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- W2019923936 abstract "Abstract It is known that fossil positron tracks in muscovite mica can be decorated by iron which is precipitated from solid solution as magnetite. It has now been established that they can also be decorated by calcium which is precipitated as epidote as the result of a solid-state phase change. The epidote is deposited in an epitaxial relationship with the muscovite. These minority phase changes are exothermic but are normally inhibited by a potential energy barrier. This barrier is lowered locally by the passage of a positron which stimulates the release of energy from the lattice to form a core of epidote which then grows laterally to form the observable track." @default.
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- W2019923936 date "1993-01-01" @default.
- W2019923936 modified "2023-09-26" @default.
- W2019923936 title "Track formation by release of lattice energy" @default.
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- W2019923936 doi "https://doi.org/10.1016/0969-8078(93)90017-x" @default.
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