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Hydrogeological Modelling Of Geothermal Waters In Pamukkale, Western Anatolia, Turkey
2017
Zenodo
The study area, located in the eastern part of the continental rift zone of the Büyük Menderes within the Menderes Massif, western Anatolia, is composed of Paleozoic metamorphic rocks, Mesozoic limestones and Eocene via Pliocene to Quaternary sediments. Paleozoic marbles, quartzites and carbonate schists, Mesozoic limestone, Pliocene sediments and Quaternary alluvium and travertine serve as permeable rocks for the geothermal waters. The geothermal waters in Pamukkale and environs with outlet
doi:10.5281/zenodo.580900
fatcat:yznilr2smjdzjfrlj5ugrjrntq