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  • 1 Department of General and Applied Geology, Eötvös Loránd University, Budapest, Hungary
  • | 2 Department of Earth & Atmospheric Sciences, University of Alberta, Edmonton, Canada
  • | 3 H-1117, Budapest, Pázmány P. sétány 1/C, Hungary
  • | 4 1-26 Earth Sciences Building, Edmonton, AB, T6G 2E3, Canada
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Abstract

In the surroundings of Berekfürdő (Trans-Tisza Region) a significant positive anomaly was observed in the fluid potential field, in the course of a regional-scale hydrogeologic study of the Great Hungarian Plain (Tóth and Almási 2001). It was assumed that the cause of this phenomenon could be the presence of structural elements in an overpressured fluid potential field. The seismic, hydraulic and hydrogeochemical evaluation of the anomaly proved the presence of a complex structure. The results furnish an example for the theoretical model of Matthäi and Roberts (1996). The identified faults, which define the basement high and rise close to the surface, represent direction-dependent control over the fluid flow systems of the Study Area. The detected horizontal barrier fault zones may act as lateral seals of the Tatárülés-Kunmadaras gas field and might ensure the active water pressure of the reservoir system. The junction of the vertically conducting and horizontally sealing fault zones near Berekfürdő represent the southern limit of the prolific hydrocarbon-bearing Szolnok and the identified “extra“ aquifer. The junction of these faults causes intensive water upwelling which was drilled by Pávai-Vajna in 1928. This exploration initiated the development of the Berekfürdő Spa.

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  • J.S. Caine J.P. Evans C.B. Forster 1996 Fault zone architecture and permeability structure Geology 24 11 1025 1028.

  • B. Czauner 2008 Vetők hidraulikai viselkedésének komplex vizsgálata Berekfürdő térségében ELTE Dept. of Physical and Applied Geology Budapest (Complex research of hydraulic behaviour of faults near Berekfürdő).

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  • Gy. Juhász 1992 A pannóniai (s.l.) formációk térképezése az Alföldön: elterjedés, fácies és üledékes környezet Földtani Közlöny 122 2–4 133 165 (Pannonian s.l. formations in the Hungarian Plain: distribution, facies and sedimentary environments).

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  • Kiss, J., E. Szalma 2007: Tündérrózsák és a gravitációs tér? (Water-lily and the gravity field?) — Magyar Geofizika, 48/2. (In Hungarian.).

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  • Lőrincz, K, F. Horváth, G. Detzky 2002: Neotectonics and its relation to the Mid-Hungarian Mobile Belt. — EGU Stephan Müller Special Publication Series 3, pp. 247266.

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  • Mádl-Szőnyi, J., J. Tóth 2009: A hydrogeological type section for the Duna-Tisza Interfluve, Hungary. — Hydrogeology Journal. DOI: .

  • S.K. Matthäi S.G. Roberts 1996 The influence of fault permeability on single-phase fluid flow near fault-sand intersections: results from steady-state high resolution models of pressure-driven fluid flow AAPG Bulletin 80 11 1763 1779.

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  • Mészáros, E. 2005: Hidrogeológiai célú szeizmikus értelmezés a Duna-völgy északkeleti részén (Seismic interpretation for hydrogeological purposes on the NE part of Danube-valley). — MSc Thesis, ELTE Dept. of Applied and Environmental Geology, 84 p. (In Hungarian.).

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  • G. Pogácsás L. Lakatos A. Barvitz G. Vakarcs Cs. Farkas 1989 Pliocén-kvarter oldaleltolódások a Nagyalföldön Általános Földtani Szemle 24 149 169 (Pliocene-Quaternary strike-slip faults in the Great Hungarian Plain).

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  • T. Tóth F. Horváth 1997 Neotectonic investigations by high resolution seismic profiling S. Marosi A. Meskó Seismic safety of the Paks nuclear power plant Academical Press Budapest 123 132.

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  • J. Tóth I. Almási 2001 Interpretation of observed fluid potential patterns in a deep sedimentary basin under tectonic compression: Hungarian Great Plain, Pannonian Basin Geofluids 1 11 36.

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  • Underschultz, J.R., C.J. Otto, R. Bartlett 2005: Formation fluids in faulted aquifers: examples from the foothills of Western Canada and the North West Shelf of Australia. — In: Boult, P., J. Kaldi (eds): Evaluating fault and cap rock seals, AAPG Hedberg Series 2, pp. 247260.

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Senior editors

Editor(s)-in-Chief: Attila DEMÉNY

Deputy Editor(s)-in-Chief: Béla RAUCSIK

Co-ordinating Editor(s): Gábor SCHMIEDL

Editorial Board

  • Zsolt BENKÓ (Geochemistry, Ar dating; Institute for Nuclear Research, Debrecen)
  • Szabolcs HARANGI (Petrology, geochemistry, volcanology; Eötvös Loránd University, Budapest)
  • Anette GÖTZ (Sedimentology; Landesamt für Bergbau, Energie und Geologie, Hannover)
  • János HAAS (Regional Geology and Sedimentology; Eötvös Loránd University, Budapest)
  • István Gábor HATVANI (Geomathematics; Institute for Geological and Geochemical Research, Budapest)
  • Henry M. LIEBERMAN (Language Editor; Salt Lake City)
  • János KOVÁCS (Quaternary geology; University of Pécs)
  • Szilvia KÖVÉR (Sedimentology; Eötvös Loránd University, Budapest)
  • Tivadar M. TÓTH (Mineralogy; Petrology    University of Szeged)
  • Stephen J. MOJZSIS (Petrology, geochemistry and planetology; University of Colorado Boulder)
  • Norbert NÉMETH (Structural geology; University of Miskolc)
  • Attila ŐSI (Paleontology; Eötvös Loránd University, Budapest)
  • József PÁLFY (Fossils and Stratigraphic Records; Eötvös Loránd University, Budapest)
  • György POGÁCSÁS (Petroleum Geology; Eötvös Loránd University, Budapest)
  • Krisztina SEBE (Tectonics, sedimentology, geomorphology University of Pécs)
  • Ioan SEGHEDY (Petrology and geochemistry; Institute of Geodynamics, Bucharest)
  • Lóránd SILYE (Paleontology; Babeș-Bolyai University, Cluj-Napoca)
  • Ákos TÖRÖK (Applied and Environmental Earth Sciences; Budapest University of Technology and Economics, Budapest)
  • Norbert ZAJZON (Petrology and geochemistry; University of Miskolc)
  • Ferenc MOLNÁR (ore geology, geochemistry, geochronology, archaeometry; Geological Survey of Finland, Espoo)

Advisory Board

Due to the changes in editorial functions, the Advisory Board has been terminated. The participation of former Advisory Board members is highly appreciated and gratefully thanked.

CENTRAL EUROPEAN GEOLOGY
Institute for Geochemical Research
Hungarian Academy of Sciences
Address: Budaörsi út 45. H-1112 Budapest, Hungary
Phone: (06 1) 309 2681
Phone/fax: (06 1) 319 3137
E-mail: demeny@geochem.hu

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2020  
Scimago
H-index
24
Scimago
Journal Rank
0,253
Scimago
Quartile Score
Geology Q3
Scopus
Cite Score
59/33=1,8
Scopus
Cite Score Rank
Geology 134/251 (Q3)
Scopus
SNIP
0,679
Scopus
Cites
146
Scopus
Documents
4
Days from submission to acceptance 247
Days from acceptance to publication 229
Acceptance
Rate
36%

 

2019  
Scimago
H-index
22
Scimago
Journal Rank
0,313
Scimago
Quartile Score
Geology Q3
Scopus
Cite Score
43/33=1,3
Scopus
Cite Score Rank
Geology 151/235(Q3)
Scopus
SNIP
0,593
Scopus
Cites
106
Scopus
Documents
7
Acceptance
Rate
47%

 

Central European Geology
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Central European Geology
Language English
Size Vol 1-63: B5
Vol 64- : A4
Year of
Foundation
2007 (1952)
Publication
Programme
2021 Volume 64
Volumes
per Year
1
Issues
per Year
4
Founder Magyar Tudományos Akadémia
Founder's
Address
H-1051 Budapest, Hungary, Széchenyi István tér 9.
Publisher Akadémiai Kiadó
Publisher's
Address
H-1117 Budapest, Hungary 1516 Budapest, PO Box 245.
Responsible
Publisher
Chief Executive Officer, Akadémiai Kiadó
ISSN 1788-2281 (Print)
ISSN 1789-3348 (Online)

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