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  • 1
    Online Resource
    Online Resource
    Mineral and Thermal Waters of Southeastern Europe. (2015)
    Cham :Springer International Publishing AG,
    Details
    Keywords: Hydraulic engineering. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (174 pages)
    Edition: 1st ed.
    ISBN: 9783319253794
    Series Statement: Environmental Earth Sciences Series
    URL: https://ebookcentral.proquest.com/lib/geomar/detail.action?docID=4091120
    DDC: 553.7909496
    Language: English
    Note: Intro -- Preface -- Contents -- 1 Geology of South-Eastern Europe -- Abstract -- Introduction -- The Synthesis' Approach -- Definition of the Research Area -- Terminology -- Geology of South-East Europe -- Time-Space Framework of the Vardar Tethys Ocean -- Pre-Vardar--Tethyan Geology of SEE -- Pre-Vardar--Tethyan Geology of the European Continent -- Pre-Vardar--Tethyan Geology of the Gondwana Continent -- Syn-Vardar--Tethyan Geology of SEE -- Syn-Vardar--Tethyan Geology of the Mega-Suture -- Syn-Vardar--Tethyan Geology of the European Side -- Syn-Vardar--Tethyan Geology of the Gondwana Side -- Post-Vardar--Tethyan Geology of South-East Europe -- The Late Cretaceous, Its Magmatism and the Problem of the Sava Zone -- Cenozoic: Period of an Unstable Orogen, Widespread Magmatism and Formation of Extensional, Sedimentary Basins -- Geotectonic Regime in the Cenozoic -- Cenozoic Sedimentary Basins -- Cenozoic Magmatism -- Acknowledgments -- References -- 2 Mineral and Thermal Waters in the Croatian Part of the Pannonian Basin -- Abstract -- Introduction -- Geological Settings -- Mineral and Thermal Water Locations and Categorization -- Hydrogeochemical Characteristics -- Utilization -- Sustainability and Environmental Impacts of Thermal Water Utilization -- Discussion and Concluding Remarks -- Acknowledgments -- References -- 3 Thermal Waters in Bulgaria -- Abstract -- Introduction -- Geological Background -- Thermal Field -- Hydrothermal Regions -- Thermal Water Characteristics -- Temperature and Flow Rate -- Chemical Composition -- Thermal Water Application -- Administration and Legislation -- Conclusions -- Acknowledgments -- References -- 4 Mineral Waters of Montenegro -- Abstract -- Introduction -- Mineral and Thermal Waters of Montenegro -- Coastal Zone (I Zone) -- Ulcinj Area (IA) -- Igalo Area (IB) -- Central Zone, Komarnica Canyon (II Zone). , Inner Dinarides Zone, Lim and Ibar Catchments (III Zone) -- Mineral Water Springs Near the Town of Ro017Eaje, Catchment Area of the Ibar River -- 0110uranovi0107a Luka Spring -- Bogajski Potok Spring -- Mineral Springs Near the Town of Bijelo Polje in the Catchment Area of the Lim River -- 010Ceo010De Spring -- Nedakusi-0160ljepa0161nici Springs -- Other Cold Carbonated Mineral Water Springs Near Bijelo Polje in the Catchment Area of the Lim River -- References -- 5 Mineral and Thermal Waters of Serbia: Multivariate Statistical Approach to Hydrochemical Characterization -- Abstract -- Introduction -- Methods -- Field and Laboratory Measurements -- Statistical Analysis -- Results and Discussion -- General Characterisation of Mineral and Thermal Waters of Serbia -- Hierarchical Cluster Analysis -- Hydrogeochemical Characterization of Clusters -- C1---Low Mineralized Water -- C2---Cold Waters with Elevated TDS -- C3---Thermal Na--HCO3 Waters -- C4---CO2 Rich Mineral Waters -- C5---Thermal Alkaline Waters -- C6---Thermo-mineral Waters -- Conclusions -- Acknowledgments -- References -- 6 Mineral and Thermal Waters of Romania -- Abstract -- Brief Historical Overview -- Mineral Water Resources---Characteristics and Utilization -- Thermal Water Resources---Characteristics and Utilization -- Relevant Legislation -- References -- 7 Thermal Waters of Albania -- Abstract -- Introduction -- Geological Setting of the Albanides -- Geothermal Regime -- Thermal Water Provinces -- Geothermometry -- Conclusions -- References -- 8 Geothermal Potential of Macedonia and Its Utilization -- Abstract -- Introduction -- Known Thermal Water Resources in Macedonia -- Thermal Resources in Use -- Kocani Geothermal Project -- Istibanja Geothermal Project -- Bansko Geothermal Project -- Smokvica Geothermal Project -- Other Projects -- Thermal Spas in Macedonia. , Overview of Other Unexplored and Unexploited Geothermal Resources -- Conclusions -- References -- 9 Mineral, Thermal and Thermomineral Waters of Bosnia and Herzegovina -- Abstract -- Introduction -- Geological Background and Hydrogeological Structures -- Basic Hydrogeological Characteristics of Waters -- Mineral Waters -- Thermal Waters -- Thermomineral Waters -- Physical and Chemical Features of Waters -- Genetic Characteristics of Waters -- Status and Results of Investigations -- Utilization of Waters -- Conclusion -- Acknowledgments -- References.
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  • 2
    Online Resource
    Online Resource
    Mineral and Thermal Waters of Southeastern Europe (2016)
    Cham : Springer International Publishing
    Details Availability
    Keywords: Earth sciences ; Earth Sciences ; Hydrogeology ; Earth sciences ; Hydrogeology ; Südosteuropa ; Mineralquelle ; Thermalwasser ; Hydrogeochemie ; Albanien ; Bosnien-Herzegowina ; Bulgarien ; Kroatien ; Nordmazedonien ; Mineralwasser ; Montenegro ; Rumänien ; Thermalquelle ; Balneologie ; Tiefenwasser ; Heilquelle ; Südosteuropa ; Mineralquelle ; Thermalwasser ; Hydrogeochemie ; Albanien ; Bosnien-Herzegowina ; Bulgarien ; Kroatien ; Nordmazedonien ; Mineralwasser ; Montenegro ; Rumänien ; Thermalquelle ; Balneologie ; Tiefenwasser ; Heilquelle
    Description / Table of Contents: Geology of South-Eastern Europe -- Mineral and Thermal Waters in the Croatian Part of the Pannonian Basin -- Thermal waters in Bulgaria -- Mineral waters of Montenegro -- Mineral and thermal waters of Serbia: multivariate statistical approach to hydrochemical characterization…- Mineral and Thermal Waters of Romania -- Thermal waters of Albania -- Geothermal potential of Macedonia and its utilization -- Mineral, Thermal and Thermomineral Waters of Bosnia and Herzegovina. /* Style Definitions */ table.MsoNormalTable {mso-style-name:"Table Normal"; mso-tstyle-rowband-size:0; mso-tstyle-colband-size:0; mso-style-noshow:yes; mso-style-priority:99; mso-style-qformat:yes; mso-style-parent:""; mso-padding-alt:0in 5.4pt 0in 5.4pt; mso-para-margin-top:0in; mso-para-margin-right:0in; mso-para-margin-bottom:10.0pt; mso-para-margin-left:0in; line-height:115%; mso-pagination:widow-orphan; font-size:11.0pt; font-family:"Calibri","sans-serif"; mso-ascii-font-family:Calibri; mso-ascii-theme-font:minor-latin; mso-fareast-font-family:"Times New Roman"; mso-fareast-theme-font:minor-fareast; mso-hansi-font-family:Calibri; mso-hansi-theme-font:minor-latin; mso-bidi-font-family:"Times New Roman"; mso-bidi-theme-font:minor-bidi;}.
    Type of Medium: Online Resource
    Pages: Online-Ressource (VII, 171 p. 44 illus., 11 illus. in color, online resource)
    Edition: 1st ed. 2016
    ISBN: 9783319253794
    Series Statement: Environmental Earth Sciences
    URL: https://doi.org/10.1007/978-3-319-25379-4
    URL: http://dx.doi.org/10.1007/978-3-319-25379-4
    URL: https://swbplus.bsz-bw.de/bsz455197245cov.jpg
    DOI: 10.1007/978-3-319-25379-4
    Language: English
    Note: Geology of South-Eastern EuropeMineral and Thermal Waters in the Croatian Part of the Pannonian Basin -- Thermal waters in Bulgaria -- Mineral waters of Montenegro -- Mineral and thermal waters of Serbia: multivariate statistical approach to hydrochemical characterization…- Mineral and Thermal Waters of Romania -- Thermal waters of Albania -- Geothermal potential of Macedonia and its utilization -- Mineral, Thermal and Thermomineral Waters of Bosnia and Herzegovina. /* Style Definitions */ table.MsoNormalTable {mso-style-name:"Table Normal"; mso-tstyle-rowband-size:0; mso-tstyle-colband-size:0; mso-style-noshow:yes; mso-style-priority:99; mso-style-qformat:yes; mso-style-parent:""; mso-padding-alt:0in 5.4pt 0in 5.4pt; mso-para-margin-top:0in; mso-para-margin-right:0in; mso-para-margin-bottom:10.0pt; mso-para-margin-left:0in; line-height:115%; mso-pagination:widow-orphan; font-size:11.0pt; font-family:"Calibri","sans-serif"; mso-ascii-font-family:Calibri; mso-ascii-theme-font:minor-latin; mso-fareast-font-family:"Times New Roman"; mso-fareast-theme-font:minor-fareast; mso-hansi-font-family:Calibri; mso-hansi-theme-font:minor-latin; mso-bidi-font-family:"Times New Roman"; mso-bidi-theme-font:minor-bidi;}.
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  • 3
    Electronic Resource
    Electronic Resource
    Elements of groundwater protection in a karst environment (1992)
    Springer
    Environmental geology 20 (1992), S. 157-164 
    Details
    ISSN: 1432-0495
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The large spread of karst in Yugoslavia (over one third of the territory) and the importance of its water resources due to the growing pollution of the environment lead to complicated research activities in various scientific fields. A multidisciplinary approach to this research should have the following basic directions: defining sources of pollution; classification of pollutants; defining hydrological, geological, and hydrogeological characteristics of the area studied; study of interaction among pollutants, groundwater, and rocks; and, finally, defining of specific protection measures. The prerequisite for any decision making should already exist in local and regional urban plans. Some basic principles of the listed directions of research are illustrated by examples from practice.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01706159
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  • 4
    Electronic Resource
    Electronic Resource
    Specific chemical composition of karst groundwater in the Ophiolite Belt of the Yugoslav Inner Dinarides: A case for covered karst (1990)
    Springer
    Environmental geology 15 (1990), S. 131-135 
    Details
    ISSN: 1432-0495
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Ophiolite Belt of the Yugoslav Inner Dinarides, for its very complicated tectonic fabric, according to the existing geological theories was considered to be a chaotic melange of the olistostrome type. Its parts of Triassic limestone were understood as thin slide sheets over ophiolites (diabases, cherts, ultramafics). Complex hydrogeological researches, conducted in the last few years, refuted such theories. They showed that Triassic limestone is much wider spread and is covered with ophiolites of Jurassic age. Results of hydrochemical analysis were among ones of most importance. Established relationships between main chemical components in groundwaters of the area, made concluding about the origin of karst groundwaters, properties of karst aquifers, and influences of ultramafics on them, possible. With typical examples it is shown what conclusions can be made according to content of calcium, magnesium, and silica, their relationships, Ca2+/Mg2+ ratio, and temperature. Results collected during regional studies indicate that recharge of karst aquifers with groundwater from ultramafics can be significant.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01705101
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  • 5
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    Active Degassing of Deeply Sourced Fluids in Central Europe: New Evidences From a Geochemical Study in Serbia (2021)
    Wiley-Agu
    Details
    Publication Date: 2021-12-03
    Description: We report on the results of an extensive geochemical survey of fluids released in the Vardar zone (central-western Serbia), a mega-suture zone at the boundary between Eurasia and Africa plates. Thirty-one bubbling gas samples are investigated for their chemical and isotopic compositions (He, C, Ar) and cluster into three distinct groups (CO2-dominated, N2-dominated, and CH4-dominated) based on the dominant gas species. The measured He isotope ratios range from 0.08 to 1.19 Ra (where Ra is the atmospheric ratio), and reveal for the first time the presence of a minor (〈20%) but detectable regional mantle-derived component in Serbia. δ13C values range from −20.2‰ to −0.1‰ (versus PDB), with the more negative compositions observed in N2-dominated samples. The carbon-helium relationship indicates that these negative δ13C compositions could be due to isotopic fractionation processes during CO2 dissolution into groundwater. In contrast, CO2-rich samples reflect mixing between crustal and mantle-derived CO2. Our estimated mantle-derived He flux (9.0 × 109 atoms m−2 s−1) is up to 2 orders of magnitude higher than the typical fluxes in stable continental areas, suggesting a structural/tectonic setting favoring the migration of deep-mantle fluids through the crust.
    Description: Published
    Description: e2021GC010017
    Description: 9T. Geochimica dei fluidi applicata allo studio e al monitoraggio di aree sismiche
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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