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 …

Carbonate build-ups in lakes, hydrothermal and fluvial settings are characterized by
distinctive geometry, spatial distribution, fabrics and geochemical signature but also by …

Abstract In the Denizli Basin (Turkey), located in the western Anatolian extensional province,
travertine and tufa deposition has been an ongoing process for at least 600,000 years …

The terrestrial limestones forming at the emergence of thermal springs show a variety of
unusual depositional facies. The specific lithological and petrological features of these …

Springs sustain groundwater-dependent ecosystems and provide freshwater for human use.
Springs often occur because faults modify groundwater flow pathways leading to discharge …

This second edition of Atlas of Structural Geology features a broad and inclusive range of
high-quality mesoscale and microscale full-color photographs, descriptions, and captions …

The study of hydrothermal travertines contributes to the understanding of the interaction
between physico‐chemical processes and microbial mats in carbonate precipitation. Three …

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 …

Abstract Middle–Late Pleistocene tectonic activity has been inferred through studies on
travertine deposits exposed in a tract of the hinterland Northern Apennines. A detailed study …