Distributed Point Source Volcanism: A Mechanism for `Regional Plains' Resurfacing, Venus

Details Distributed Point Source Volcanism: A Mechanism for `Regional Plains' Resurfacing, Venus Distributed Point Source Volcanism: A Mechanism for `Regional Plains' Resurfacing, Venus

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1061h&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1061

Physics

2

Scientific paper

V23/24 hosts shields that form a thin porous layer across >10x106
km2; variations in thermal gradient/conductivity, radioactive
content/distribution, and surface T can result in time transgressive,
incipient shallow point-source partial melting.

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