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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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ring silicates
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illite (11)
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sulfobismuthites
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tellurides
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tetradymite (2)
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Primary terms
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absolute age (12)
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Africa
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Southern Africa
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Asia
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Far East
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Korea
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Khakasiya Russian Federation (1)
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Israel
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Turkey
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bacteria (4)
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carbon
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Cenozoic
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Quaternary
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upper Pleistocene (1)
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Tertiary
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Neogene
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upper Pliocene
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Paleogene
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Oligocene (1)
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Paleocene (2)
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-
-
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Chordata
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Vertebrata
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Tetrapoda
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Mammalia
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Theria
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Eutheria
-
Rodentia (1)
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Reptilia
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Testudines (1)
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clay mineralogy (17)
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Hungary
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Pieniny Klippen Belt (5)
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Southern Europe
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Greece (2)
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Galicia Spain (1)
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Italy
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Apennines
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Romania
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hydrology (1)
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igneous rocks
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Slovakia
Inclusions in calcite phantom crystals suggest role of clay minerals in dolomite formation
Argentotetrahedrite-(Zn), Ag 6 (Cu 4 Zn 2 )Sb 4 S 13 , a new member of the tetrahedrite group
Hellandite-(Y)–hingganite-(Y)–fluorapatite retrograde coronae: a novel type of fluid-induced dissolution–reprecipitation breakdown of xenotime-(Y) in the metagranites of Fabova Hoľa, Western Carpathians, Slovakia
Destruction of the Royal Town at Visegrád, Hungary: Historical Evidence and Archaeoseismology of the A.D. 1541 Earthquake at the Proposed Danube Dam Site
Characterization of the metasomatizing agent in the upper mantle beneath the northern Pannonian Basin based on Raman imaging, FIB-SEM, and LA-ICP-MS analyses of silicate melt inclusions in spinel peridotite
Incorporation mechanism of tungsten in W-Fe-Cr-V-bearing rutile
The Last Glacial and Holocene history of mountain woodlands in the southern part of the Western Carpathians, with emphasis on the spread of Fagus sylvatica
Carbonate-bearing phosphohedyphane–“Hydroxylphosphohedyphane” and cerussite: Supergene products of galena alteration in Permian aplite (Western Carpathians, Slovakia)
Fluorapophyllite-(NH 4 ), NH 4 Ca 4 (Si 8 O 20 )F⋅8H 2 O, a new member of the apophyllite group from the Vechec quarry, eastern Slovakia
Non-condensed shell beds in hiatal successions: instantaneous cementation associated with nutrient-rich bottom currents and high bivalve production
Paleomagnetic and magnetic fabric data from Lower Triassic redbeds of the Central Western Carpathians: new constraints on the paleogeographic and tectonic evolution of the Carpathian region
Gold ± Copper Endowment and Deposit Diversity in the Western Tethyan Magmatic Belt, Southeast Europe: Implications for Exploration
A case study for identification of organic–silt bottom sediments in an artificial lake formed in gravel alluvium in the geotourism locality of Slnečné Jazerá in Senec (Bratislava, Slovakia)
Petrogenesis of a Large-Scale Miocene Zeolite Tuff in the Eastern Slovak Republic: The Nižný Hrabovec Open-Pit Clinoptilolite Mine
A Local Magnitude Scale for Slovakia, Central Europe
Vanadian and chromian garnet- and epidote-supergroup minerals in metamorphosed Paleozoic black shales from Čierna Lehota, Strážovské vrchy Mountains, Slovakia: crystal chemistry and evolution
Depth estimation from downward continuation: An entropy-based approach to normalized full gradient
Fluorarrojadite-(BaNa), BaNa 4 CaFe 13 Al(PO 4 ) 11 (PO 3 OH)F 2 , a new member of the arrojadite group from Gemerská Poloma, Slovakia
Vulnerability assessment and its validation: the Gömör-Torna Karst, Hungary and Slovakia
Abstract Reliability is the greatest concern in recent karst vulnerability assessments. Checking the validity of results and understanding the operation of karst systems are therefore the most promising areas for improvement. We report an application of the Slovene Approach to a test site in the Gömör-Torna Karst of Hungary and Slovakia. The resource vulnerability map provided an appropriate result and showed that the overlying sediments and thicker soil may effectively decrease the vulnerability of this unconfined area. The source vulnerability of the Kis-Tohonya Spring was evaluated for the purposes of protection zoning. The results of long-term hydrograph and recession curve analyses were helpful in understanding the functioning of the Kis-Tohonya Spring and the karst system. The importance of the different regimes contributing to the slow and fast flow of the spring under different hydrological conditions was shown. Ongoing research aims to feed these results back into the source vulnerability assessment of the spring.