Several clay samples from the "Tusa Tuffites" have been studied. Microfauna association show that the studied sequence is Upper Aquitanian to Burdigalian in age. The epiclastic volcanic debris in the arenaceous tur- bidites is related to the existence of a continental ande- sitic volcanism probably almost simultaneous to the deposition of the tuffites. The paleogeographic position of the sedimentary basin of the "Tusa Tuffites" is discussed.
Alcune osservazioni sulle "tufiti di Tusa" nell'area compresa tra la Valsinni e Rocca Imperiale (confine calabro-lucano)
TURCO, Eugenio
1984-01-01
Abstract
Several clay samples from the "Tusa Tuffites" have been studied. Microfauna association show that the studied sequence is Upper Aquitanian to Burdigalian in age. The epiclastic volcanic debris in the arenaceous tur- bidites is related to the existence of a continental ande- sitic volcanism probably almost simultaneous to the deposition of the tuffites. The paleogeographic position of the sedimentary basin of the "Tusa Tuffites" is discussed.File in questo prodotto:
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