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Authors: | Natale, Jacopo* Vitale, Stefano* Giordano, Guido* Fedele, Lorenzo* Lucci, Federico* Vona, Alessandro* Prinzi, Ernesto Paolo* Tramparulo, Francesco D'Assisi* Isaia, Roberto* Ciarcia, Sabatino* |
Title: | The Taverna San Felice Dike (NE of Roccamonfina Volcano): Unraveling Magmatic Intrusion Processes and Volcano‐Tectonics in the Tyrrhenian Margin of the Southern Apennines | Journal: | Geochemistry Geophysics Geosystems | Series/Report no.: | /24 (2023) | Publisher: | Wiley-Agu | Issue Date: | 20-Jul-2023 | DOI: | 10.1029/2023GC010994 | Keywords: | magmatic dike Tectonic extension |
Abstract: | The Roccamonfina volcano is located within the Garigliano Graben (southern Apennines, Italy) and has been active throughout the Middle-Late Pleistocene. Along its polyphase volcanic history (630–55 ka), including several caldera-forming eruptions (385–230 ka), several effusive/mildly explosive monogenetic events occurred along the volcano slopes, within the summit caldera, and along the graben-bounding carbonate reliefs. In this paper, we present a multidisciplinary study of a mafic magmatic feeder dike intruded within the Meso-Tertiary carbonates and overlying Lower Pleistocene breccias of Mt Cesima, northeast of the Roccamonfina volcano. We performed a stratigraphic and structural survey of the area and petrographic analyses on several samples of the dike. Results indicate that a ∼1 km long fissure fed an eruption that also emplaced a Strombolian pyroclastic sequence. Petrological data show that an open-system mafic recharge fueled the tephritic magma that fed the eruption, whereas no evidence of significant pre/syn-eruptive assimilation of carbonate has been identified. Stratigraphic and petrological data do not allow to firmly constrain the timing of the eruption, which could belong both to the pre-Brown Leucitic Tuff (>354 ka) and to the post-White Trachytic Tuffs (<230 ka) epochs of activity of the Roccamonfina volcano. Structural data show that the dike is broadly oriented E-W and changes direction toward NE-SW in correspondence with a pre-existing fault damage zone. We suggest that magma was intruded during an N-S trending extensional event in the Middle Pleistocene, whose prolonged activity resulted in regional uplift and exhumation of regional significance. |
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Geochem Geophys Geosyst - 2023 - Natale.pdf | Open Access Published Article | 22.9 MB | Adobe PDF | View/Open |
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