partial thermoremanent magnetization

partial thermoremanent magnetization

[′pär·shəl ¦thər·mō′rem·ə·nənt ‚mag·nə·tə′zā·shən]
(geophysics)
The thermoremanent magnetization acquired by cooling in an ambient field over only a restricted temperature interval, as opposed to the entire temperature range from Curie point to room temperature. Abbreviated PTRM.
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