Quaternary erosion-induced isostatic rebound in the western Alps: COMMENT: COMMENT
作者： R. Westaway , D. Bridgland
DOI: 10.1130/G24664C.1
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摘要: [Champagnac et al. (2007)][1] deduced that rock uplift in the western Alps is occurring mainly as isostatic response to erosion and thus being largely driven by climate rather than other potential causes such plate motions. They reported spatial average rates within
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