Ágnes Novothny
Dados Biográficos
| ID | 4131675 |
|---|---|
| NOME | Ágnes Novothny |
| PRENOMES | Ágnes |
| SOBRENOME | Novothny |
| ASSINATURA | NOVOTHNY Á |
| AFILIAÇÕES | Eötvös Loránd University |
| ORCID | 0000-0003-3513-0406 |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 11 |
| TOTAL DE CITAÇÕES | 0 |
| TOTAL COMO AUTOR | 11 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 2002 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2025 |
| ÍNDICE H | 0 |
The preservation potential of loess in low-elevation mountains (Mecsek Mountains, Hungary)
Loess–paleosol outcrops were logged and dated to trace loess cover during the Pleistocene in a low-elevation mountainous area. The exposed successions were a maximum of 15 m thick and stratigraphically fragmentary. Still, results suggest that loess was deposited in all climatically suitable periods within the limits of the dating methods (ca. 400 ka), and probably also beyond this. Luminescence measurements provided numerical ages from ca. 18 ka …
Unravelling pedogenic processes at Basaharc Loess profile in Hungary
Investigation of spectral properties of different Quaternary paleosols and parent materials
Diffuse Reflectance Spectroscopy (DRS) is a rapid, relatively new method in Quaternary research to analyse sediments and paleosols. This method takes into account clay mineral content, amount of Fe-bearing minerals and grain size composition of samples, simultaneously. Different Quaternary sediment samples were chosen forcharacterization and comparison their reflectance curves to detect the essential spectral properties of differentpaleosols and …
A multi-proxy study on polygenetic middle-to late pleistocene paleosols in the Hévízgyörk loess-paleosol sequence (Hungary)
Correlation of drilling cores and the Paks brickyard key section at the area of Paks, Hungary
Dating of a Last Glacial loess sequence by relative geomagnetic palaeointensity
Stable isotope composition of bulk and secondary carbonates from the Quaternary loess-paleosol sequence in Süttő, Hungary
Investigating the penultimate and last glacial cycles of the Süttő loess section (Hungary) using luminescence dating, high-resolution grain size, and magnetic susceptibility data
Luminescence dating of Upper Pleistocene loess from the Island of Susak in Croatia
Luminescence and amino acid racemization chronology of the loess–paleosol sequence at Süttő, Hungary
The loess profile at Albertirsa, Hungary—improvements in loess stratigraphy by luminescence dating
Sem obras proeminentes nesta página.
The loess profile at Albertirsa, Hungary—improvements in loess stratigraphy by luminescence dating
Luminescence and amino acid racemization chronology of the loess–paleosol sequence at Süttő, Hungary
Investigating the penultimate and last glacial cycles of the Süttő loess section (Hungary) using luminescence dating, high-resolution grain size, and magnetic susceptibility data
Luminescence dating of Upper Pleistocene loess from the Island of Susak in Croatia
Dating of a Last Glacial loess sequence by relative geomagnetic palaeointensity
Stable isotope composition of bulk and secondary carbonates from the Quaternary loess-paleosol sequence in Süttő, Hungary
Investigation of spectral properties of different Quaternary paleosols and parent materials
Diffuse Reflectance Spectroscopy (DRS) is a rapid, relatively new method in Quaternary research to analyse sediments and paleosols. This method takes into account clay mineral content, amount of Fe-bearing minerals and grain size composition of samples, simultaneously. Different Quaternary sediment samples were chosen forcharacterization and comparison their reflectance curves to detect the essential spectral properties of differentpaleosols and …
A multi-proxy study on polygenetic middle-to late pleistocene paleosols in the Hévízgyörk loess-paleosol sequence (Hungary)
Correlation of drilling cores and the Paks brickyard key section at the area of Paks, Hungary
The preservation potential of loess in low-elevation mountains (Mecsek Mountains, Hungary)
Loess–paleosol outcrops were logged and dated to trace loess cover during the Pleistocene in a low-elevation mountainous area. The exposed successions were a maximum of 15 m thick and stratigraphically fragmentary. Still, results suggest that loess was deposited in all climatically suitable periods within the limits of the dating methods (ca. 400 ka), and probably also beyond this. Luminescence measurements provided numerical ages from ca. 18 ka …
Unravelling pedogenic processes at Basaharc Loess profile in Hungary
Loess (11 obras) · Paleosol (11 obras) · Geology and Paleoclimatology Research (10 obras) · Geology (9 obras) · Paleontology (9 obras) · Geochemistry (8 obras) · Pleistocene (7 obras) · Marine and environmental studies (6 obras) · Glacial period (5 obras) · Interglacial (5 obras)