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Plains Tectonics on Venus

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dc.contributor.author Banerdt, W. B. en_US
dc.contributor.author McGill, G. E. en_US
dc.contributor.author Zuber, M. T. en_US
dc.date.accessioned 2004-09-30T23:07:50Z
dc.date.available 2004-09-30T23:07:50Z
dc.date.issued 1996 en_US
dc.identifier.clearanceno 96-1235 en_US
dc.identifier.uri http://hdl.handle.net/2014/26372
dc.description.abstract Tectonic deformation in the plains of Venus is pervasive, with virtually every area of the planet showing evidence for faulting or fracturing. This deformation can be classified into three general categories, defined by the intensity and areal extent of the surface deformation: distributed deformation, concentrated deformation, and local fracture patterns. en_US
dc.format.extent 3144582 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other tectonics tectonic formation tectonic deformation venus venus tectonics venus geology en_US
dc.title Plains Tectonics on Venus en_US


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