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      <title>Tracing the transition from hypogene to epigene karstification in the Villány Thermal Karst area, Hungary: Linking submicron-scale cave processes with regional groundwater flow system dynamics</title>
      <altTitles>Localisation de la transition entre karstification hypogène et épigène dans la région karstique thermale de Villány, Hongrie : relation entre les processus à l’échelle submicronique en cavité et la dynamique régionale du système d’écoulement des eaux souterraines;Seguimiento de la transición de la karstificación hipógena a la epigénica en la zona kárstica termal de Villány, Hungría: Vinculación de los procesos cavernarios a escala submicrónica con la dinámica del sistema regional de flujo de aguas subterráneas;追踪匈牙利Villány热岩溶区从深成岩溶到表生岩溶的转变:将亚微米尺度洞穴过程与区域地下水流系统动态联系起来;Rastreando a transição da carstificação hipogênica para epigênica na área do Carste Termal de Villány, Hungria: vinculando processos de cavernas em escala submicrométrica com a dinâmica do sistema regional de fluxo de águas subterrâneas;</altTitles>
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      <abstractText>The geological conditions of the Villány Thermal Karst (VTK) area in southwestern Hungary provide an excellent opportunity for hydrogeological research on hypogene cave formation along the boundaries between the unconfined and adjacent confined carbonate regions. The aim of this study was to investigate the hypogene caves of the VTK area from a hydrogeological perspective to identify the effects of waters flowing upward and downward and the related speleothems. Special attention was paid to evaluating the current hydrogeological conditions and their potential for cave formation. Therefore, an in situ experiment was conducted in the largest cave situated at the karst water table. Based on these results, the karst development of the area was reconstructed, integrating the results of the regional groundwater flow system evaluation with the geological evolution history. The results showed that all the caves of the VTK region show the effects of upwelling thermal waters. However, features directly related to the infiltration of precipitation are also abundant. During the in situ experiment, microscale dissolution and significant carbonate precipitation were observed in the cave, primarily near the water table, indicating that active cave formation is not currently occurring. The development of the hypogene caves in the area was initiated by the inversion of the Pannonian Basin, during which compression-driven overpressured fluids could have interacted with the topography-driven flow systems recharged through the exhumed surfaces. However, the topography-driven flow systems have recently overwhelmed the overpressured system, and karst development is now governed by epigene processes.</abstractText>
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          <label>65. Vigassy T, Leél-Őssy S, Demény A (2010) A Nagyharsányi-és a Beremendi-kristálybarlang és képződményeik genetikai vizsgálata (The crystal caves of Nagyharsány and Beremend, and genetic investigation of their precipitations). Földtani Közlöny 140(1):73–88</label>
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      <link>/api/publication/36199088</link>
      <label>Hegedűs-Csondor Katalin et al. Tracing the transition from hypogene to epigene karstification in the Villány Thermal Karst area, Hungary: Linking submicron-scale cave processes with regional groundwater flow system dynamics. (2025) HYDROGEOLOGY JOURNAL 1431-2174 1435-0157 33 4 1109-1131</label><template>&lt;div class=&quot;JournalArticle Publication short-list&quot;&gt; &lt;div class=&quot;authors&quot;&gt; &lt;span class=&quot;author-name&quot; mtid=&quot;10054824&quot;&gt; &lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10054824&quot; target=&quot;_blank&quot;&gt;Hegedűs-Csondor, Katalin&lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-type&quot;&gt; &lt;/span&gt; ; &lt;span class=&quot;author-name&quot; mtid=&quot;10013960&quot;&gt; &lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10013960&quot; target=&quot;_blank&quot;&gt;Sebe, Krisztina&lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-type&quot;&gt; &lt;/span&gt; ; &lt;span class=&quot;author-name&quot; mtid=&quot;10055756&quot;&gt; &lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10055756&quot; target=&quot;_blank&quot;&gt;Molnár, Zsombor&lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-type&quot;&gt; &lt;/span&gt; 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mtid=&quot;36199088&quot; target=&quot;_blank&quot;&gt;Tracing the transition from hypogene to epigene karstification in the Villány Thermal Karst area, Hungary: Linking submicron-scale cave processes with regional groundwater flow system dynamics&lt;/a&gt;&lt;/div&gt; &lt;div class=&quot;pub-info&quot;&gt; &lt;span class=&quot;journal-title&quot;&gt;HYDROGEOLOGY JOURNAL&lt;/span&gt; &lt;span class=&quot;journal-volume&quot;&gt;33&lt;/span&gt; : &lt;span class=&quot;journal-issue&quot;&gt;4&lt;/span&gt; &lt;span class=&quot;page&quot;&gt; pp. 1109-1131. , 23 p. &lt;/span&gt; &lt;span class=&quot;year&quot;&gt;(2025)&lt;/span&gt; &lt;/div&gt; &lt;div class=&quot;pub-end&quot;&gt;&lt;div class=&quot;identifier-list&quot;&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;10.1007/s10040-025-02911-5&quot; target=&quot;_blank&quot; href=&quot;https://doi.org/10.1007/s10040-025-02911-5&quot;&gt; 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src=&quot;/frontend/resources/grid/publication-core-icon.png&quot;&gt; &lt;img title=&quot;Idézőközlemény&quot; style=&quot;float: left&quot; src=&quot;/frontend/resources/grid/publication-citation-icon.png&quot;&gt; &lt;div class=&quot;autype autype0&quot;&gt; &lt;span class=&quot;author-name&quot; mtid=&quot;10054824&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10054824&quot; target=&quot;_blank&quot;&gt;Hegedűs-Csondor Katalin (&lt;span class=&quot;authorship-author-name&quot;&gt;Hegedűs-Csondor Katalin&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; Hidrogeológia&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-affil&quot;&gt;&lt;span title=&quot;Eötvös Loránd Tudományegyetem&quot;&gt;ELTE&lt;/span&gt;/&lt;span title=&quot;Természettudományi Kar&quot;&gt;TTK&lt;/span&gt;/&lt;span title=&quot;Földrajz- és Földtudományi Intézet&quot;&gt;FoldrFoldt_I&lt;/span&gt;/&lt;span title=&quot;Földtudományi Központ&quot;&gt;Ft_K&lt;/span&gt;/Általános és Alkalmazott Földtani Tanszék&lt;/span&gt; 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&lt;span class=&quot;authorAux-mtmt&quot;&gt; Geológia&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-affil&quot;&gt;&lt;span title=&quot;Pannon Egyetem&quot;&gt;PE&lt;/span&gt;/&lt;span title=&quot;Mérnöki Kar&quot;&gt;MK&lt;/span&gt;/&lt;span title=&quot;Bio-nanotechnológiai és Műszaki Kémiai Kutatóintézet&quot;&gt;BNTMUKKI&lt;/span&gt;/HUN-REN-PE Környezeti Ásványtan Kutatócsoport; &lt;span title=&quot;Pannon Egyetem&quot;&gt;PE&lt;/span&gt;/&lt;span title=&quot;Mérnöki Kar&quot;&gt;MK&lt;/span&gt;/&lt;span title=&quot;Bio-nanotechnológiai és Műszaki Kémiai Kutatóintézet&quot;&gt;BNTMUKKI&lt;/span&gt;/Környezeti Ásványtan Kutatócsoport&lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; mtid=&quot;10016893&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10016893&quot; target=&quot;_blank&quot;&gt;Dezső József (&lt;span class=&quot;authorship-author-name&quot;&gt;Dezső József&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; 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target=&quot;_blank&quot;&gt;Tracing the transition from hypogene to epigene karstification in the Villány Thermal Karst area, Hungary: Linking submicron-scale cave processes with regional groundwater flow system dynamics&lt;/a&gt;&lt;/div&gt; &lt;div&gt; &lt;span class=&quot;journal-title&quot;&gt;HYDROGEOLOGY JOURNAL&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/1431-2174&quot;&gt;1431-2174&lt;/a&gt; &lt;a target=&quot;_blank&quot; href=&quot;https://portal.issn.org/resource/ISSN/1435-0157&quot;&gt;1435-0157&lt;/a&gt;)&lt;/span&gt;: &lt;span class=&quot;journal-volume&quot;&gt;33&lt;/span&gt; &lt;span class=&quot;journal-issue&quot;&gt;4&lt;/span&gt; &lt;span class=&quot;page&quot;&gt; pp 1109-1131 &lt;/span&gt; &lt;span class=&quot;year&quot;&gt;(2025)&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: Angol | &lt;/span&gt; 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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;36199088&amp;sort=publishedYear,desc&amp;sort=title&quot;&gt; Idézett közlemények száma: 29 &lt;/a&gt; &lt;/div&gt; &lt;div class=&quot;mtid&quot;&gt;&lt;span class=&quot;long-pub-mtid&quot;&gt;Közlemény: 36199088&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;DOI XML&lt;/span&gt; &lt;/div&gt; &lt;div class=&quot;funder&quot;&gt; A Villányi-termálkarszt komplex hidraulikai és geokémiai feldolgozása(116227) Támogató: NKFIH, European Union’s Horizon 2020 Research and Innovation Programme(810980), ÉMNL(RRF-2.3.1-21-2022-00014) Támogató: NKFIH &lt;/div&gt; &lt;div class=&quot;lastModified&quot;&gt;Utolsó módosítás: 2026.02.25. 15:50 Balázs András (MTMT Központ, admin) &lt;/div&gt; &lt;div class=&quot;lockedBy&quot;&gt;Központi kezelésű 2026.01.27. 20:11 Vasvari Lilian (MTMT Központ, admin) &lt;/div&gt; &lt;/div&gt;&lt;/div&gt;</template2>
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