The behavior of thallium during alteration of the K-alkaline rocks from the Roccamonfina Volcano (Campania, southern Italy)

التفاصيل البيبلوغرافية
العنوان: The behavior of thallium during alteration of the K-alkaline rocks from the Roccamonfina Volcano (Campania, southern Italy)
المؤلفون: Calderoni, G., Ferri, T., Giannetti, B., Masi, U.
المصدر: Chemical Geology; March 1985, Vol. 48 Issue: 1-4 p103-113, 11p
مستخلص: Tl behavior in the alteration of leucite and related K-alkaline rocks from the Quaternary Roccamonfina Volcano has been outlined. The dominant weathering product is analcite, that shows a moderate loss of Tl relative to the coexisting leucite (R̄= 0.74 ± 0.21). Weathering of leucite to halloysite is subordinate and characterized by a very strong depletion in Tl (R̄= 0.14 ± 0.15).
قاعدة البيانات: Supplemental Index
الوصف
تدمد:00092541
DOI:10.1016/0009-2541(85)90038-5