Crustal structure of the Western Carpathians and Pannonian Basin: Seismic models from CELEBRATION 2000 data and geological implications

Janik, Tomasz; Grad, M.; Guterch, A.; Vozár, J.; Bielik, Miroslav; Vozárová, Anna; Hegedűs, E.; Kovács, Csaba Attila; Kovàcs, István; Keller, G. Randy

doi:10.1016/j.jog.2010.12.002

Cited by 59 publications

(81 citation statements)

References 56 publications

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“…The CCZ may have been cre ated by hor i zon tal dis place ment at the contact be tween the In ner West ern Carpathians blocks and blocks de rived of Eu ro pean Plat form and the plat form it self. This in ter pre ta tion is sup ported by seis mic mod els of the CEL-11 pro file (Janik et al, 2011), part of the CELEBRATION 2000 pro ject, where the Eu ro pean Plat form mar gin is sit u ated north of the Klippen Belt and where, in the space be tween the Eu ro pean Plat form and the Klippen Belt, a newly in ter preted Pieniny crustal seg ment has been in serted.…”

Section: The Relationship Between Carpathian Conductivity Zone and Thmentioning

confidence: 94%

New magnetic anomalies of the Outer Capathians in NE Slovakia and their relationship to the Carpathian Conductivity Zone

Kucharič¹,

Bezák

Kubeš³

et al. 2012

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Hith erto un known mag netic anom a lies have been de tected while as sem bling a mag netic pic ture of the Slovakian ter ri tory. An im pres sive mag netic anom aly was rec og nized in the northeasternmost part of Slovakia as so ci ated with sed i men tary rocks of the flysch belt. This is a rare phe nom e non, be cause the flysch se quence in Slovakia typ i cally lacks mag netic rocks. Thus, an ig ne ous body in truded into the flysch might cause the anom aly. The shape and the char ac ter of the anom a lous body sug gests that its source is lo cated at shal low depth be neath the sur face. The anom aly has been mod elled in 2D space. It is in ter preted as a Neo gene vol ca nic neck made of in ter me di ate rocks. Such an in ter pre ta tion is sup ported by re sults of thermo met ric in ves ti ga tion of fluid in clu sions, vitrinite reflectance and fis sion tracks. Fur ther mi nor anom a lies within this area, might also be caused by small near these subvolcanic bod ies. The Carpathian Con duc tiv ity Zone is lo cated near these new ob served mag netic anom a lies, which there fore pro vide a new view on the im por tance of this zone. The re gion as a re sult may have po ten tial for metalogenesis, un der ground stor age of car bon di ox ide, and hy dro car bons.

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Section: The Relationship Between Carpathian Conductivity Zone and Thmentioning

confidence: 94%

New magnetic anomalies of the Outer Capathians in NE Slovakia and their relationship to the Carpathian Conductivity Zone

Kucharič¹,

Bezák

Kubeš³

et al. 2012

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“…The high-quality seismic data obtained reveal a variety of both the P-and S-wave phases. The main results were published in Guterch et al (1999Guterch et al ( , 2004Guterch et al ( , 2007, Grad et al (1999, 2002a,b, 2003a, 2009), Jensen et al (1999, Środa and POLONAISE P3 Working Group (1999), Wilde-Pió rko et al (1999), Krysi nski et al (2000, 2009, Bayer et al (2002), Czuba et al (2002), Janik et al (2002Janik et al ( , 2005Janik et al ( , 2009Janik et al ( , 2011Janik et al ( ), Środa et al (2002Janik et al ( , 2006, Winchester et al (2002), Rů žek et al (2003, Hrubcová et al (2005, 2010), Majda nski et al (2005, Malinowski et al (2005,b), Br€ uckl et al (2007, 2010, Šumanovac et al (2009), andNarkiewicz et al (2011).…”

Section: A New Generation Of Long-range Seismic Experimentsmentioning

confidence: 97%

Crustal and Lithospheric Structures Between the Alps and East European Craton from Long-Range Controlled Source Seismic Experiments

Guterch

Grad²,

Keller³

et al. 2015

Treatise on Geophysics

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“…We consider that the observed geothermal parameters -both the temperature and the heat flow density distribution -are regionally influenced by the thermal phenomena of the deep-seated fault system related to the European Platform margin situated north of the Klippen Belt (Janik et al, 2011;Kucharič et al, 2013b and others).…”

Section: Analysis Of Data and Interpretationmentioning

confidence: 99%

Regional and local phenomena influencing the thermal state in the Flysch belt of the northeastern part of Slovakia

Majcin

Bilčík

Кутас

et al. 2014

Contributions to Geophysics and Geodesy

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Abstract:The locality of the northeastern most part of Slovakian Flysch belt belongs to interesting areas in terms of the interpretation of geothermal conditions in mutual relation with the lithosphere structure and their tectonic development. The evaluation of the geothermal energy sources parameters of this locality is likewise worthwhile. The region under study has the centre in position of the borehole Zboj ZB-1 and spreads out Slovakia also in Poland and Ukraine.Our contribution provides the analyses of existing geothermal data enhanced by the construction of temperature field models corresponding to the global and local aspects that influence the temperature and heat flow density distributions. The analyses are related to the structures and effects of separate phenomena along as well as across the Carpathian arc. The model calculations were carried out both by analytical and numerical methods of solving the heat transfer equations including their steady state forms and transient cases too.Besides the regional trend of thermal activity decrease in direction from East-Slovakian Basin to the outer Carpathian units the combined local influences are applied: subsurface thermophysical parameters of rock complexes distributions, non-stationary sources from supposed subvolcanic bodies in close surroundings of borehole Zboj ZB-1, and the effects of the hydrological factors. Considering the observed higher thermal activity in arched zone along the Carpathian structures we discussed the thermal effects of rock complexes supposed as a source of regional Carpathian Conductivity Anomaly and the transfer of heat from East-Slovakian Basin to Outer Carpathian Flysch units. The analysis and the modelling results suggest that the mentioned activity is caused by the influences of source type phenomena mainly related to deep fault systems at the margin of the European Platform. That means the anomalies in heat flow density distribution can reach the value 70 mW/m 2 and more in the zone above the thermally active deep-fault system with the presence of volcanism and hydrothermal activities.

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Crustal structure of the Western Carpathians and Pannonian Basin: Seismic models from CELEBRATION 2000 data and geological implications

Cited by 59 publications

References 56 publications

New magnetic anomalies of the Outer Capathians in NE Slovakia and their relationship to the Carpathian Conductivity Zone

New magnetic anomalies of the Outer Capathians in NE Slovakia and their relationship to the Carpathian Conductivity Zone

Crustal and Lithospheric Structures Between the Alps and East European Craton from Long-Range Controlled Source Seismic Experiments

Regional and local phenomena influencing the thermal state in the Flysch belt of the northeastern part of Slovakia

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