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Previous studies of basalts from Idaho have suggested the induced TL of basalts increases with age.
Meteorite data suggest two possible explanations for this observation which are that (1) the initial glassy or amorphous phases crystalize with time to produce feldspar, the mineral producing the TL signal, and (2) feldspars lose Fe as they equilibrate and since Fe is a quencher of TL this would cause an increase in TL.
The compositionally-corrected induced thermoluminescence values for a suite of basalts from Big Island of Hawaii show a weak correlation with age although the TL-age slope for the Hawaii samples is shallower than similar data for basalts from Idaho.
We have measured the induced thermoluminescence (TL) properties of fifteen samples of basalts collected from the Big Island of Hawaii in order to continue our investigation into the possible utility of this technique as a chronometer.
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