Continuum approximation of dyking with a theory for poro-viscoelastic–viscoplastic deformation
To reach Earth’s surface, magma must ascend from the hot, ductile asthenosphere through cold and brittle rock in the lithosphere. It does so via fluid-filled fractures called dykes. While the continuum mechanics of ductile asthenosphere is well established, there has been little theoretical work on...
Main Authors: | , , , , |
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格式: | Journal article |
语言: | English |
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Oxford University Press
2023
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