Add to ORKGABSTRACT. Lacustrine carbonate deposition in Hungary has been traditionally interpreted as the outcome of the dry, ho
Holocene limnic deposits characteristic of the average latitudes have partially outcropped as a resu...
The 10m thick Madaras loess–palaeosol profile is one of the Hungarian outcrops that yielded Upper Pa...
Limnosilicites constitute a specific group of siliceous rocks originating in freshwater limnic (lake...
From the 19th International Radiocarbon Conference held in Keble College, Oxford, England, April 3-7...
Freshwater carbonates are unique depositions in the centre of the Carpathian Basin, with debated ori...
The first radiocarbon dates available on the evolution of the freshwater carbonates of the Danube-Ti...
The geochemical analyses of karst springs and their freshwater carbonate deposits provide an opport...
One of Hungary's geological and environmental treasures is nestled in the heart of the Great Hungari...
Lacustrine chalk is very common in post-glacial lakes of northern Poland. In the deposit of Lake Kru...
The Petény Cave located on the Hungarian Highlands yielded one of the most well-documented vertebrat...
International audienceBoth the mineralogy and facies of lacustrine bio-induced carbonates are contro...
Cryogenically formed carbonate particles represent a rather new class of speleothems whose origin is...
Abstract In this paper we present sedimentological and geochemical data for a section of fluvial de...
International audienceThe Lake Afourgagh sediment record and facies successions provide an outstandi...
The Dachstein platform was an extensive carbonate platform developed on the westernmost shelf of the...
Holocene limnic deposits characteristic of the average latitudes have partially outcropped as a resu...
The 10m thick Madaras loess–palaeosol profile is one of the Hungarian outcrops that yielded Upper Pa...
Limnosilicites constitute a specific group of siliceous rocks originating in freshwater limnic (lake...
From the 19th International Radiocarbon Conference held in Keble College, Oxford, England, April 3-7...
Freshwater carbonates are unique depositions in the centre of the Carpathian Basin, with debated ori...
The first radiocarbon dates available on the evolution of the freshwater carbonates of the Danube-Ti...
The geochemical analyses of karst springs and their freshwater carbonate deposits provide an opport...
One of Hungary's geological and environmental treasures is nestled in the heart of the Great Hungari...
Lacustrine chalk is very common in post-glacial lakes of northern Poland. In the deposit of Lake Kru...
The Petény Cave located on the Hungarian Highlands yielded one of the most well-documented vertebrat...
International audienceBoth the mineralogy and facies of lacustrine bio-induced carbonates are contro...
Cryogenically formed carbonate particles represent a rather new class of speleothems whose origin is...
Abstract In this paper we present sedimentological and geochemical data for a section of fluvial de...
International audienceThe Lake Afourgagh sediment record and facies successions provide an outstandi...
The Dachstein platform was an extensive carbonate platform developed on the westernmost shelf of the...
Holocene limnic deposits characteristic of the average latitudes have partially outcropped as a resu...
The 10m thick Madaras loess–palaeosol profile is one of the Hungarian outcrops that yielded Upper Pa...
Limnosilicites constitute a specific group of siliceous rocks originating in freshwater limnic (lake...