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<div class="Book Publication short-list" xmlns="http://www.w3.org/1999/html" xmlns="http://www.w3.org/1999/html"> <div class="authors"> <span class="author-name" mtid="10013847"> <a href="/gui2/?type=authors&mode=browse&sel=10013847" target="_blank">Babinszki, E</a> </span> <span class="author-type"> (eds.) </span> ; <span class="author-name" mtid="10052684"> <a href="/gui2/?type=authors&mode=browse&sel=10052684" target="_blank">Piros, O</a> </span> <span class="author-type"> (eds.) </span> ; <span class="author-name" mtid="10010453"> <a href="/gui2/?type=authors&mode=browse&sel=10010453" target="_blank">Budai, T</a> </span> <span class="author-type"> (eds.) </span> ; <span class="author-name" mtid="10028584"> <a href="/gui2/?type=authors&mode=browse&sel=10028584" target="_blank">Gyalog, L</a> </span> <span class="author-type"> (eds.) </span> ; <span class="author-name" mtid="10016894"> <a href="/gui2/?type=authors&mode=browse&sel=10016894" target="_blank">Halász, A</a> </span> <span class="author-type"> (eds.) </span> ; 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<span class="author-name" >Koroknai B </span> ; <span class="author-name" mtid="10016373"><a href="/gui2/?type=authors&mode=browse&sel=10016373" target="_blank">Lukács R (<span class="authorship-author-name">Haranginé Lukács Réka</span> <span class="authorAux-mtmt"> Geológia, geokémia</span>) </a> </span> <span class="author-affil"><span title="Research Centre for Astronomy and Earth Sciences">CSFK</span>/Institute for Geological and Geochemical Research; <span title="Eötvös Loránd University">ELTE</span>/<span title="Faculty of Science">ELU FoS</span>/<span title="Institute of Geography and Earth Sciences">Inst_GeogrEarthSci</span>/<span title="Center of Earth Sciences">Cntr_EarthSci</span>/MTA-ELTE Volcanology Research Group</span> ; <span class="author-name" mtid="10001322"><a href="/gui2/?type=authors&mode=browse&sel=10001322" target="_blank">M Tóth T (<span class="authorship-author-name">M. Tóth Tivadar</span> <span class="authorAux-mtmt"> Kőzettan</span>) </a> </span> <span class="author-affil"><span title="University of Szeged">SZTE</span>/<span title="Faculty of Science and Informatics">TTIK</span>/<span title="Földrajzi és Földtudományi Intézet">FFI</span>/Department of Mineralogy, Geochemistry and Petrology</span> </div> </div> <div class="title"><a href="/gui2/?mode=browse¶ms=publication;33825476" target="_blank">Magyarország litosztratigráfiai egységeinek leírása I. : Prekainozoos képződmények.</a></div><div class="publish-data"> <span class="published-at"> Bp</span>: <span class="publishers">Supervisory Authority for Regulatory Affairs</span>, <span class="pages">275 p.</span> <span class="year">(2023)</span> </div> <span class="volume"> <span class="volumeTitle"></span> </span> <div class="pub-footer"> <span class="language" xmlns="http://www.w3.org/1999/html">Language: Hungarian | </span> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <span class="isbnOrIssn"> ISBN: </span> <a style="color:blue" title="9789636713287" target="_blank" href="https://www.worldcat.org/search?q=isbn%3A9789636713287"> 9789636713287 </a> </span> <span class="id identifier oa_none" title="none"> <span class="isbnOrIssn"> ISBN: </span> <a style="color:black" title="9789636713263" target="_blank" href="https://www.worldcat.org/search?q=isbn%3A9789636713263"> 9789636713263 </a> </span> <span class="id identifier oa_GOLD" title=" Gold "> <a style="color:blue" title="https://sztfh.hu/downloads/foldtan/prekainozoos_online.pdf" target="_blank" href="https://sztfh.hu/downloads/foldtan/prekainozoos_online.pdf"> Other URL </a> </span> <span class="id identifier oa_GREEN" title=" Green "> <a style="color:blue" title="27396" target="_blank" href="http://publicatio.bibl.u-szeged.hu/27396"> SZTE Publicatio </a> </span> </span> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;33825476&sort=publishedYear,desc&sort=title"> Number of cited publications: 28 </a> </div> <div class="mtid"><span class="long-pub-mtid">Publication: 33825476</span> | <span class="status-data status-VALIDATED"> Validated </span> Core Citing | <span class="type-subtype">Book ( Handbook ) </span> | <span class="pub-category">Scientific</span> | <span class="publication-sourceOfData">kézi felvitel</span> </div> <div class="lastModified">Last Modified: 2024.03.12. 17:06 Csilla Bernátskyné Babus (SZTE admin4) </div> <div class="chapters"> <b><a target="_blank" href="/api/publication?from=BookChapter&cond=book.mtid;eq;33825476">Chapters: 45</a></b> </div> </div></div>
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This work was financially supported by the University of Szeged Open Access Fund (4635), the Bolyai Research Scholarship of the Hungarian Academy of Sciences (BO/266/18), and the National Research, Development, and Innovation Fund (projects no. K 108375 and K 131690).
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The Szeged Basin (S Hungary) occupies a relatively central position within the European Alpine–Carpathian–Dinaride orogenic belt. An ongoing controversy about the tectonic position of the study area indicates that its evolution is still not fully understood; however, several important hydrocarbon occurrences are known in the fractured basement reservoirs. The main aim of this contribution is to investigate the petrographic features and possible Alpine metamorphic conditions of volcanic/volcanoclastic and siliciclastic rocks from the Kelebia basement area. Due to the outcrop conditions and poor exposure, study samples are obtained from cores and core chips resulting from oil exploration. Based on an evaluation of petrographic (including also cathodoluminescence analysis) and microstructural features, joined with mineralogical and metamorphic data such as “illite crystallinity” and K-white mica crystallite size obtained by X-ray powder diffractometry (XRPD), a very low- to low-grade (ca. 300°C) Alpine metamorphic imprint of this portion of the basement can be proposed. Several deformation characteristics (deformation lamellae in quartz, deformation twins in dolomite, fragmented porphyroclasts, and strain shadows) were recognized in the studied samples, showing a weakly to moderately developed disjunctive foliation in the Permian rocks, as well as quartz veinlets, microcracks, and fluid inclusion planes in the Lower Triassic sandstones. Most likely, one of the Cretaceous orogenic events, namely, the “Turonian” phase (Early–Late Cretaceous nappe stacking), resulted in the prograde greenschist facies metamorphism in the study area, instead of the burial depth. We propose that the Permo-Triassic cover succession was also affected by shearing episodes accompanied by fluid migrations along the contact zone between the tectonic units. The scientific approach and dataset provided here are examples of how the application of XRPD parameters of phyllosilicates and micropetrographic observations can help to understand the evolution of an orogen and improve knowledge about the basement structure.
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10003544"> <a href="/gui2/?type=authors&mode=browse&sel=10003544" target="_blank">Varga, Andrea ✉</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10001330"> <a href="/gui2/?type=authors&mode=browse&sel=10001330" target="_blank">Pál-Molnár, Elemér</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10002161"> <a href="/gui2/?type=authors&mode=browse&sel=10002161" target="_blank">Raucsik, Béla</a> </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;33594461" mtid="33594461" target="_blank">Revealing the Mineralogical and Petrographic Signs of Fluid-Related Processes in the Kelebia Basement Area (Szeged Basin, S Hungary): A Case Study of Alpine Prograde Metamorphism in a Permo-Triassic Succession</a></div> <div class="pub-info"> <span class="journal-title">GEOFLUIDS</span> <span class="journal-volume">2023</span> <span class="page"> pp. 1-18. Paper: 8600576 , 18 p. </span> <span class="year">(2023)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_GOLD" title=" Gold "> <a style="color:blue" title="10.1155/2023/8600576" target="_blank" href="https://doi.org/10.1155/2023/8600576"> DOI </a> </span> <span class="id identifier oa_GOLD" title=" Gold "> <a style="color:black" title="158620" target="_blank" href="http://real.mtak.hu/158620"> REAL </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000926101100002" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000926101100002"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85147534761" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85147534761"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="https://www.hindawi.com/journals/geofluids/2023/8600576/" target="_blank" href="https://www.hindawi.com/journals/geofluids/2023/8600576/"> Other URL </a> </span> <span class="id identifier oa_GREEN" title=" Green "> <a style="color:blue" title="26463" target="_blank" href="http://publicatio.bibl.u-szeged.hu/26463"> SZTE Publicatio </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Publication:33594461 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Validated </span></span> <span class="pub-core">Core Citing </span> <span class="pub-type">Journal Article (Article ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Scientific</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="" class="citingPub-count">Citing papers: 2</span> | Independent citation: 1 | Self citation: 1 | Unknown citation: 0 | Number of citations in WoS: 1 | Number of citations in Scopus: 2 | WoS/Scopus assigned: 2 | Number of citations with DOI: 1 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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(<span class="authorship-author-name">Raucsikné Varga Andrea Beáta</span>
<span class="authorAux-mtmt"> földtudomány, kőzettan, geokémia</span>)
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<span class="author-affil"><span title="University of Szeged">SZTE</span>/<span title="Faculty of Science and Informatics">TTIK</span>/<span title="Földrajzi és Földtudományi Intézet">FFI</span>/Department of Mineralogy, Geochemistry and Petrology</span>
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;33594461" target="_blank">Revealing the Mineralogical and Petrographic Signs of Fluid-Related Processes in the Kelebia Basement Area (Szeged Basin, S Hungary): A Case Study of Alpine Prograde Metamorphism in a Permo-Triassic Succession</a></div> <div> <span class="journal-title">GEOFLUIDS</span>
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<span class="journal-volume">2023</span>
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pp 1-18
Paper 8600576.
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<span title="" class="citingPub-count">Citing papers: 2</span>
| Independent citation: 1
| Self citation: 1
| Unknown citation: 0
| Number of citations in WoS: 1
| Number of citations in Scopus: 2
| WoS/Scopus assigned: 2
| Number of citations with DOI: 1
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<div class="mtid"><span class="long-pub-mtid">Publication: 33594461</span>
| <span class="status-data status-VALIDATED"> Validated
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<div class="lastModified">Last Modified: 2023.03.06. 08:43 Béla Raucsik (geokémia, agyagásványtan, kőzettan)
</div>
<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Comments</u>: This work was financially supported by the University of Szeged Open Access Fund (4635), the Bolyai Research Scholarship of the Hungarian Academy of Sciences (BO/266/18), and the National Research, Development, and Innovation Fund (projects no. K 108375 and K 131690).</pre>
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Shale diagenesis differs from that of sandstone and carbonate rocks with regard to the type, evolution stage, and evolution mode. The quality of shale reservoirs is closely linked to the extent of diagenetic evolution. This study identifies the types and characteristics of shale diagenesis using thin sections and scanning electron microscopy (SEM) observations. The stages of shale diagenesis are determined by analyzing organic matter evolution and clay mineral transformation and establishing a diagenetic evolution sequence. This paper describes the comprehensive diagenetic evolution of organic matter, clay minerals, clastic particles, and carbonate minerals to determine the diagenesis types, diagenetic sequences, and pore evolution occurring during diagenetic evolution. The results show that the diagenesis types of shale in the second member of the Funing Formation include compaction, dissolution, cementation, metasomatism, dolomitization, syneresis, and transformation of clay minerals, as well as thermal evolution of organic matter. The middle diagenetic A stage is prevalent, with some areas in the early and middle diagenetic B stages. The shale underwent a diagenetic evolution sequence, including the collapse and shrinkage of montmorillonite interlayers in the early stage; the rapid formation and transformation of illite and smectite mixed layers, massive hydrocarbon generation of organic matters, and dissolution of unstable components in the middle stage; and the occurrence of fractures filled with gypsum, quartz, ferrocalcite, or other authigenic minerals in the later stage. Dissolution pores and fractures are the dominant shale reservoirs of the second member of the Funing Formation in the Subei Basin. The results provide new insights into understanding the formation and evolution of reservoir spaces during shale diagenesis and information for the exploration and development of lacustrine shale oil and gas.
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Department of Geological Sciences, Stanford University, Stanford, CA 94305, United States
Department of Geosciences, Trinity University, San Antonio, TX 78212, United States
Department of Natural & Applied Sciences, University of Wisconsin-Green Bay, Green Bay, WI 54311, United States
Department of Geosciences, The Pennsylvania State University, University ParkPA 16802, United States
Cantrell GeoLogic, Franklin, TN 37069, United States
Department of Resources & Environmental Engineering, Guizhou University, Guizhou Province, Guiyang, 550025, China
Export Date: 24 January 2023
Correspondence Address: Li, X.; Department of Geological Sciences, United States; email: geo.xwli@gmail.com
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Li, X ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Lehrmann, DJ. </span> <span class="author-type"> </span> ; <span class="author-name" > Luczaj, J </span> <span class="author-type"> </span> ; <span class="author-name" > Kelley, BM. </span> <span class="author-type"> </span> ; <span class="author-name" > Cantrell, DL. </span> <span class="author-type"> </span> ; <span class="author-name" > Yu, M </span> <span class="author-type"> </span> ; <span class="author-name" > Ferrill, NL </span> <span class="author-type"> </span> ; <span class="author-name" > Payne, JL. </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;33098794" mtid="33098794" target="_blank">Unraveling overprinted formation mechanisms of massive dolostone in the Lower Triassic sequence of an isolated carbonate platform in Nanpanjiang Basin, south China</a></div> <div class="pub-info"> <span class="journal-title">SEDIMENTARY GEOLOGY</span> <span class="journal-volume">440</span> <span class="page"> Paper: 106240 </span> <span class="year">(2022)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.sedgeo.2022.106240" target="_blank" href="https://doi.org/10.1016/j.sedgeo.2022.106240"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000888850600001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/WOS:000888850600001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85137630526" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85137630526"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://linkinghub.elsevier.com/retrieve/pii/S0037073822001610" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S0037073822001610"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Publication:33098794 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Validated </span></span> <span class="pub-core"> Citing </span> <span class="pub-type">Journal Article (Article ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Scientific</span> </div> </div> </div><div class="JournalArticle Publication long-list">
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;
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;33098794" target="_blank">Unraveling overprinted formation mechanisms of massive dolostone in the Lower Triassic sequence of an isolated carbonate platform in Nanpanjiang Basin, south China</a></div> <div> <span class="journal-title">SEDIMENTARY GEOLOGY</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0037-0738">0037-0738</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1879-0968">1879-0968</a>)</span>:
<span class="journal-volume">440</span>
<span class="page">
Paper 106240.
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<div class="pub-footer">
<span class="language" xmlns="http://www.w3.org/1999/html">Language:
English
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<span class="identifiers">
<span class="id identifier oa_none" title="none">
<a style="color:blue" title="10.1016/j.sedgeo.2022.106240" target="_blank" href="https://doi.org/10.1016/j.sedgeo.2022.106240">
DOI
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<span class="id identifier oa_none" title="none">
<a style="color:blue" title="000888850600001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/WOS:000888850600001">
WoS
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<span class="id identifier oa_none" title="none">
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<div class="mtid"><span class="long-pub-mtid">Publication: 33098794</span>
| <span class="status-data status-VALIDATED"> Validated
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<div class="lastModified">Last Modified: 2023.01.03. 12:54 Béla Raucsik (geokémia, agyagásványtan, kőzettan)
</div>
<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Comments</u>: Department of Geological Sciences, Stanford University, Stanford, CA 94305, United States
Department of Geosciences, Trinity University, San Antonio, TX 78212, United States
Department of Natural & Applied Sciences, University of Wisconsin-Green Bay, Green Bay, WI 54311, United States
Department of Geosciences, The Pennsylv...</pre>
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Noorian, Y ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Moussavi-Harami, R </span> <span class="author-type"> </span> ; <span class="author-name" > Hollis, C </span> <span class="author-type"> </span> ; <span class="author-name" > Reijmer, JJG. </span> <span class="author-type"> </span> ; <span class="author-name" > Mahboubi, A </span> <span class="author-type"> </span> ; <span class="author-name" > Omidpour, A </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;32533869" mtid="32533869" target="_blank">Control of climate, sea-level fluctuations and tectonics on the pervasive dolomitization and porosity evolution of the Oligo-Miocene Asmari Formation (Dezful Embayment, SW Iran)</a></div> <div class="pub-info"> <span class="journal-title">SEDIMENTARY GEOLOGY</span> <span class="journal-volume">427</span> <span class="page"> Paper: 106048 </span> <span class="year">(2022)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.sedgeo.2021.106048" target="_blank" href="https://doi.org/10.1016%2Fj.sedgeo.2021.106048"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000788277300001" target="_blank" href="http://gateway.isiknowledge.com/gateway/Gateway.cgi?&GWVersion=2&SrcAuth=CustomerName&SrcApp=CustomerName&DestLinkType=FullRecord&KeyUT=000788277300001&DestApp=WOS"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85120615957" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85120615957"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://linkinghub.elsevier.com/retrieve/pii/S0037073821002001" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S0037073821002001"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Publication:32533869 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Validated </span></span> <span class="pub-core"> Citing </span> <span class="pub-type">Journal Article (Article ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Scientific</span> </div> </div> </div><div class="JournalArticle Publication long-list"> <div class="authors"> <img title="Idézőközlemény" style="float: left" src="/frontend/resources/grid/publication-citation-icon.png"> <div class="autype autype0"> <span class="author-name" >Noorian Y ✉ </span> ; 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Recrystallization of dolomite can alter textural, mineralogical and geochemical attributes used to infer environmental conditions of initial dolomitization. A meta-analysis of the published literature shows that extensive recrystallization is most common in old and deeply buried dolomites, but data from the Palaeocene–Eocene Umm er Radhuma Formation in Qatar show that this can also happen in geologically young carbonates that have never been deeply buried. Evidence of extensive recrystallization comes from a principal component analysis of published mineralogical and geochemical data that are integrated with new clumped isotope (∆47) measurements and cathodoluminescence petrography. The observations indicate that dolomite stoichiometry and cation ordering correlate with dolomite texture and depth: shallow mimetic dolomites are less stoichiometric and poorly-ordered whereas coarser and deeper planar-e and planar-s to nonplanar dolomites with mottled cathodoluminescence signatures are more stoichiometric and well-ordered, suggesting they have recrystallized. Dolomite δ18O data (Vienna Pee Dee Belemnite) also covary with texture, as mimetic dolomites have the narrowest range (−0.45‰ to +0.38‰), planar-e dolomites are generally ≤0‰ (−2.4‰ to +0.68‰) and planar-s to nonplanar dolomites exhibit the widest range (−2.3‰ to +1.4‰). The principal component analysis results indicate one component with positive loadings for dolomite stoichiometry (+0.752) and cation ordering (+0.813), and negative loading for δ18O (−0.833), trends predicted in recrystallized dolomites. The ∆47-derived temperatures (32 to 46°C) and δ18Ow (+0.18 to +2.6‰ Vienna Standard Mean Ocean Water) reflect recrystallization by warm, slightly evaporated seawater at shallow depths. In the context of a meta-analysis of recrystallized dolomites in the literature, this study implies that extensive dolomite recrystallization in Cenozoic dolomites and shallow-burial conditions is an under-appreciated phenomenon. The results of this study also demonstrate that initial petrological attributes can be significantly altered after dolomitization, hindering interpretations of past seawater chemistry and environmental conditions of dolomitization.
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University of Torino, Department of Earth Sciences, Torino, Italy
ETH Zurich, Department of Earth Sciences, Zurich, Switzerland
Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network, Budapest, Hungary
Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Debrecen, Hungary
Goethe University Frankfurt, Department of Geosciences, Frankfurt am Main, Germany
University of Hamburg, Department of Earth Sciences, Institute for Geology, Hamburg, Germany
Export Date: 2 July 2021
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Barale, L. </span> <span class="author-type"> </span> ; <span class="author-name" > Bertok, C. ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > D’atri, A. </span> <span class="author-type"> </span> ; <span class="author-name" > Piana, F. </span> <span class="author-type"> </span> ; <span class="author-name" > Bernasconi, S.M. </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10024408"> <a href="/gui2/?type=authors&mode=browse&sel=10024408" target="_blank">Czuppon, G.</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10013199"> <a href="/gui2/?type=authors&mode=browse&sel=10013199" target="_blank">Palcsu, L.</a> </span> <span class="author-type"> </span> ; <span class="author-name" > Gerdes, A. </span> <span class="author-type"> </span> ; <span class="author-name" > Birgel, D. </span> <span class="author-type"> </span> ; <span class="author-name" > Martire, L. </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;32089112" mtid="32089112" target="_blank">U-pb dating and geochemical constraints to early cretaceous hydrothermal dolomitization in the provenÇal domain (Maritime alps, nw italy-se france)</a></div> <div class="pub-info"> <span class="journal-title">OFIOLITI</span> <span class="journal-volume">46</span> : <span class="journal-issue">2</span> <span class="page"> pp. 131-149. , 19 p. </span> <span class="year">(2021)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.4454/ofioliti.v46i2.543" target="_blank" href="https://doi.org/10.4454/ofioliti.v46i2.543"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000667160800002" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000667160800002"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85108619059" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85108619059"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://www.ofioliti.it/index.php/ofioliti/article/view/631/576" target="_blank" href="https://www.ofioliti.it/index.php/ofioliti/article/view/631/576"> Other URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Publication:32089112 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Validated </span></span> <span class="pub-core">Core Citing </span> <span class="pub-type">Journal Article (Article ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Scientific</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="" class="citingPub-count">Citing papers: 2</span> | Independent citation: 1 | Self citation: 1 | Unknown citation: 0 | Number of citations in WoS: 2 | Number of citations in Scopus: 2 | WoS/Scopus assigned: 2 | Number of citations with DOI: 2 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;32089112" target="_blank">U-pb dating and geochemical constraints to early cretaceous hydrothermal dolomitization in the provenÇal domain (Maritime alps, nw italy-se france)</a></div> <div> <span class="journal-title">OFIOLITI</span>
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<div class="publication-citation" style="margin-left: 0.5cm;">
<span title="" class="citingPub-count">Citing papers: 2</span>
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<div class="lastModified">Last Modified: 2023.09.07. 17:25 Katalin Temesvári (GKEM admin)
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Comments</u>: National Research Council of Italy, Institute of Geosciences and Earth Resources, Torino, Italy
University of Torino, Department of Earth Sciences, Torino, Italy
ETH Zurich, Department of Earth Sciences, Zurich, Switzerland
Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, ...</pre>
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Xiong, Y </span> <span class="author-type"> </span> ; <span class="author-name" > Wang, LC </span> <span class="author-type"> </span> ; <span class="author-name" > Tan, XC ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Liu, Yun </span> <span class="author-type"> </span> ; <span class="author-name" > Liu, MJ </span> <span class="author-type"> </span> ; <span class="author-name" > Qiao, ZF </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;31674311" mtid="31674311" target="_blank">Dolomitization of the Ordovician subsalt Majiagou Formation in the central Ordos Basin, China: fluid origins and dolomites evolution</a></div> <div class="pub-info"> <span class="journal-title">PETROLEUM SCIENCE</span> <span class="journal-volume">18</span> <span class="page"> pp. 362-379. , 18 p. </span> <span class="year">(2021)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_GOLD" title=" Gold "> <a style="color:blue" title="10.1007/s12182-020-00522-1" target="_blank" href="https://doi.org/10.1007/s12182-020-00522-1"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000591976500001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/WOS:000591976500001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85096453856" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85096453856"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="http://link.springer.com/10.1007/s12182-020-00522-1" target="_blank" href="http://link.springer.com/10.1007/s12182-020-00522-1"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Publication:31674311 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Validated </span></span> <span class="pub-core"> Citing </span> <span class="pub-type">Journal Article (Article ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Scientific</span> </div> </div> </div><div class="JournalArticle Publication long-list"> <div class="authors"> <img title="Idézőközlemény" style="float: left" src="/frontend/resources/grid/publication-citation-icon.png"> <div class="autype autype0"> <span class="author-name" >Xiong Y </span> ; 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Funding Agency and Grant Number: University of Szeged Open Access Fund [4389]; Bolyai Research Scholarship of the Hungarian Academy of SciencesHungarian Academy of Sciences [BO/266/18]; National Research, Development and Innovation Fund [OTKA K 108375]; New National Excellence Program of the Ministry of Human Capacities [UNKP-18-4-SZTE-16]; New National Excellence Program of the Ministry for Innovation and Technology [UNKP-19-4-SZTE-34]
Funding text: For petrographic analysis of the Pennsylvanian Teseny rocks, Mining and Geological Survey of Hungary (Dept. of Geological and Geophysical Collections, Budapest) provided thin section collection from borehole Bm-1. We thank Gyorgy Szakmany and Sandor Jozsa (Eotvos Lorand University, Budapest), Zoltan Mathe (Mecsekerc Ltd., Pecs), and Balint Peterdi (Mining and Geological Survey of Hungary) for the studied samples. The authors are grateful to Tivadar M. Toth (University of Szeged) and Ronald J. Bakker and Federica Zaccarrini (Montanuniversitat Leoben) for their supports during analytical measurements. This work was financially supported by the University of Szeged Open Access Fund (4389), the Bolyai Research Scholarship of the Hungarian Academy of Sciences (BO/266/18), the National Research, Development and Innovation Fund (OTKA K 108375), the New National Excellence Program of the Ministry of Human Capacities (UNKP-18-4-SZTE-16), and the New National Excellence Program of the Ministry for Innovation and Technology (UNKP-19-4-SZTE-34).
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Comments</u>: Funding Agency and Grant Number: University of Szeged Open Access Fund [4389]; Bolyai Research Scholarship of the Hungarian Academy of SciencesHungarian Academy of Sciences [BO/266/18]; National Research, Development and Innovation Fund [OTKA K 108375]; New National Excellence Program of the Ministry of Human Capacities [UNKP-18-4-SZTE-16]; New National Excellence Program of the Ministry for In...</pre>
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<span class="author-affil"><span title="Eötvös Loránd University">ELTE</span>/<span title="Faculty of Science">ELU FoS</span>/<span title="Institute of Geography and Earth Sciences">Inst_GeogrEarthSci</span>/<span title="Center of Earth Sciences">Cntr_EarthSci</span>/MTA-ELTE Geological, Geophysical and Space Sciences Research Group</span>
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;31372620" target="_blank">A rejtelmes dolomit</a></div> <div> <span class="journal-title">FÖLDTANI KÖZLÖNY</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0015-542X">0015-542X</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/2559-902X">2559-902X</a>)</span>:
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pp 233-266
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<div class="pub-footer">
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<span class="identifiers">
<span class="id identifier oa_GOLD" title=" Gold
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DOI
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<span class="id identifier oa_GREEN" title=" Green
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<a style="color:black" title="123244" target="_blank" href="http://real.mtak.hu/123244">
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Scopus
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<div class="publication-citation" style="margin-left: 0.5cm;">
<span title="" class="citingPub-count">Citing papers: 1</span>
| Independent citation: 1
| Self citation: 0
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| WoS/Scopus assigned: 1
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<div class="mtid"><span class="long-pub-mtid">Publication: 31372620</span>
| <span class="status-data status-VALIDATED"> Validated
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<div class="notDuplums"><a target="_blank" href="/api/publication/31372620/notduplums">1 marked as not duplum</a>
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<div class="lastModified">Last Modified: 2023.09.11. 09:27 Zsolt Baráth (KIADÓK központi 3, admin)
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Comments</u>: Cited By :1
Export Date: 4 January 2023</pre>
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Jiao, X </span> <span class="author-type"> </span> ; <span class="author-name" > Liu, Y </span> <span class="author-type"> </span> ; <span class="author-name" > Yang, W </span> <span class="author-type"> </span> ; <span class="author-name" > Zhou, D </span> <span class="author-type"> </span> ; <span class="author-name" > Bai, B </span> <span class="author-type"> </span> ; <span class="author-name" > Zhang, T </span> <span class="author-type"> </span> ; <span class="author-name" > Zhao, M </span> <span class="author-type"> </span> ; <span class="author-name" > Li, Z </span> <span class="author-type"> </span> ; <span class="author-name" > Meng, Z </span> <span class="author-type"> </span> ; <span class="author-name" > Yang, Y </span> <span class="author-type"> </span> et al. </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;31034402" mtid="31034402" target="_blank">Fine-grained volcanic-hydrothermal sedimentary rocks in Permian Lucaogou Formation, Santanghu Basin, NW China: Implications on hydrocarbon source rocks and accumulation in lacustrine rift basins</a></div> <div class="pub-info"> <span class="journal-title">MARINE AND PETROLEUM GEOLOGY</span> <span class="journal-volume">114</span> <span class="page"> Paper: 104201 </span> <span class="year">(2020)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.marpetgeo.2019.104201" target="_blank" href="https://doi.org/10.1016/j.marpetgeo.2019.104201"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000514747800004" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/WOS:000514747800004"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85076857900" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85076857900"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://linkinghub.elsevier.com/retrieve/pii/S0264817219306555" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S0264817219306555"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Publication:31034402 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Validated </span></span> <span class="pub-core"> Citing </span> <span class="pub-type">Journal Article (Article ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Scientific</span> </div> </div> </div><div class="JournalArticle Publication long-list"> <div class="authors"> <img title="Idézőközlemény" style="float: left" src="/frontend/resources/grid/publication-citation-icon.png"> <div class="autype autype0"> <span class="author-name" >Jiao X </span> ; 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<div class="lastModified">Last Modified: 2021.01.14. 13:21 Petra Csonka (SZTE admin5 SZAOK Anatómia)
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Comments</u>: Cited By :1
Export Date: 12 February 2021
Correspondence Address: M Tóth, T.; University of Szeged, Hungary; email: mtoth@geo.u-szeged.hu
Funding text 1: The authors thank Enago (www.enago.com) for the English language review. Three anonymous reviewers are thanked for their valuable comments.
Cited By :3
...</pre>
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Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Szeged, 6720, Hungary
Public Limited Company for Radioactive Waste Management (PURAM), Budapest, 2040, Hungary
Export Date: 12 February 2021
Correspondence Address: Tóth, T.M.; Department of Mineralogy, Hungary; email: mtoth@geo.u-szeged.hu
Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Szeged, 6720, Hungary
Public Limited Company for Radioactive Waste Management (PURAM), Budapest, 2040, Hungary
Export Date: 18 April 2021
Correspondence Address: Tóth, T.M.; Department of Mineralogy, Hungary; email: mtoth@geo.u-szeged.hu
Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Szeged, 6720, Hungary
Public Limited Company for Radioactive Waste Management (PURAM), Budapest, 2040, Hungary
Export Date: 12 September 2021
Correspondence Address: Tóth, T.M.; Department of Mineralogy, Hungary; email: mtoth@geo.u-szeged.hu
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10001322"> <a href="/gui2/?type=authors&mode=browse&sel=10001322" target="_blank">M. Tóth, T ✉</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10047666"> <a href="/gui2/?type=authors&mode=browse&sel=10047666" target="_blank">Molnár, L</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10060779"> <a href="/gui2/?type=authors&mode=browse&sel=10060779" target="_blank">Körmös, S</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10038084"> <a href="/gui2/?type=authors&mode=browse&sel=10038084" target="_blank">Czirbus, N</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10013776"> <a href="/gui2/?type=authors&mode=browse&sel=10013776" target="_blank">Schubert, F</a> </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;31646840" mtid="31646840" target="_blank">Localisation of Ancient Migration Pathways inside a Fractured Metamorphic Hydrocarbon Reservoir in South-East Hungary</a></div> <div class="pub-info"> <span class="journal-title">APPLIED SCIENCES-BASEL</span> <span class="journal-volume">10</span> : <span class="journal-issue">20</span> <span class="page"> Paper: 7321 , 20 p. </span> <span class="year">(2020)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_GOLD" title=" Gold "> <a style="color:blue" title="10.3390/app10207321" target="_blank" href="https://doi.org/10.3390/app10207321"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000585209600001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000585209600001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85093865923" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85093865923"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://www.mdpi.com/2076-3417/10/20/7321" target="_blank" href="https://www.mdpi.com/2076-3417/10/20/7321"> Other URL </a> </span> <span class="id identifier oa_GREEN" title=" Green "> <a style="color:blue" title="22092" target="_blank" href="http://publicatio.bibl.u-szeged.hu/22092"> SZTE Publicatio </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Publication:31646840 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Validated </span></span> <span class="pub-core">Core Citing </span> <span class="pub-type">Journal Article (Article ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Scientific</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="" class="citingPub-count">Citing papers: 2</span> | Independent citation: 0 | Self citation: 2 | Unknown citation: 0 | Number of citations in WoS: 1 | Number of citations in Scopus: 2 | WoS/Scopus assigned: 2 | Number of citations with DOI: 2 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Comments</u>: Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Szeged, 6720, Hungary
Public Limited Company for Radioactive Waste Management (PURAM), Budapest, 2040, Hungary
Export Date: 11 February 2021
Correspondence Address: Tóth, T.M.; Department of Mineralogy, Hungary; email: mtoth@geo.u-szeged.hu
Departme...</pre>
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10000210"> <a href="/gui2/?type=authors&mode=browse&sel=10000210" target="_blank">Fodor, L ✉</a> </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;30852034" mtid="30852034" target="_blank">Results, problems and future tasks of palaeostress and fault-slip analyses in the Pannonian Basin: the Hungarian contribution</a></div> <div class="pub-info"> <span class="journal-title">FÖLDTANI KÖZLÖNY</span> <span class="journal-volume">149</span> : <span class="journal-issue">4</span> <span class="page"> pp. 297-326. , 30 p. </span> <span class="year">(2019)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_GOLD" title=" Gold "> <a style="color:blue" title="10.23928/foldt.kozl.2019.149.4.297" target="_blank" href="https://doi.org/10.23928/foldt.kozl.2019.149.4.297"> DOI </a> </span> <span class="id identifier oa_GREEN" title=" Green "> <a style="color:black" title="173101" target="_blank" href="http://real.mtak.hu/173101"> REAL </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85074969994" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85074969994"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="http://ojs3.mtak.hu/index.php/foldtanikozlony/article/view/1711" target="_blank" href="http://ojs3.mtak.hu/index.php/foldtanikozlony/article/view/1711"> Other URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Publication:30852034 </span> <span class="status-holder"><span class="status-data status-APPROVED"> Published </span></span> <span class="pub-core">Core Citing </span> <span class="pub-type">Journal Article (Article ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Scientific</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="" class="citingPub-count">Citing papers: 5</span> | Independent citation: 4 | Self citation: 1 | Unknown citation: 0 | Number of citations in WoS: 2 | Number of citations in Scopus: 4 | WoS/Scopus assigned: 4 | Number of citations with DOI: 4 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<span class="authorAux-mtmt"> Geológia</span>)
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<span class="author-affil"><span title="Eötvös Loránd University">ELTE</span>/<span title="Faculty of Science">ELU FoS</span>/<span title="Institute of Geography and Earth Sciences">Inst_GeogrEarthSci</span>/<span title="Center of Earth Sciences">Cntr_EarthSci</span>/MTA-ELTE Geological, Geophysical and Space Sciences Research Group; <span title="Eötvös Loránd University">ELTE</span>/<span title="Faculty of Science">ELU FoS</span>/<span title="Institute of Geography and Earth Sciences">Inst_GeogrEarthSci</span>/<span title="Center of Earth Sciences">Cntr_EarthSci</span>/MTA-ELTE Volcanology Research Group</span>
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;30852034" target="_blank">Results, problems and future tasks of palaeostress and fault-slip analyses in the Pannonian Basin: the Hungarian contribution</a></div> <div> <span class="journal-title">FÖLDTANI KÖZLÖNY</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0015-542X">0015-542X</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/2559-902X">2559-902X</a>)</span>:
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<span title="" class="citingPub-count">Citing papers: 5</span>
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| Unknown citation: 0
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<div class="mtid"><span class="long-pub-mtid">Publication: 30852034</span>
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<div class="lastModified">Last Modified: 2023.09.08. 14:29 Zsolt Baráth (KIADÓK központi 3, admin)
</div>
<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Comments</u>: Export Date: 27 November 2019
Correspondence Address: Fodor, L.; MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/C, Hungary; email: lasz.Fodor@yahoo.com</pre>
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Funding Agency and Grant Number: American Association of Petroleum Geologists; Geological Society of America Graduate Student Research Grant Program; International Association of Sedimentologists; Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [OTKA K124313]; National Research, Development and Innovation Office (NKFIH) [KH 125584]
Funding text: This work was supported by the American Association of Petroleum Geologists Grants-in-Aid Program, the Geological Society of America Graduate Student Research Grant Program, the International Association of Sedimentologists Post-Graduate Grant Scheme, and the Hungarian Scientific Research Fund (OTKA K124313). SK was supported by the National Research, Development and Innovation Office (NKFIH, KH 125584). The authors are indebted to Tames Budai and Gyula Konrad for their continued help and support, and to Mecsekerc Ltd. for providing access to the VP-2 drill cores. The comments and suggestions of Alessandro Iannace and an anonymous reviewer are greatly appreciated. This is an Oklahoma State University Boone Pickens School of Geology contribution #2018-93.
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<span class="author-name" >Machel HG
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;30342399" target="_blank">Multi-phase dolomitization and recrystallization of Middle Triassic shallow marine–peritidal carbonates from the Mecsek Mts. (SW Hungary), as inferred from petrography, carbon, oxygen, strontium and clumped isotope data</a></div> <div> <span class="journal-title">MARINE AND PETROLEUM GEOLOGY</span>
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<div class="mtid"><span class="long-pub-mtid">Publication: 30342399</span>
| <span class="status-data status-VALIDATED"> Validated
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<div class="lastModified">Last Modified: 2021.10.20. 17:28 Katalin Temesvári (MTMT ellenőrzés admin5)
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Comments</u>: Funding Agency and Grant Number: American Association of Petroleum Geologists; Geological Society of America Graduate Student Research Grant Program; International Association of Sedimentologists; Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [OTKA K124313]; National Research, Development and Innovation Office (NKFIH) [KH 125584]
Funding text: T...</pre>
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Department of Mineralogy Geochemistry and Petrology, University of SzegedH-6722, Hungary
Geothermal Service Provider LtdH-6724, Hungary
Export Date: 27 November 2019
Correspondence Address: Varga, A.; Department of Mineralogy Geochemistry and Petrology, University of SzegedHungary; email: raucsikvarga@geo.u-szeged.hu
Funding Agency and Grant Number: Economy Development and Innovation Operative Programme [GINOP-2.1.1-15-2016-00970]; National Research, Development and Innovation Fund of Hungary [K 108375]
Funding text: The authors are thankful for the hydrochemical data and the scale and rock samples from the geothermal heating systems operating in Szeged owned by the Geothermal Service Provider Ltd., Hungary. This research was financially supported by the Economy Development and Innovation Operative Programme (GINOP-2.1.1-15-2016-00970). Regarding sandstone reservoir characterization, this research was also supported by the National Research, Development and Innovation Fund of Hungary (project Number K 108375).
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10003544"> <a href="/gui2/?type=authors&mode=browse&sel=10003544" target="_blank">Varga, A</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10029355"> <a href="/gui2/?type=authors&mode=browse&sel=10029355" target="_blank">Bozsó, G</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10051080"> <a href="/gui2/?type=authors&mode=browse&sel=10051080" target="_blank">Garaguly, I</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10002161"> <a href="/gui2/?type=authors&mode=browse&sel=10002161" target="_blank">Raucsik, B</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10037489"> <a href="/gui2/?type=authors&mode=browse&sel=10037489" target="_blank">Bencsik, A</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10032630"> <a href="/gui2/?type=authors&mode=browse&sel=10032630" target="_blank">Kóbor, B</a> </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;30644307" mtid="30644307" target="_blank">Cements, Waters, and Scales: An Integrated Study of the Szeged Geothermal Systems (SE Hungary) to Characterize Natural Environmental Conditions of the Thermal Aquifer</a></div> <div class="pub-info"> <span class="journal-title">GEOFLUIDS</span> <span class="journal-volume">2019</span> <span class="page"> Paper: 4863814 , 21 p. </span> <span class="year">(2019)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_GOLD" title=" Gold "> <a style="color:blue" title="10.1155/2019/4863814" target="_blank" href="https://doi.org/10.1155/2019/4863814"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000467102300001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000467102300001"> WoS </a> </span> <span class="id identifier oa_GOLD" title=" Gold "> <a style="color:black" title="100517" target="_blank" href="http://real.mtak.hu/100517"> REAL </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85065622077" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85065622077"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://www.hindawi.com/journals/geofluids/2019/4863814/" target="_blank" href="https://www.hindawi.com/journals/geofluids/2019/4863814/"> Other URL </a> </span> <span class="id identifier oa_GREEN" title=" Green "> <a style="color:blue" title="15256" target="_blank" href="http://publicatio.bibl.u-szeged.hu/15256"> SZTE Publicatio </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Publication:30644307 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Validated </span></span> <span class="pub-core">Core Citing </span> <span class="pub-type">Journal Article (Article ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Scientific</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="" class="citingPub-count">Citing papers: 8</span> | Independent citation: 6 | Self citation: 2 | Unknown citation: 0 | Number of citations in WoS: 4 | Number of citations in Scopus: 6 | WoS/Scopus assigned: 6 | Number of citations with DOI: 6 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<span class="authorAux-mtmt"> földtudomány, kőzettan, geokémia</span>)
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<span class="author-affil"><span title="University of Szeged">SZTE</span>/<span title="Faculty of Science and Informatics">TTIK</span>/<span title="Földrajzi és Földtudományi Intézet">FFI</span>/Department of Mineralogy, Geochemistry and Petrology</span>
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;
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<span class="author-affil"><span title="University of Szeged">SZTE</span>/<span title="Faculty of Science and Informatics">TTIK</span>/<span title="Földrajzi és Földtudományi Intézet">FFI</span>/Department of Mineralogy, Geochemistry and Petrology</span>
;
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href="/gui2/?type=authors&mode=browse&sel=10002161" target="_blank">Raucsik B
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<span class="authorAux-mtmt"> geokémia, agyagásványtan, kőzettan</span>)
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<span class="author-affil"><span title="University of Szeged">SZTE</span>/<span title="Faculty of Science and Informatics">TTIK</span>/<span title="Földrajzi és Földtudományi Intézet">FFI</span>/Department of Mineralogy, Geochemistry and Petrology</span>
;
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<span class="author-affil"><span title="University of Szeged">SZTE</span>/<span title="Faculty of Science and Informatics">TTIK</span>/<span title="Földrajzi és Földtudományi Intézet">FFI</span>/Department of Mineralogy, Geochemistry and Petrology</span>
;
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<span class="author-affil"><span title="University of Szeged">SZTE</span>/<span title="Faculty of Science and Informatics">TTIK</span>/<span title="Földrajzi és Földtudományi Intézet">FFI</span>/Department of Mineralogy, Geochemistry and Petrology</span>
</div>
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;30644307" target="_blank">Cements, Waters, and Scales: An Integrated Study of the Szeged Geothermal Systems (SE Hungary) to Characterize Natural Environmental Conditions of the Thermal Aquifer</a></div> <div> <span class="journal-title">GEOFLUIDS</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/1468-8115">1468-8115</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1468-8123">1468-8123</a>)</span>:
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Paper 4863814.
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<span title="" class="citingPub-count">Citing papers: 8</span>
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| Self citation: 2
| Unknown citation: 0
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| Number of citations in Scopus: 6
| WoS/Scopus assigned: 6
| Number of citations with DOI: 6
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<a target="_blank" href="/api/publication?cond=citations.related;eq;30644307&sort=publishedYear,desc&sort=title">
Number of cited publications: 17
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<div class="mtid"><span class="long-pub-mtid">Publication: 30644307</span>
| <span class="status-data status-VALIDATED"> Validated
</span>
Core Citing
| <span class="type-subtype">Journal Article
( Article
)
</span>
| <span class="pub-category">Scientific</span>
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<div class="lastModified">Last Modified: 2022.02.09. 15:39 Andrea Vándor (VA, admin)
</div>
<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Comments</u>: Department of Mineralogy Geochemistry and Petrology, University of SzegedH-6722, Hungary
Geothermal Service Provider LtdH-6724, Hungary
Export Date: 27 November 2019
Correspondence Address: Varga, A.; Department of Mineralogy Geochemistry and Petrology, University of SzegedHungary; email: raucsikvarga@geo.u-szeged.hu
Fundin...</pre>
</div></div>