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- W2184782114 abstract "Although the metav olcanics interbedded in the Palaeozoic basement of the tectonic units constituting the Peloritani belt show various and contrasting geodynamic aff inities,. these rocks are the only record allowing us to establish the chronology of the extensive and compressive events which developed prior to the Hercynian orogenesis. For this reason, their study becomes very important in reconst ructing a pre-Herc ynian geodynamic model for the Peloritani area. This paper examines two of the most important metavolcanic successions, outcropping in the southern sector of the Peloritani belt. Geochemical analyses, carried out on these two metavolcanic successions, reveal differ ent magmatic affi nities: the first succession, Early Ordovician in age, has an alkaline basaltic composition and within plate affi nity; the second, Late Ordovician in age, consists of metavolcanics with orogenic affi nity. Taking into account these diff erent geochemical features, the present paper proposes a preliminary geodynamic model for the Palaeozoic basement of the Peloritani plate, spanning an interval from Late Cambrian- Early Ordovician to Late Ordovician." @default.
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- W2184782114 date "2001-01-01" @default.
- W2184782114 modified "2023-09-27" @default.
- W2184782114 title "A tentative pre- Variscan geodynamic model for the Palaeozoic basement of the Peloritani mountains (Sicily): evidence from meta-igneous products" @default.
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