Topographic Constraints on Magma Reservoir Volume and Depth for Small Near-Polar Volcanoes in the Northern Plains of Mars

Physics

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Scientific paper

Shallow, edifice-centered depressions may form when subsurface magma
melts ground ice. Here, assuming variable porosities, we use MOLA data
and thermal calculations to explore the minimum sill volume, thickness
and depth required to produce the observed depressions.

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