Calcite is a common mineral precipitated within upper crustal fault zones and associated
fractures, forming veins, mineral cements and fault coatings. It has the potential to be dated …

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

A transformative advance in Earth science is the development of low‐temperature
thermochronometry to date Earth surface processes or quantify the thermal evolution of …

Rare earth element geochemistry in carbonate rocks is utilized increasingly for studying both
modern oceans and palaeoceanography, with additional applications for investigating water …

In this paper we present the first detailed geochemical study of the world-famous actively
forming Pamukkale and Karahayit travertines (Denizli Basin, SW-Turkey) and associated …

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 …

Direct evidence for fault reactivation is crucial for understanding long-term fault behavior and
reconstruction of fluid circulation and hydrocarbon migration and accumulation during active …

Mineralisation associated with fault, vein and shear zone systems can be related to
processes that operated when those systems were active. Despite the complexity of …

The depositional and erosional history of the Lapis Tiburtinus endogenic travertine located
circa 25 km to the east of Rome, Central Italy, near the Colli Albani quiescent volcano, is …

Natural CO2 discharges are abundant in Turkey as evident from ongoing deposition of
recent terrace-mound travertines and emplacement of significant travertine vein and breccia …