Evidence of Normal Faulting and Dike Intrusion at Valles Marineris from Pit Crater Topography

Details Evidence of Normal Faulting and Dike Intrusion at Valles Marineris from Pit Crater Topography Evidence of Normal Faulting and Dike Intrusion at Valles Marineris from Pit Crater Topography

Mar 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005lpi....36.1008o&link_type=abstract

36th Annual Lunar and Planetary Science Conference, March 14-18, 2005, in League City, Texas, abstract no.1008

Physics

1

Scientific paper

Pit crater chain topography is found to be consistent with causative
normal faulting and dike intrusion to the north of the
Ius-Melas-Coprates chasmata, while causative normal faulting is the sole
process identified to the south of this chasmata.

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