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- W2343266422 abstract "Fluid inclusions are known to be formed at pressures reaching some tens of kilobars. The solid matrix encompassing the fluid filled cavity experiences decompression as a consequence of uplift processes such as eruptions. This event may prompt the mechanical failure of the host-mineral matrix through either stretch or decrepitation, depending on a ductile or brittle mechanism of matrix failure, respectively [1-3]." @default.
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- W2343266422 date "2015-01-01" @default.
- W2343266422 modified "2023-09-23" @default.
- W2343266422 title "The Smaller the Harder: Theorization of a Threshold Size below which Fluid Inclusions do not Decrepitate" @default.
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- W2343266422 hasPublicationYear "2015" @default.
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