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- W2977895909 abstract "The Pleistocene travertine terraces of Antalya are well known karstic features and have been investigated by several authors. They are principally the correlated sediments of the karstic erosion in the Korkuteli-Kestel-Bucak area to the north. Some parts of these travertines have already been attributed to Pliocene, but no travertines older than Pliocene have been indicated in the area. According to paleogeomorph ological studies, karstic erosion must have started during the late middle Miocene as a part of the formation of the denudational surface of Erol's D.I system in the Taurus Mountains. This karstic activity had started as a surficial process under the influence of a warm-humid climate and penetrated as horizontal extending karstic systems beneath this denudational surface. These karstic systems have gradually developed in vertical extent, as the base level lowered and the step-like geomorphological upper Miocene (D.II) and Pliocene (D.III) denudational surface systems developed. Thus, the intramountain tectonic basins solutionally deepened and enlarged in limestones and as correlated sediments of this karstic phenomena, the Asartepe, Tasyayla and Kocaaliler travertine terraces developed at an altitude of 1200-800 m in the Upper Aksu basin to the north during the late upper Miocene, and eventually in the Messinian. As for the correlated sediments of karstic solution in the Tahtali Dag area in the south, the Saylica fan-delta-travertine complex at an altitude of 700-300 m developed during the Pliocene. The travertine terraces of Antalya City at -55 to 300 m are the correlated sediments of the karstic solutional activity in the Kestel-Bucak polje depressions during the Quaternary." @default.
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- W2977895909 date "1993-01-01" @default.
- W2977895909 modified "2023-10-16" @default.
- W2977895909 title "TRAVERTINE FORMATIONS IN THE ANTALYA AREA AS CORRELATED SEDIMENTS OF KARSTIC EROSIONAL PHASES IN THE SURROUNDING TAURUS MOUNTAINS" @default.
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