Pb-210-Ra-226 disequilibria in volcanic rocks
Isotopes of the U-decay series, such as 238U-230Th-226Ra, have been used successfully to study timescales of magmatic processes. This study provides an overview of a shorter lived isotope pair, 210Pb-226Ra, which allows study of processes occuring during a crucial time window for magma ascent and er...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2010
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