@article{article_579986, title={THE GEOLOGY OF AROUND ESKİŞEHİR AND THERMAL WATER SOURCES}, journal={Bulletin of the Mineral Research and Exploration}, volume={103-104}, pages={15–15}, year={1985}, author={Gözler, M. Ziya and Cevher, Fahrettin and Küçükayman, Arif}, abstract={<p class="MsoNormal" style="text-align:justify;">The investigated area comprises
Eskişehir province and its immediate vicinitiy. The basement consist of
Pre-Triassic tectonic unit comprising metamorphic, ophiolitic and
metadetritics. Jurassic is represented by detritics and limestones. These are
unconformably overlain by sediments and volcanic rocks of Paleocene, Eocene,
Miocene and Pliocene age. The uppermost unit consist of sandstones of
Pleistocene age. The magmatic rocks are respectively represented by porpyritic
granite and an assemblage of andesite, bazalt and tüff. The vertical fault
systems passing throuh North of Eskişehir, responsible for the present
morphology trends E-W and the northern and southern system dip respectively to
the S and N the reverse faulting of the region is belived to have played and
important role in the tectonic evolution of studiee area. </p> <p> </p>}, number={103-104}, publisher={Maden Tetkik ve Arama Genel Müdürlüğü}