Understanding the behavior of fluids in seismically active faults and their chemical-physical
(dis) equilibrium with the host rock is important to understand the role of fluids upon …

The mechanical discontinuities in the upper crust (ie, faults and related fractures) lead to the
uprising of geothermal fluids to the Earth's surface. If fluids are enriched in Ca2+ and HCO3 …

Carbon capture and storage (CCS) technology is routinely cited as a cost effective tool for
climate change mitigation. CCS can directly reduce industrial CO2 emissions and is …

Studying travertine deposits and the network of banded calcite veins that form their roots in
the substratum can place important constraints on neotectonic activity and the …

Travertine-depositing hot springs can generate various carbonate minerals with or without
the participation of microorganisms. They thus serve as good natural laboratories to study …

Banded Ca‐carbonate veins in travertine deposits are efficient recorders of the
compositional fluctuations of geothermal fluids flowing (or flowed) from deep reservoirs up to …

Linking the architecture of structural conduits with the hydrothermal fluids migrating from the
reservoir up to the surface is a key-factor in geothermal research. A contribution to this …

Travertine deposits have long been considered as powerful tools for investigating
neotectonics and reconstructing palaeoseismic events. We document, for the first time, the …

Facies character, diagenesis, geochemical signature, porosity, permeability, and geometry
of the upper Pleistocene Tivoli travertines were investigated integrating information from six …

This study examines the impact of polyphase tectonics on the development of structurally
controlled hydrothermal fluid pathways in carbonate geothermal reservoirs. Our case study …