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Observations suggest that impactors and volcanism are connected, but themechanism that links these events is unknown. This research proposes the impactexsolution hypothesis to explain how planetary scale collisions triggervolcanism. This hypothesis says that when large objects such as asteroids orcomets hit planets, they generate seismic waves that cause exsolution in magma,which initiates eruptions. Observations of the Chicxulub impact and Deccanvolcanism support this hypothesis. These observations include changes in feederdike orientations, changes in isotope geochemistry, and changes in lava flowdynamics following the Chicxulub impact.

Using impact exsolution to link the Chicxulub collision and Deccan volcanism