Disequilibrium of the 238U series in basalt
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Abstract
Radioisotope analyses of basalt samples from Hawaii, Japan, and Iwo Jima show that: (1)234U and238U are virtually in radioactive equilibrium, (2)230Th exceeds equilibrium values in all these samples, (3)210Pb concentrations range from 10–200% of the equilibrium values and average 30% deficient, and (4)226Ra is probably not in equilibrium with234U.
The source regions of the basalts or magma forming processes are open systems, chemically. The enrichment of some of the uranium-daughter nuclides is insufficient to account for the excess206Pb in volcanic rocks.
The isotopic composition of lead and specific activity of210Pb in sublimates from Showa-shinzan, Japan are also reported.
Study Area
Publication type | Article |
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Publication Subtype | Journal Article |
Title | Disequilibrium of the 238U series in basalt |
Series title | Earth and Planetary Science Letters |
DOI | 10.1016/0012-821X(66)90032-X |
Volume | 1 |
Issue | 6 |
Year Published | 1966 |
Language | English |
Publisher | Elsevier |
Description | 5 p. |
First page | 387 |
Last page | 391 |
Country | United States, Japan |
State | Hawaii |
Other Geospatial | Iwo Jima |
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