By A. Ionescu Tulcea, C. Ionescu Tulcea
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A complex pattern of magnetic anomalies (fig. , 2011), while another isolated anomaly (fig. 11; F) corresponds to the Volturno river. Fig. , 2004). The letters A-F indicate the main magnetic anomalies recognized in the area. 3 Ischia and Procida volcanic complexes The Ischia island represents an alkali-trachytic volcanic complex, whose eruptive activity lasted from the Late Pleistocene up to historical times (Vezzoli, 1988). , 1991). The main eruptive events of the Ischia-ProcidaPhlegrean Fields system suggest at least five eruptive cycles, ranging in age from 135 ky to prehistorical and historical times.
The widespread volcanic activity, which controlled the stratigraphic architecture of the Naples Bay during the Late Quaternary, has disallowed the application of a classical stratigraphic approach, due to the occurrence of interlayered sedimentary sequences and intervening volcanic bodies (volcanites and volcaniclastites). , 1994) and to the highstand phase of sea level (HST; Posamentier & Vail, 1988). A sketch stratigraphic diagram of the SDTQ and its components has been constructed in order to clarify the stratigraphic relationships between systems tracts (Fig.
Buried and isolated volcanic mounds, genetically related to the Vesuvius activity, have been distinguished through seismic interpretation (fig. 17). 5 km offshore the Vesuvius and corresponds to a main magnetic anomaly (fig. 18) reaching intensity of 400 nT. It shows an acoustically transparent seismic facies and three main elevated peaks. Fig. 18. , 2010). The Torre del Greco volcanic structure is depicted by the profile. The total magnetic field offshore the Somma-Vesuvius volcanic complex shows that the shape of the anomalies is dipolar; there is no apparent effect caused by the occurrence of remnant magnetization with a different direction to that of the present-day main field (fig.
Topics in the Theory of Lifting. by A. Ionescu Tulcea, C. Ionescu Tulcea