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- W4385497797 abstract "Surface deformation measurements play a key role in illuminating magma transport systems at active volcanic systems, however, unambiguous separation of deep and shallow transport remains elusive. The Socorro Magma Body (SMB) lacks an upper crustal magma transport system, allowing us to link geodetic measurements with predictions of numerical models investigating material/rheologic heterogeneities and magma-mush interaction in the mid-/lower crust. New InSAR observations confirm that a pattern of central surface uplift surrounded by a region of subsidence (previously coined sombrero deformation) has persisted over >100 yrs at the SMB. Our models suggest this pattern may reflect the presence of a large (>100 km width), weaker-than-ambient, compliant region surrounding the mid-crustal magma body. Interactions between the pressurizing sill-like magma body and the compliant region drive circulatory motions that manifest the sombrero pattern, depending on both viscoelastic relaxation and pressurization timescales, explaining its rare observation and transient nature." @default.
- W4385497797 created "2023-08-03" @default.
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- W4385497797 date "2023-08-04" @default.
- W4385497797 modified "2023-09-27" @default.
- W4385497797 title "Pressurizing magma within heterogeneous crust: a case study at the Socorro Magma Body, New Mexico, USA" @default.
- W4385497797 doi "https://doi.org/10.31223/x5z084" @default.
- W4385497797 hasPublicationYear "2023" @default.
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