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 …

This paper focuses on brittle deformation and fluid-rock interaction, for enhancing
permeability in carbonate geothermal reservoir. The relationships between fractures and …

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 …

Active faults within the southern Apennines fold-and-thrust belt modulate the present-day
upwelling of hydrothermal fluids at surface. In the Monte Alpi area, we investigated the …

Travertine deposits in western Turkey are very well‐exposed in the area of Kocabaş, in the
eastern part of the Denizli Basin. The palaeoclimatic significance of these travertines is …

Abstract Knowledge of earthquake source faults is crucial for the calculation of robust
Coulomb stress models. However, source faults are often poorly constrained, especially for …

Abstract 3D modelling represents a powerful tool to characterize the geobody architecture of
depositional systems. Several examples have been proposed in literature both for marine …

Genetic and diagenetic processes of travertine were examined at Futamata hot spring,
where both active and inactive (subfossil and fossil) travertines are present. Geochemical …

The reservoir characterization of the Brazilian Santos Basin's pre-salt carbonates is a major
challenge due to the faciological and depositional complexity, providing high lateral and …

Travertines are generally considered as carbonate deposits related to Ca-rich hot springs.
Ca-deficiency hot springs, however, can also produce travertines under suitable conditions …