The Stress State of the Lunar Lithosphere and the Volumes of Intruded and Erupted Magmas

Details The Stress State of the Lunar Lithosphere and the Volumes of Intruded and Erupted Magmas The Stress State of the Lunar Lithosphere and the Volumes of Intruded and Erupted Magmas

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1549s&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1549

Physics

Scientific paper

Using a new model of dike rise from the upper mantle we find the ranges
of magma densities, magma source depths and lithosphere tensile stresses
that could deliver large volumes of magma to either erupt at, or to
intrude close to, the lunar surface.

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