2019
DOI: 10.1038/s41598-019-53696-z
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Fault-controlled deep hydrothermal flow in a back-arc tectonic setting, SE Tyrrhenian Sea

Abstract: Understanding magmatic systems and deep hydrothermal circulation beneath arc-volcanoes provides insights into deep processes associated with slab-subduction and mantle-wedge partial melting. Here we analyze hydrothermal flow below a structural high (Capo Vaticano Ridge, CVR) located offshore Capo Vaticano (western Calabria) and affected by magmatic intrusions generated from above the Ionian subducting-slab. In order to explain observations, we combine geophysical and numerical modelling results. Fluid-flow mod… Show more

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Cited by 13 publications
(10 citation statements)
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“…The final Quaternary phase (Figure 9d) is dominated by the building of Vavilov volcano (2.4–0.1 Ma; Sartori, 2005 and references therein), by the opening of the Marsili Basin (see ODP 650 in Figure 3; Kastens et al., 1988) and by the build‐up of the central Marsili volcano (age ranging from 0.7 Ma; Marani & Trua, 2002; to 0.003 Ma; see Iezzi et al., 2014). The opening of the Marsili back‐arc basin is coeval with the formation of the Aeolian volcanic arc whose spatial evolution is linked to the decoupling and roll‐back of the slab below the Calabrian Arc (De Astis, Ventura, & Vilardo, 2003; Bortoluzzi et al., 2010; Loreto et al., 2019). Along the eastern/southeastern Tyrrhenian Basin, a compressional phase acting during upper Pliocene/lower Pleistocene (Argnani & Trincardi, 1988, 1993) caused localized inversion of basins, as in the Paola Basin.…”
Section: Discussionmentioning
confidence: 99%
“…The final Quaternary phase (Figure 9d) is dominated by the building of Vavilov volcano (2.4–0.1 Ma; Sartori, 2005 and references therein), by the opening of the Marsili Basin (see ODP 650 in Figure 3; Kastens et al., 1988) and by the build‐up of the central Marsili volcano (age ranging from 0.7 Ma; Marani & Trua, 2002; to 0.003 Ma; see Iezzi et al., 2014). The opening of the Marsili back‐arc basin is coeval with the formation of the Aeolian volcanic arc whose spatial evolution is linked to the decoupling and roll‐back of the slab below the Calabrian Arc (De Astis, Ventura, & Vilardo, 2003; Bortoluzzi et al., 2010; Loreto et al., 2019). Along the eastern/southeastern Tyrrhenian Basin, a compressional phase acting during upper Pliocene/lower Pleistocene (Argnani & Trincardi, 1988, 1993) caused localized inversion of basins, as in the Paola Basin.…”
Section: Discussionmentioning
confidence: 99%
“…Traditionally, the term "fluids" include liquids and gases that fill void spaces arising from deformation in rock masses. Fluids are also magmatic melts, which themselves are sources of hydrothermal fluids ascending to the earth's surface through conducting faults [21]. The migration of fluid solutions affects the shear resistance of the faults through the lubrication and hydraulic effects on the walls of the fractured rock.…”
Section: Methodological Basismentioning
confidence: 99%
“…There are numerous Computational Fluid Dynamics (CFD) solvers such as Ansys-Fluent, Feflow, Visual Modflow, Comsol Multiphysics which can be used to perform numerical simulations in solving heat and fluid flow problems in earth sciences (Sarkar et al, 2002;MacKenna and Blackwell, 2004;Üner and Doğan, 2019;Loreto et al, 2019). Among them, finite volume based on the CFD Ansys-Fluent program was selected in this study, since it is capable of solving simultaneous equations of mass, momentum and energy conservations.…”
Section: Numerical Modelmentioning
confidence: 99%
“…Therefore, high-permeability values are assigned to fault zones in our models. Heat and fluid flow properties which are presented in Table (1) and ( 2) are taken from these previous studies (McKenna and Blackwell 2004;Magri et al, 2010;Loreto et al, 2019;Üner and Düşünür Doğan 2021).…”
Section: Numerical Modelmentioning
confidence: 99%
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