PUMA
Istituto di Geoscienze e Georisorse     
Villa I., Taddeucci G. K-Ar datability of altered rocks: variability of excess Ar in hydrothermal minerals. In: Bulletin of Volcanology, vol. 54 (1) pp. 84 - 86. Springer, 1991.
 
 
Abstract
(English)
⁴⁰Ar/⁹ Ar stepwise heating on one hydrothermal anhydrite and two partly hydrothermalized feldspars from a borehole in Vulcano volcano show that the initial trapped Ar does not have a constant isotopic composition. The constant ⁴⁰Ar/⁶Ar ratio of the anhydrite, 3063, is not a well-defined endmember for the two feldspars, which record a variety of fluid compositions. As the system is young (<100 ka), radiogenic Ar is much less than excess Ar.
URL: http://www.springerlink.com/content/k5432h7h50345200/?p=5eb950197a254d718c68c1026ac34f3b&pi=7
DOI: 10.1007/BF00278209
Subject geochronology
altered rocks
K-Ar dating
Ar isotopes
hydrothermal minerals


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