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      <comment>Eötv̈os Loránd Geophysical Institute of Hungary, Palaeomagnetic Laboratory, H-1145 Budapest, Columbus ut. 17-23, Hungary            
            Geological Institute of the Slovak Academy of Sciences, 840 05 Bratislava 45, Dúbravská cesta 9, Slovakia            
            Geophysical Institute of the Slovak Academy of Sciences, 845 28 Bratislava, Dúbravská cesta 9, Slovakia            
            Eötvös Loránd University, Geophysics Department, H-1117 Budapest, Pazmany Peter setany 1/c, Hungary            
            University of Miskolc, Department of Geology, H-3515 Miskolc, Egyetemváros, Hungary            
            831 03 Bratislava, Matičná 5, Slovakia            
            Export Date: 16 April 2025; Cited By: 11; Correspondence Address: E. Márton; Eötvös Loránd Geophysical Institute of Hungary, Palaeomagnetic Laboratory, H-1145 Budapest, Columbus ut. 17-23, Hungary; email: paleo@elgi.hu</comment>
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      <abstractText>On geological grounds, the ignimbrites/tuffs of the Ipolytarnóc area were regarded as belonging to the oldest of the three Miocene “tuff complexes” of the Pannonian Basin. From the paleomagnetic point of view, the three complexes are significantly different in the area which comprises North Hungary and South Slovakia, since the oldest is characterized by about 80º, the middle by about 30º counterclockwise, while the youngest about 10º clockwise rotation with respect to the present North. The significant differences in declinations are attributed to block rotations, which affected the area in the time intervals of 18.5–17.5 Ma and 16–14.5 Ma. Earlier, a pilot study on three ignimbrite sites from Ipolytarnóc indicated only 30º of counterclockwise rotation, which suggested that the volcanism was younger than assumed, while the underlying Eggenburgian sediments showed the expected large rotation. Following up indications, we carried out a detailed paleomagnetic study at this locality on a large number of samples from the terrestrial sequence which covers the Eggenburgian sandstone. These were the “footprint sandstone” and the overlying unaltered, ignimbrites which represent three volcanic cycles separated by clastic sediments. Ignimbrites from the surrounding area were also tested. The results obtained are of high quality, statistically well defined on the site level and are highly consistent on the between-site level. The polarity is normal for the first two cycles and reversed for the youngest. The rotation angle indicated is about 30º. Thus, we conclude that the ignimbrites at the Ipolytarnóc area are indeed younger than 17.5 Ma, so they belong to the “Middle Tuff Complex” of the Pannonian Basin.</abstractText>
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&lt;div class=&quot;lastModified&quot;&gt;Utolsó módosítás: 2020.09.18. 16:00 Szabó Regina (ELTE TTK admin 5)
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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: Eötv̈os Loránd Geophysical Institute of Hungary, Palaeomagnetic Laboratory, H-1145 Budapest, Columbus ut. 17-23, Hungary            
            Geological Institute of the Slovak Academy of Sciences, 840 05 Bratislava 45, Dúbravská cesta 9, Slovakia            
            Geophysical Institute of the Slovak Academy of Sciences, 845 28 Bratislava, Dúbravská cesta 9, Slovakia            
      ...&lt;/pre&gt;
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