210Pb-226Ra and 228Ra-232Th systematics in young arc lavas: Implications for magma degassing and ascent rates
New data show that island arc rocks have (210Pb/226Ra)o ratios which range from as low as 0.24 up to 2.88. In contrast, (228Ra/232Th) appears always within error of 1 suggesting that the large 226Ra-excesses observed in arc rocks were generated more than 30 years ago. This places a maximum estimate...
المؤلفون الرئيسيون: | Turner, S, Black, S, Berlo, K |
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التنسيق: | Journal article |
اللغة: | English |
منشور في: |
2004
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مواد مشابهة
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Pb-210-Ra-226 and Ra-228-Th-232 systematics in young arc lavas: implications for magma degassing and ascent rates
حسب: Turner, S, وآخرون
منشور في: (2004) -
Pb-210-Ra-226-Th-230 implications for the timescales of island arc magma degassing
حسب: Turner, S, وآخرون
منشور في: (2005) -
Tracing pre-eruptive magma degassing using (Pb-210/Ra-226) disequilibria in the volcanic deposits of the 1980-1986 eruption of Mount St. Helens
حسب: Berlo, K, وآخرون
منشور في: (2006) -
Pb-210-Ra-226 disequilibria in volcanic rocks
حسب: Berlo, K, وآخرون
منشور في: (2010) -
Pb-210-Ra-226 disequilibria: Mantle melting or gas fractionation?
حسب: Berlo, K, وآخرون
منشور في: (2008)