Abstract The Plio-Quaternary fluvio-lacustrine sediments located in the Uşak-Karahallı area
(SW-Anatolia) have been investigated with multidisciplinary approaches to highlight their …

Although fossil fluvial travertines have been described, factors controlling their formation are
poorly understood because of the paucity of their modern counterparts. To disclose …

The Quaternary calcareous tufas precipitated in the Kurkur Oasis area in the southern
Western Desert of Egypt were analyzed to determine their implications for the construction of …

The Tibetan Plateau is known as the core area of the third pole of the Earth and is a key area
for global climate change research. This study uses the Zabuye Salt Lake travertine dam as …

The Bahçecik travertines, located in Gümüşhane (NE-Turkey) have been investigated for the
first time using a multidisciplinary approach, which included sedimentological (lithofacies …

Palaeoclimatic and palaeoenvironmental proxy data are presented for the Late Quaternary
based on mineralogical, geochemical and palynological analysis of a palaeosoil-sediment …

In this study, the correlation of the Balkayası travertine formations with the Salanda Fault
Zone (SFZ) located within the Central Anatolian Volcanic Province (CAVP) was investigated …

Late Pleistocene travertine deposits along the Jordan Valley and the north-east margin of
the Dead Sea were identified at three locations: Deir Alla, Suwayma and Az Zara areas. The …

The Başkale Basin is located in the easternmost part of Türkiye, within a tectonically active
area, and located at the intersection of Europe, Asia and the Middle East. In this study, the …

Development of Quaternary fluvial tufa buildings are often associated with warm and humid
phases and are commonly used as climate indicators. El Nogal de El Batán Holocene fluvial …