A deeply eroded shoshonitic lava flow of the Radicofani eruptive center has been dated by Whole rock 40Ar-39Ar stepwise heating. The plateau age of 1299 +/- 3 ka agrees with the isochron age of 1305 +/- 5 ka. Small amounts of excess Ar are present; therefore previously reported K/Ar ages are very likely to be affected as well. The duration of the volcanic activity thus cannot be precisely calculated, but it is thought to have been short-lived.

40Ar/39Ar dating of a shoshonitic lava flow of the Radicofani volcanic center (Souther Tuscany)

MA Laurenzi;
1991

Abstract

A deeply eroded shoshonitic lava flow of the Radicofani eruptive center has been dated by Whole rock 40Ar-39Ar stepwise heating. The plateau age of 1299 +/- 3 ka agrees with the isochron age of 1305 +/- 5 ka. Small amounts of excess Ar are present; therefore previously reported K/Ar ages are very likely to be affected as well. The duration of the volcanic activity thus cannot be precisely calculated, but it is thought to have been short-lived.
1991
40Ar-39Ar dating
Radicofani
Tuscany
shoshonitic lava
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/208835
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