Late Ross-orogenic deformation of basement rocks in the northern Deep Freeze Range, Victoria Land, Antarctica; the Lichen Hills shear zone
Kinematic data from the basement rocks exposed at Lichen Hills in the upper Rennick Glacier, northern Victoria Land, indicate the presence of an intra-Wilson Terrane late Ross-orogenic high-strain reverse shear zone. ENE directed ductile shearing and WSW-directed late-stage brittle reverse faults ov...
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Format: | Article in Journal/Newspaper |
Language: | English |
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Deutsche Gesellschaft fuer Polarforschung e.V.
2011
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Online Access: | http://hdl.handle.net/1959.13/1061540 |