Volumetric analysis of complex lunar craters: Implications for basin rim formation

Mathematics – Logic

Scientific paper

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Scientific paper

The transition in hypervelocity impact structures from complex craters to basins is defined by a transition in uplifted central features from peaks to peak rings. Volumetric and morphologic analyses of the central peaks in complex lunar craters are combined with subsurface data from terrestrial complex impact structures in an effort to characterize the crater to basin transition.

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