Paleomagnetismus a magnetostratigrafie krasových sedimentů ve Slovinsku

Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F08%3A00308063" target="_blank" >RIV/67985831:_____/08:00308063 - isvavai.cz</a>
Výsledek na webu
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Jazyk výsledku
angličtina
Název v původním jazyce
Palaeomagnetism and magnetostratigraphy of Karst sediments in Slovenia
Popis výsledku v původním jazyce
Intensive palaeomagnetic research in Slovenia has contributed substantially to the understanding of cave sediments in different tectonic and geomorphic settings in the territory. However results suggest that there were probably some distinct phases of masive deposition in caves. The podest one took place from about 1.8 to more than 5.4 ma (with two distinct phases at 1.8-3.6 and about 4.1-5.4 Ma). For the first time in Slovenia, biostratigraphic data helped to correlate magnetostratigraphy logs with theGPTS and to allocate the cave fill agens more precisely to pre-Quaternary times.
Název v anglickém jazyce
Palaeomagnetism and magnetostratigraphy of Karst sediments in Slovenia
Popis výsledku anglicky
Intensive palaeomagnetic research in Slovenia has contributed substantially to the understanding of cave sediments in different tectonic and geomorphic settings in the territory. However results suggest that there were probably some distinct phases of masive deposition in caves. The podest one took place from about 1.8 to more than 5.4 ma (with two distinct phases at 1.8-3.6 and about 4.1-5.4 Ma). For the first time in Slovenia, biostratigraphic data helped to correlate magnetostratigraphy logs with theGPTS and to allocate the cave fill agens more precisely to pre-Quaternary times.

Rok uplatnění
2008
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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