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  • 1
    Online Resource
    Online Resource
    Cham : Springer International Publishing | Cham : Imprint: Springer
    Keywords: Geology. ; Physical geography. ; Sedimentology.
    Description / Table of Contents: Caves And Karst Of Turkey -- Turkey’s Karst And Water Resources -- Karst Hydrogeology Of Manavgat River Basin -- Karst Of Antalya Travertine, South West Of Turkey -- Geologic And Hydrogeologic Factors Affecting Sinkhole (Obruk) Development In Central Turkey -- Karst Areas Of Turkey -- Karst Springs Of Turkey -- Dumanli Karst Springs, Manavgat River, Antalya, Turkey -- Karst Hydrogeology In Geothermal Reservoirs -- Karstic Hot Water Aquifers In Turkey.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XVII, 118 p. 97 illus., 73 illus. in color.)
    Edition: 1st ed. 2022.
    ISBN: 9783030953614
    Series Statement: Cave and Karst Systems of the World
    Language: English
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  • 2
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Caves. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (125 pages)
    Edition: 1st ed.
    ISBN: 9783030953614
    Series Statement: Cave and Karst Systems of the World Series
    DDC: 551.44709561
    Language: English
    Note: Intro -- Foreword -- Preface -- Contents -- About the Authors -- 1 Karst of Turkey -- Abstract -- 1.1 Introduction -- 1.2 Tectonic of Turkey -- 1.3 Tertiary Units -- 1.3.1 Karst in the Taurus Area -- References -- 2 Turkey's Karst and Water Resources -- Abstract -- 2.1 Introduction -- 2.2 Gypsum Karst -- 2.2.1 General Overview in Gypsum Karst -- 2.2.2 Gypsum Karst in Turkey -- 2.3 Karst Water Resources -- 2.3.1 Taurus Karst Region -- 2.3.2 Central Anatolia Karst Region -- 2.3.3 South Anatolia Karst Region -- 2.3.4 North Anatolia and Thrace Karst Region -- 2.4 Conclusions -- References -- 3 Karst of Antalya Travertine, Southwest of Turkey -- Abstract -- 3.1 Introduction -- 3.2 Geographical Setting -- 3.3 Geological Setting -- 3.3.1 Stratigraphy -- 3.3.1.1 Autochthonous Units -- Mesozoic -- Cenozoic -- 3.3.1.2 Allochthonous Units -- Çataltepe Unit -- Alakirçay (Ispartaçay) Unit -- Tahtalidag Unit -- 3.3.2 Structural Geology -- 3.3.3 Paleogeography -- 3.4 Karst Geomorphology -- 3.4.1 Travertine -- 3.4.2 Karst Features -- 3.4.3 Poljes and Dolines -- 3.4.4 Submarine Discharge -- 3.5 Hydrogeological Characterization -- 3.5.1 General Hydrogeology -- 3.5.2 Kirkgözler Springs -- 3.5.3 Düdenbaşi Spring -- References -- 4 Konya-Karapinar Sinkholes (Obruks) of Turkey -- Abstract -- 4.1 Introduction -- 4.2 Geology -- 4.2.1 Konya-Karapinar Plain -- 4.2.2 Geology of Obruk Plain -- 4.2.3 Structural Geology -- 4.3 Hydrogeological Units -- 4.4 Obruk's Development -- 4.4.1 Origin of Obruks -- 4.4.2 Morphometry of Obruks -- 4.4.3 Recen Obruks -- 4.4.4 Old Obruks -- 4.5 Conclusions -- References -- 5 Origin and Catchment Area of the Köprüçay Karst Springs -- Abstract -- 5.1 Introduction -- 5.2 Geological Units and Hydrogeological Functions -- 5.2.1 Autochthonous Units -- 5.2.1.1 Paleozoic -- 5.2.1.2 Mesozoic -- 5.2.1.3 Cenozoic. , 5.2.1.4 Geological Units and Hydrological Functions -- 5.2.2 Allochthonous Units -- 5.3 Bulasan and Beşkonak Flow Records -- 5.4 Conclusion -- References -- 6 Tectonic Influences on Groundwater Flow Systems in Karst of the Southwest Taurus Mountains, Turkey -- Abstract -- 6.1 Introduction -- 6.2 Tectogenetic Control of Karstification -- 6.3 The Effect of the Quaternary Ice Age Term on Taurus Karst Processes -- 6.4 The Major Controls on the Karst Hydrogeology -- 6.5 Antalya Travertine Plateau -- 6.6 Hydrothermal Pamukkale Travertine -- References -- 7 Karst Areas of Turkey -- Abstract -- 7.1 Introduction -- 7.2 Karst Limestone -- 7.2.1 The Taurus Mountains -- 7.2.2 Thrace and the Black Sea Mountains -- 7.2.3 The Western Anatolia -- 7.2.4 The Central Anatolia -- 7.2.5 The Eastern Anatolia -- 7.2.6 The South Eastern Anatolia -- 7.3 Gypsum Karst -- 7.4 Spectacular Karst Features of Turkey -- 7.4.1 Large Poljes -- 7.4.2 Obruks -- 7.4.3 Tufa and Travertine Deposits -- 7.5 Karst Hydrogeology -- 7.6 Eustatism and Active Tectonic -- 7.7 Conclusion -- References -- 8 Karst Springs of Turkey: Hydrogeology of the Kirkgözler Karst Springs, Antalya -- Abstract -- 8.1 Introduction -- 8.2 Geologic Setting -- 8.3 Hydrogeology -- 8.3.1 Aquifers -- 8.3.2 Karst Springs -- 8.3.2.1 Kirkgözler Springs -- 8.3.2.2 Düdenbaşi Spring -- 8.4 Hydrochemistry -- 8.5 Natural and Artificial Tracing -- 8.6 Conclusions -- References -- 9 The Karst Springs of Antalya, Turkey -- Abstract -- 9.1 Introduction -- 9.2 The Oluköprü Springs -- 9.3 Spring Discharge Rates -- 9.4 Recharge Areas of the Springs -- 9.5 Allochthonous Units -- 9.6 Conclusion -- References -- 10 Karst Hydrogeology of Pamukkale Thermal Springs, Denizli, Turkey -- Abstract -- 10.1 Introduction -- 10.2 Hydrogeological Properties -- 10.3 Hydrogeochemical Aspects -- 10.4 Pollution and Protection Studies -- 10.5 Conclusion. , References -- 11 Beyazsu and Karasu Karst Springs Mardin-Nusaybin Area (SE Turkey) -- Abstract -- 11.1 Introduction -- 11.2 Geology of the Deep Aquifer Systems -- 11.3 Hydrogeological Setting -- 11.4 Water Quality -- 11.5 Deep Aquifer System -- 11.6 Conclusions -- References -- 12 Karst Hydrogeology of Muğla-Gökova Karst Springs -- Abstract -- 12.1 Introduction -- 12.2 The Springs of Gökova -- 12.2.1 Azmak Spring Group -- 12.2.2 The Akbük Bay Springs -- 12.3 Hydrogeological Characteristics of the Rocks -- 12.3.1 The Hydrogeological Characteristics of Autochthonous Units -- 12.3.2 The Hydrogeological Characteristics of the Allochthonous Units -- References -- 13 Karst Springs and Waterfalls-Zamanti River, Eastern Turkey -- Abstract -- 13.1 Introduction -- 13.2 Geology -- 13.3 Hydrology -- 13.4 Hydrogeology -- 13.5 Recession Curve Analysis of the Large Karstic Springs -- 13.6 Conclusion -- References -- 14 Niğde-Pozanti Şekerpinari Springs, South of Turkey -- Abstract -- 14.1 Introduction -- 14.2 Geological Structure -- 14.3 Hydrology -- 14.4 Water Chemistry -- References -- 15 Karstic Hot Water Aquifers in Turkey -- Abstract -- 15.1 Introduction -- 15.2 General Properties of the Karstic Hot Water Aquifers -- 15.3 Important Karstic Hot Water Aquifers and Their Classification According to Age -- 15.3.1 Cenozoic Limestone Formations -- 15.3.2 Mesozoic Crystalline Limestone Formations -- 15.3.3 Paleozoic Marble Formations -- 15.4 Exploitation Problems in Karstic Hot Water Aquifers -- 15.5 Results and Suggestions -- References.
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  • 3
    ISSN: 1432-0495
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The study area is situated within the complex structure and karst system of the western Taurids. Basinwide interpretation of the structural features, each of which has great importance, will enlighten many complicated hydrogeologic problems encountered in the area. Thus, considering the previous views on the structural geology of the area, an interpretation of the structural and tectonic features of the study area by means of satellite images was undertaken, and based on the data gained, new approaches were suggested to solve the hydrogeological problems. In particular, determination of the recharge-discharge mechanisms of the Olukköprü and Dumanli karst springs, which are the most important karst groundwater discharge points in the region, has been attempted. Within the framework of this study, a tectonic-lineament map of a large area covering Eğirdir, Beyşehir, and Suğla lakes at the north and the basins to the south of these lakes was prepared.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1435-0157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Les données hydrochimiques et sur la qualité de l'eau (sauf la microbiologie) ont été tirées d'un suivi pendant deux ans; les résultats des analyses indiquent que la plus forte pollution de l'eau souterraine est observée dans les parties centrale et orientale de la ville d' Eskişehir. La dégradation de la qualité de l'eau souterraine en dehors de la zone urbaine est due aux activités agricoles. La pollution de l'eau souterraine la plus grave dans la plaine d'Eskişehir est due aux composés azotés (ammoniaque, nitrite et nitrate). Les concentrations en ammoniaque, en nitrite et en nitrate des 51 puits siuvis sont respectivement comprises entre 0.01 et 1.65 mg/L, 0.01 et 1.80 mg/L, et 1.1 à 257.0 mg/L. Les concentrations en orthophosphate de l'eau souterraine varient entre 0.01 et 1,25 mg/L. Des variations saisonnières considérables de la qualité de l'eau souterraine ont été observées. En général, la qualité de l'eau souterraine est meilleure en saison humide qu'en saison sèche.
    Abstract: Los datos de hidroquímica y de calidad del agua (excepto biológica), obtenidos a raíz de un programa de muestreo y análisis de dos años de duración, indican que las concentraciones mayores de contaminantes aparecen en las zonas central y este de la ciudad. La degradación en la calidad del agua subterránea en el exterior del núcleo urbano está asociada a las actividades agrícolas. La contaminación más importante en el llano de Eskişehir es por componentes nitrogenados (amonio, nitrito, nitrato). Las concentraciones de amonio, nitrito y nitrato de los 51 pozos muestreados oscilan entre 0.01–1.65 mg/L, 0.01–1.80 mg/L y 1.1–257.0 mg/L, respectivamente. Las concentrationes de ortofosfato en el agua subterránea oscilan entre 0.01–1.25 mg/L. Se observó también una gran variación estacional en la calidad de estas agua. En general, la calidad de las mismas en épocas húmedas es mejor que en épocas secas.
    Notes: Hydrochemical and water-quality (except biological) data obtained through a two-year sampling and analysis program indicate that the highest concentrations of groundwater pollution occur in the central and eastern parts of Eskişehir city. Groundwater quality degradation outside the urban area results from agricultural activities. The most serious pollution of groundwater in the Eskişehir plain is from nitrogen compounds (ammonia, nitrite, and nitrate). The concentrations of ammonia, nitrite, and nitrate of the 51 surveyed water wells range from 0.01–1.65 mg/L, 0.01–1.80 mg/L, and 1.1–257.0 mg/L, respectively. Orthophosphate concentrations in groundwater range from 0.01–1.25 mg/L. Considerable seasonal fluctuation in the groundwater quality was observed. In general, the groundwater quality in wet seasons was better than the quality in dry seasons.
    Type of Medium: Electronic Resource
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