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      <abstractText>Nagy felbontású rétegtani tagolás és ezt megalapozó mélyfúrás geofizikai adatrendszer hiányában a Duna–Tisza-köze területére vonatkozó vízföldtani modellezések kényszerűen egyszerű földtani alapra épülnek. A tanulmányban 593 közelmúltban digitalizált mélyfúrás karotázs korrelációjára alapozva mutatjuk be a térség negyedidőszaki rétegsorát. Az üledékföldtani egységek korát a terület magfúrásainak mágneses szuszceptibilitás adatokra épülő, közelmúltban publikált rétegtani beosztására alapozva adtuk meg. A negyedidőszaki rétegsor alapvető tagolására a pleisztocén közepi klímaromlás (Mid Pleistocene Transition) idejének (1,2 millió év) megfelelő korrelációs felszín szolgált („MPT felület”). Alatta döntően egyveretű homok sorozatokból álló rétegsor települ, fölötte finomszemű üledékek közé ágyazott kis vastagságú homokrétegek összességében fölfelé durvuló sorozata látható. Előbbit nagy méretű, intenzív oldalazó eróziót kifejtő vagy elágazó vízfolyás hozhatta létre, utóbbi kisméretű vízfolyások által épített hordalékkúp jelenlétére utalhat. Elkülöníthető egy a hordalékkúppal laterálisan érintkező, a mai Duna-völggyel párhuzamos, attól K-re eső, ártéri üledékeket csak alárendelten tartalmazó homok összlet is, melynek kora 450–250 ezer év közé tehető, s amely ismét nagyméretű vízfolyás (Duna) jelenlétét igazolja. A mágneses szuszceptibilitás és fauna adatok figyelembevételével az MPT felület alatti folyóvízi rétegsor további három egységre, a hordalékkúp összlet ugyancsak három kisebb, egyenként fölfelé durvuló üledékciklusra tagolható. Az utóbbiak bázisa fölött települő finomszemű képződmények felszín közeli regionális vagy lokális vízrekesztők lehetnek. A térképezett rétegtani egységek száma a korábbi 1–3-ról 8-ra, a térképezés alapjául szolgáló értékelt mélyfúrások száma a korábbi 66-ról (Urbancsek 1977) 593-ra emelkedett, ami a földtani modell felbontásában nagyságrendi növekedés. A bemutatott korrelációk területi kiterjesztésének és a megbízható rétegtani tagolás következetes alkalmazásának eszköze lehet a mágneses szuszceptibilitás – mint paleoklíma változások kimutatására alkalmas fizikai mennyiség – számításba vétele a vízkutató fúrások mélyfúrási geofizikai vizsgálatának tervezésekor.</abstractText>
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&lt;span class=&quot;author-name&quot; mtid=&quot;10075659&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10075659&quot; target=&quot;_blank&quot;&gt;Mekker Julianna (&lt;span class=&quot;authorship-author-name&quot;&gt;Mekker Julianna&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; hidrogeológia&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; mtid=&quot;10064936&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10064936&quot; target=&quot;_blank&quot;&gt;Szabó Zsóka (&lt;span class=&quot;authorship-author-name&quot;&gt;Szabó Zsóka&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; Hidrogeológia&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; mtid=&quot;10038191&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10038191&quot; target=&quot;_blank&quot;&gt;Bauer Márton (&lt;span class=&quot;authorship-author-name&quot;&gt;Bauer Márton&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; Földtudományok&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; mtid=&quot;10054128&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10054128&quot; target=&quot;_blank&quot;&gt;Gál Nóra Edit (&lt;span class=&quot;authorship-author-name&quot;&gt;Gál Nóra Edit&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; geológia, hidrogeológia&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; mtid=&quot;10053965&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10053965&quot; target=&quot;_blank&quot;&gt;Kun Éva (&lt;span class=&quot;authorship-author-name&quot;&gt;Kun Éva&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; földtudomány&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; mtid=&quot;10060214&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10060214&quot; target=&quot;_blank&quot;&gt;Szűcs Andrea (&lt;span class=&quot;authorship-author-name&quot;&gt;Szűcs Andrea&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; geológia, vízgeokémia, környezetgeológia&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; mtid=&quot;10053425&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10053425&quot; target=&quot;_blank&quot;&gt;Szőcs Teodóra (&lt;span class=&quot;authorship-author-name&quot;&gt;Szőcs Teodóra&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; Hidrogeológia&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; mtid=&quot;10009915&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10009915&quot; target=&quot;_blank&quot;&gt;Fancsik Tamás (&lt;span class=&quot;authorship-author-name&quot;&gt;Fancsik Tamás&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; Geofizika&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; mtid=&quot;10043232&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10043232&quot; target=&quot;_blank&quot;&gt;Püspöki Zoltán (&lt;span class=&quot;authorship-author-name&quot;&gt;Püspöki Zoltán&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; Földtan&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; &lt;/div&gt; &lt;/div&gt; &lt;div class=&quot;title&quot;&gt;&lt;a href=&quot;/gui2/?mode=browse&amp;params=publication;35621710&quot; target=&quot;_blank&quot;&gt;A Duna–Tisza-köze negyedidőszaki képződményei mágneses szuszceptibilitás és karotázs korrelációs vizsgálatok alapján&lt;/a&gt;&lt;/div&gt; &lt;div&gt; &lt;span class=&quot;journal-title&quot;&gt;HIDROLÓGIAI KÖZLÖNY&lt;/span&gt; &lt;span class=&quot;journal-issn&quot;&gt;(&lt;a target=&quot;_blank&quot; href=&quot;https://portal.issn.org/resource/ISSN/0018-1323&quot;&gt;0018-1323&lt;/a&gt; &lt;a target=&quot;_blank&quot; href=&quot;https://portal.issn.org/resource/ISSN/2939-8495&quot;&gt;2939-8495&lt;/a&gt;)&lt;/span&gt;: &lt;span class=&quot;journal-volume&quot;&gt;104&lt;/span&gt; &lt;span class=&quot;journal-issue&quot;&gt;4&lt;/span&gt; &lt;span class=&quot;page&quot;&gt; pp 43-62 &lt;/span&gt; &lt;span class=&quot;year&quot;&gt;(2024)&lt;/span&gt; &lt;/div&gt; &lt;div class=&quot;pub-footer&quot;&gt; &lt;span class=&quot;language&quot; xmlns=&quot;http://www.w3.org/1999/html&quot;&gt;Nyelv: Magyar | &lt;/span&gt; &lt;span class=&quot;identifiers&quot;&gt; &lt;span class=&quot;id identifier oa_GOLD&quot; title=&quot; Gold &quot;&gt; &lt;a style=&quot;color:blue&quot; title=&quot;10.59258/hk.17594&quot; target=&quot;_blank&quot; href=&quot;https://doi.org/10.59258/hk.17594&quot;&gt; DOI &lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;id identifier oa_GREEN&quot; title=&quot; Green &quot;&gt; &lt;a style=&quot;color:blue&quot; title=&quot;225517&quot; target=&quot;_blank&quot; href=&quot;https://real.mtak.hu/225517&quot;&gt; REAL &lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;id identifier oa_none&quot; title=&quot;none&quot;&gt; &lt;a style=&quot;color:blue&quot; title=&quot;397954&quot; target=&quot;_blank&quot; href=&quot;http://hdl.handle.net/2437/397954&quot;&gt; DEA &lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;id identifier oa_none&quot; title=&quot;none&quot;&gt; &lt;a style=&quot;color:blue&quot; title=&quot;https://www.webofscience.com/wos/rc/full-record/RC:152969245_S24&quot; target=&quot;_blank&quot; href=&quot;https://www.webofscience.com/wos/rc/full-record/RC:152969245_S24&quot;&gt; Egyéb URL &lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;id identifier oa_none&quot; title=&quot;none&quot;&gt; &lt;a style=&quot;color:blue&quot; title=&quot;13286752300127577094&quot; target=&quot;_blank&quot; href=&quot;http://scholar.Google.com/scholar?hl=en&amp;lr=&amp;cluster=13286752300127577094&quot;&gt; Google scholar &lt;/a&gt; &lt;/span&gt; &lt;/span&gt; &lt;OnlyViewableByAuthor&gt;&lt;div class=&quot;ratings&quot;&gt; &lt;div class=&quot;journal-subject&quot;&gt;IV. Agrártudományok Osztálya IVAO&amp;nbsp;&amp;nbsp;&amp;nbsp;A&lt;/div&gt; &lt;div class=&quot;journal-subject&quot;&gt;X. Földtudományok Osztálya XFO&amp;nbsp;&amp;nbsp;&amp;nbsp;A&lt;/div&gt; &lt;/div&gt;&lt;/OnlyViewableByAuthor&gt; &lt;div class=&quot;publication-citation&quot;&gt; &lt;a target=&quot;_blank&quot; href=&quot;/api/publication?cond=citations.related;eq;35621710&amp;sort=publishedYear,desc&amp;sort=title&quot;&gt; Idézett közlemények száma: 13 &lt;/a&gt; &lt;/div&gt; &lt;div class=&quot;mtid&quot;&gt;&lt;span class=&quot;long-pub-mtid&quot;&gt;Közlemény: 35621710&lt;/span&gt; | &lt;span class=&quot;status-data status-VALIDATED&quot;&gt; Egyeztetett &lt;/span&gt; Forrás Idéző | &lt;span class=&quot;type-subtype&quot;&gt;Folyóiratcikk ( Szakcikk ) &lt;/span&gt; | &lt;span class=&quot;pub-category&quot;&gt;Tudományos&lt;/span&gt; | &lt;span class=&quot;publication-sourceOfData&quot;&gt;kézi felvitel&lt;/span&gt; &lt;/div&gt; &lt;div class=&quot;special-affiliations&quot;&gt; Speciális affiliáció: Hidrológiai Közlöny szerkesztősége &lt;/div&gt; &lt;div class=&quot;lastModified&quot;&gt;Utolsó módosítás: 2026.10.07. 08:41 Kovács Marcell (MTMT Közp., admin) &lt;/div&gt; &lt;/div&gt;&lt;/div&gt;</template2>
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