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Titlebook: Caves and Karst of Turkey - Volume 2; Geology, Hydrogeolog Gültekin Günay,Koray T?rk,Eric Gilli Book 2022 The Editor(s) (if applicable) and

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樓主: Fillmore
11#
發(fā)表于 2025-3-23 12:00:33 | 只看該作者
Vermeidung und Abbau korrosiver Energie,tification heights of up to 2000?m are especially seen in the vicinity of Antalya city and generally in the Southwest of Turkey’s Taurus Mountains. Especially, Antalya and its surroundings present such typical karstification properties. K?rkg?zler karst springs in the north of Antalya plain are one
12#
發(fā)表于 2025-3-23 16:38:12 | 只看該作者
13#
發(fā)表于 2025-3-23 21:36:39 | 只看該作者
Vermeidung und Abbau korrosiver Energie,exist discharging from the carbonates of the Taurus Mountain range of Southern Turkey. These large springs are characterized by great discharge rates (generally over 10?m./s) which have a large residence or turnover times of many years or decades of years, and large, well-regulated spring flows. The
14#
發(fā)表于 2025-3-24 01:39:24 | 只看該作者
Innovation and the Open Innovation concept, of watery and dry sinkholes (obruks) formed in the lacustrine Neogene limestone in the Karap?nar plain is close to thousands. Groundwater with unconfined aquifer characteristics appears close to the surface and form sinkhole lakes by taking part in some of the sinkholes. The basement formation unde
15#
發(fā)表于 2025-3-24 05:24:26 | 只看該作者
16#
發(fā)表于 2025-3-24 09:50:23 | 只看該作者
https://doi.org/10.1007/978-3-8349-8090-8te Tertiary into the Quaternary period. The Quaternary tectonism is characterized by normal faults and, in this western part, by block faults. With uplift, karstification increased and the surface drainage of many lakes and rivers was transformed into subsurface drainage. The climate changed drastic
17#
發(fā)表于 2025-3-24 10:48:17 | 只看該作者
18#
發(fā)表于 2025-3-24 15:49:19 | 只看該作者
19#
發(fā)表于 2025-3-24 19:40:05 | 只看該作者
20#
發(fā)表于 2025-3-25 01:42:52 | 只看該作者
Conceptual framework and hypotheses,e Midyat limestone is highly karstified. Karstic springs discharging from the Midyat formation are located mainly at the eastern part where this formation outcrops over large areas. The hydrogeological properties of the lithological units are described mainly based on the data obtained from the shal
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