Magma compressibility and the missing source for some dike intrusions

@article{Rivalta2008MagmaCA,
  title={Magma compressibility and the missing source for some dike intrusions},
  author={Eleonora Rivalta and Paul Segall},
  journal={Geophysical Research Letters},
  year={2008},
  volume={35}
}
Dike intrusions are often accompanied by localized deflation, interpreted as depressurizing magma chambers feeding the dike. In some cases the inferred volume decrease is a factor of 4 or 5 less than the volume increase of the dike. Here we explore whether this discrepancy can be explained by compressibility of the magma combined with the fact that cracks are much more compliant than equidimensional magma chambers. If pressure changes are small, the magma compressibility βm is constant, and the… 

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