about
Widespread effusive volcanism on Mercury likely ended by about 3.5 GaOnset of solid-state mantle convection and mixing during magma ocean solidificationRevised constraints on absolute age limits for Mercury's Kuiperian and Mansurian stratigraphic systemsCarbon contents in reduced basalts at graphite saturation: Implications for the degassing of Mars, Mercury, and the MoonMercury's Caloris basin: Continuity between the interior and exterior plains
P2860
description
im September 2014 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована у вересні 2014
@uk
name
Long-lived explosive volcanism on Mercury
@en
Long-lived explosive volcanism on Mercury
@nl
type
label
Long-lived explosive volcanism on Mercury
@en
Long-lived explosive volcanism on Mercury
@nl
prefLabel
Long-lived explosive volcanism on Mercury
@en
Long-lived explosive volcanism on Mercury
@nl
P2860
P356
P1476
Long-lived explosive volcanism on Mercury
@en
P2093
David A. Rothery
Rebecca J. Thomas
P2860
P304
P356
10.1002/2014GL061224
P407
P577
2014-09-04T00:00:00Z
P819
2014GeoRL..41.6084T