[HTML][HTML] Fluid-rock interaction, skarn genesis, and hydrothermal alteration within an upper crustal fault zone (Island of Elba, Italy)
The Terranera magnetite-hematite-pyrite deposit of the Island of Elba (Italy) is an historical
skarn deposit hosted by a fault zone of regional importance (Zuccale Fault) and by its …
skarn deposit hosted by a fault zone of regional importance (Zuccale Fault) and by its …
Deformation mechanisms of blueschist facies continental metasediments may offer insights into deep episodic tremor and slow slip events
Exhumed fossil subduction zones are archives of the deformation conditions and
mechanisms from depths not directly accessible. Microstructural analysis of samples …
mechanisms from depths not directly accessible. Microstructural analysis of samples …
Stretched thin: Oligocene extrusion and ductile thinning of the Basal Unit along the Evia Shear Zone, NW Cyclades, Greece
TA Ducharme, DA Schneider, B Grasemann… - …, 2022 - Wiley Online Library
We present field‐based structural, geochronological, and petrological evidence for a major
new Oligocene extensional shear zone, the Evia Shear Zone (ESZ), on the island of Evia in …
new Oligocene extensional shear zone, the Evia Shear Zone (ESZ), on the island of Evia in …
Structural characterization and K–Ar illite dating of reactivated, complex and heterogeneous fault zones: lessons from the Zuccale Fault, Northern Apennines
Abstract We studied the Zuccale Fault (ZF) on Elba, part of the Northern Apennines, to
unravel the complex deformation history that is responsible for the remarkable architectural …
unravel the complex deformation history that is responsible for the remarkable architectural …
[HTML][HTML] Tectonic-Sedimentary evolution of the Tuscan shelf (Italy): Seismic-stratigraphic/structural analysis of Neogenic succession in the Tyrrhenian Sea between …
A reinterpretation of the vectorized version of public vintage seismic profiles in the
Tyrrhenian Sea (Italy), between Elba Island and Monte Argentario promontory, was …
Tyrrhenian Sea (Italy), between Elba Island and Monte Argentario promontory, was …
[HTML][HTML] Syn-tectonic contact aureole and metasomatic reaction zones in carbonate and pelitic host rocks (Elba Island, Italy)
In this paper we describe deformation processes and metasomatic reaction zones
developed in a contact aureole formed in the upper crust (c. 6 km depth) due to the …
developed in a contact aureole formed in the upper crust (c. 6 km depth) due to the …
Metamorphic Domes in Northern Tunisia: Exhuming the Roots of Nappe Belts by Widespread Post‐Subduction Delamination in the Western Mediterranean
G Booth Rea, S Gaidi, F Melki, W Marzougui… - …, 2023 - Wiley Online Library
Cenozoic extension in the Western Mediterranean has been related to the dynamics of back‐
arc domains. Although, in most of its orogenic belts extension propagated into the fore‐arc …
arc domains. Although, in most of its orogenic belts extension propagated into the fore‐arc …
Cyclic brittle‐ductile oscillations recorded in exhumed high‐pressure continental units: A record of deep episodic tremor and slow slip events in the northern …
F Giuntoli, G Viola - Geochemistry, Geophysics, Geosystems, 2021 - Wiley Online Library
The geological record of deep fossil seismogenesis in subduction zones is limited due to
common rock overprinting during exhumation and only a few regions expose well …
common rock overprinting during exhumation and only a few regions expose well …
[HTML][HTML] Reappraising the seismogenic potential of a low-strain rate region: Active faulting in the eastern Siena Basin (southern Tuscany, Italy)
We investigated the active tectonics and earthquake potential of the eastern Siena Basin, a
slowly deforming portion of southern Tuscany in the inner Northern Apennines. This region …
slowly deforming portion of southern Tuscany in the inner Northern Apennines. This region …
Fractures, fluid flow and inherited structures in geothermal systems: inputs from the Fe-ore deposits of eastern Elba Island (Northern Apennines, Italy)
Geothermal systems in terrains affected by polyphase deformation have reservoirs with a 3D
geometry that is always difficult to predict. In this paper we describe a fossil exhumed …
geometry that is always difficult to predict. In this paper we describe a fossil exhumed …