Single‐chamber silicic magma system inferred from shear wave discontinuities of the crust and uppermost mantle, Coso geothermal area, California

@article{Wilson2002SinglechamberSM,
  title={Single‐chamber silicic magma system inferred from shear wave discontinuities of the crust and uppermost mantle, Coso geothermal area, California},
  author={Charles Kent Wilson and Craig H. Jones and Hersh Gilbert},
  journal={Journal of Geophysical Research},
  year={2002},
  volume={108},
  pages={2226}
}
[1] Analysis of seismograms from teleseismic rays traversing the Coso geothermal area near Ridgecrest, California, suggests the geothermal system lies over a single shallow magma reservoir (∼5 km below the surface) that also plays a crucial role in the local change in deformation style from areas to the north and west. The character of the magma reservoir and the absence of a lower crustal magma reservoir is inferred from three crustal P-to-S conversions observed using receiver function… 

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