Carbonate complexes underlying Flysch belt and subsurface Neogene volcanic in the NE part of Slovakia – a potential for geothermal energy and raw materials

Carbonate complexes underlying Flysch belt and subsurface Neogene volcanic in the NE part of Slovakia – a potential for geothermal energy and raw materials

A positive gravity anomaly was observed in the Flysch belt realm. Based on this fact and available geological knowledge we suppose that the source of gravity anomaly might be carbonate rocks lying perhaps in the footwall of Flysch sediments. The carbonates belong perhaps to the Penninic crust cover...

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Bibliographic Details
Main Authors: Ľudovít KUCHARIČ, Vladimír BEZÁK, Dušan MAJCIN, Ján VOZÁR
Format: Article
Language:English
Published: Earth Science Institute, Slovak Academy of Sciences, Slovakia 2012-12-01
Series:Contributions to Geophysics and Geodesy
Subjects:
applied geophysics, magnetometry, gravimetry, geothermics, carbonate complexes, neogene volcanism, flysch sediments, outer carpathians
Online Access:https://journal.geo.sav.sk/cgg/article/view/78

Internet

https://journal.geo.sav.sk/cgg/article/view/78

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