Widespread effusive volcanism on Mercury likely ended by about 3.5 Ga
about
Impact-induced changes in source depth and volume of magmatism on Mercury and their observational signatures.The surface roughness of Mercury from the Mercury Laser Altimeter: Investigating the effects of volcanism, tectonism, and impact crateringRevised constraints on absolute age limits for Mercury's Kuiperian and Mansurian stratigraphic systemsSize-frequency distribution of different secondary crater populations: 1. Equilibrium caused by secondary impactsMercury's Caloris basin: Continuity between the interior and exterior plains
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Widespread effusive volcanism on Mercury likely ended by about 3.5 Ga
description
im Juli 2016 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована в липні 2016
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Widespread effusive volcanism on Mercury likely ended by about 3.5 Ga
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Widespread effusive volcanism on Mercury likely ended by about 3.5 Ga
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Widespread effusive volcanism on Mercury likely ended by about 3.5 Ga
@en
Widespread effusive volcanism on Mercury likely ended by about 3.5 Ga
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Widespread effusive volcanism on Mercury likely ended by about 3.5 Ga
@en
Widespread effusive volcanism on Mercury likely ended by about 3.5 Ga
@nl
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Widespread effusive volcanism on Mercury likely ended by about 3.5 Ga
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Christian Klimczak
Clark R. Chapman
Maria E. Banks
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10.1002/2016GL069412
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2016-07-21T00:00:00Z