Traditionally, fresh water carbonate research has focused on the sedimentology and
palaeontology of ancient lacustrine deposits. Lithofacies in such low‐energy deposits are …

Morphologically-different deposits of thermal travertines are known worldwide, but what
factors controlled their morphology, volume, and growth for tens of thousands of years is …

Faults and associated fracture networks can significantly influence regional flow of
groundwater, hydrocarbons and other fluids. The distribution of CO2 springs and seeps …

Groundwaters of the southern Colorado Plateau–Arizona Transition Zone region are a
heterogeneous mixture of chemically diverse waters including meteoric (epigenic) fluids …

Fissure ridge travertines grown from geothermal springs of Denizli Basin, southwestern
Turkey, are investigated through stratigraphic, structural, geochemical, and …

Oxygen isotope ratio (δ 18 O) value deviations from the Meteoric Water Line with no
significant change in the hydrogen isotope (δ 2 H) composition have been reported in …

The way faults control upward fluid flow in nonmagmatic hydrothermal systems in
extensional context is still unclear. In the Eastern Pyrénées, an alignment of twenty‐nine hot …

This paper presents an integrated study directed toward an understanding of the tectonic
control on the hydrothermal circulation and resulting deposition of Middle–Late Pleistocene …

We describe the structural and petrophysical evolution of extensional fault zones developed
in low porosity, poorly lithified, quartz-dominated sandstones from the Mio-Pliocene …

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 …