the southern boundary of Law Dome that runs between Vanderford and Totten Glaciers. The rift length exceeds 400 km and width varies from 50 to 100 km. In accordance with results of depth to Moho estimations and density modelling, for axial part of the rift it is characteristic an essential thinning of the Earth crust thickness, it is raised up to 24–26 km and continue to be elevated along entire length of this structure. The thickness of sedimentary rocks within the rift exceeds 3 km, their high density probably evidence that they were formed during Late Paleozoic – Early Mesozoic. The results of our investigations support tectonic nature of this structure as continuous rift developed since the Mesozoic extension phase (~160 Ma) of the Wilkes Land continental margin. Second distinctive structure is the strong reversely magnetized Law Dome magnetic anomaly with an area of about 9,500 km 2 . This anomaly would map out one of the largest mafic/ultramafic intrusions of the Earth, similar in extent to Norway’s Bjerkreim-Sokndal layered intrusion, the Coompana Block gabbro in Australia, or even the granitic-gneiss complex in the Adirondack Mountains of North America.