Magmatic Intrusions Beneath Martian Highland Volcanoes: Clues from Eruptive History, Thermal-Magnetic-Gravity Modeling and Electron Reflectometry

Details Magmatic Intrusions Beneath Martian Highland Volcanoes: Clues from Eruptive History, Thermal-Magnetic-Gravity Modeling and Electron Reflectometry Magmatic Intrusions Beneath Martian Highland Volcanoes: Clues from Eruptive History, Thermal-Magnetic-Gravity Modeling and Electron Reflectometry

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2180l&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2180

Computer Science

Scientific paper

Gravity and magnetic field measurements imply that the magma chamber
beneath Tyrrhena Patera partially demagnetized surrounding crust, while
the larger magma accumulation at Syrtis Major completely demagnetized
10,000s of square kilometers of crust.

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