Abstract

A detailed K-Ar and paleomagnetic study was made on the oldest outcropping lavas of the Roccamonfina volcano. The very first episodes of volcanism were concentrated at around 1 M.Y., whereas most of the activity occurred between 0.4 and 0.5 M.Y. After the formation of a caldera a second cycle of volcanism started at 0.25 M.Y. The paleomagnetic measurements indicate an episode of normal polarity at 1.10 + 0.05 M.Yr. The occurrence of this episode was suggested by Watkins (14) in 1968. There is no evidence of other magnetic events on younger rocks.

Highlights

  • The very first episodes of volcanism were concentrated at around 1 M.Y., whereas most of t h e activity occurred between 0.4 and 0.5 M.Y

  • paleomagnetic study was made on t h e

  • After t h e formation of a caldera a second cycle of volcanism started a t 0.25 M.Y. The paleomagnetic measurements indicate an episode of normal polarity at 1.10 + 0.05 M.Yr

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Summary

Tipo petrográfico

RMP 30 RMP 31 km 20.7, SS 430 km 15.9, SS 430 (sotto la cava) km 18.5, SS 430 km 18.2, SS 430 cava tra i km 10-18, SS 430.

Tefrite leucitica Fonolite leucitica
CONCLUSIONI
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