Šujan, M., Braucher, R., Mandic, O., Fordinál, K., Brixová, B., Kyška Pipík, R., Šimo, V., Jamrich, M., Rybár, S., Klučiar, T., Ruman, A., Zvara, I., Kováč, M., 2021: Lake pannon transgression onthe westernmost tip of the carpathians constrained by biostratigraphy and authigenic 10be/9be dating (central Europe). Rivista Italiana di Paleontologia e Stratigrafia, roč. 127, č. 3, s. 627-653

Šamajová,L., Hók, J., Csibri, T., Bielik, M., Teťák, F., Brixová, B., Sliva, Ľ., Šály, B., 2019: Geophysical and geological interpretation of the vienna basin pre-neogene basement (Slovak part of the Vienna Basin). Geologica Carpatica, roč. 70, č. 5, s. 418-431

Kušnirák, D., Hermann, Z., Bielik, M., Putiška, R., Mojzeš, A., Brixová, B., Pašteka, R., Dostál, I., Zahorec, P., Papčo, J., Hók,J., Bošanský, M., Krajnak, M., 2020: Physical properties of Hradiste border fault (Turiec Basin, Western Carpathians, Slovakia) inferred by multidisciplinary geophysicalapproach. Geologica Carpathica, roč. 714, č. 1, s. 1335-0552

Brixová, B., Mosná, A., Mojzeš, A., 2018: Geophysical research of the Western Carpathians faults - Sološnica (case study). EGRSE, roč.25, č. 2, s. 12-19

Brixová, B., Putiška, R., Dostál, I., Bednarik, M., 2018: Využitie plytkého geofyzikálneho prieskumu pri posudzovaní vápencového podložia v bývalom kameňolome /Shallow geophysical survey in reviewing of the limestone massif bedrock in the former stone quarry. EGRSE, roč. 25, č. 1, s. 33-39.

Šujan, M., Braucher, R., Mandic, O., Fordinál, K., Brixová, B., Kyška Pipík, R., Šimo, V., Jamrich, M., Rybár, S., Klučiar, T., Ruman, A., Zvara, I., Kováč, M., 2021: Lake pannon transgression onthe westernmost tip of the carpathians constrained by biostratigraphy and authigenic 10be/9be dating (central Europe). Rivista Italiana di Paleontologia e Stratigrafia, roč. 127, č. 3, s. 627-653

Šamajová,L., Hók, J., Csibri, T., Bielik, M., Teťák, F., Brixová, B., Sliva, Ľ., Šály, B., 2019: Geophysical and geological interpretation of the vienna basin pre-neogene basement (Slovak part of the Vienna Basin). Geologica Carpatica, roč. 70, č. 5, s. 418-431

Kušnirák, D., Hermann, Z., Bielik, M., Putiška, R., Mojzeš, A., Brixová, B., Pašteka, R., Dostál, I., Zahorec, P., Papčo, J., Hók,J., Bošanský, M., Krajnak, M., 2020: Physical properties of Hradiste border fault (Turiec Basin, Western Carpathians, Slovakia) inferred by multidisciplinary geophysicalapproach. Geologica Carpathica, roč. 714, č. 1, s. 1335-0552

Lačný, A., Putiška, R., Vojtko, R., Dušeková, L., Mojzeš, A., Brixová, B., Zvara, I., Andrássy, E., Magdolen, P., 2021: Study of dolines of the Cajla Karst originated on covered karst landform (Malé Karpaty Mts., Western Carpathians). Acta Geologica Slovaca. roč. 13, č. 2, s. 177-190.

Pašteka, R., Hajach, M., Brixová, B., Mikuška, J., Stanley, J., 2021: Real magnetic stripping method in unexploded ordnance detection andremediation - a case study from Rohoznk military training range in SW Slovakia. Contributions to Geophysics and Geodesy.roč. 51, č. 3, s. 277-294.

Samajova L., Hok J., Csibri T., Bielik M., Tesak F., Brixova B., Sliva L., Saly B., 2019: Geophysical and geological interpretation of the vienna basin pre-neogene basement (Slovak part of the Vienna Basin). Geologica Carpathica, 70 (5) , pp. 418-431. citation: Sujan, M., Rybar, S., Thamo-Bozso, E., Kluciar, T., Tibensky, M., Sebe, K., 2022.: Collapse wedges in periglacial eolian sands evidence Late Pleistocene paleoseismic activity of the Vienna Basin Transfer Fault (western Slovakia). Sedimentary Geology, Vol. 2022, No. 431 (106103)

Samajova L., Hok J., Csibri T., Bielik M., Tesak F., Brixova B., Sliva L., Saly B., 2019: Geophysical and geological interpretation of the vienna basin pre-neogene basement (Slovak part of the Vienna Basin). Geologica Carpathica, 70 (5) , pp. 418-431. citation: Szanyi, G., Gráczer, Z., Balázs, B., Kovács, I.J. , 2021: The transition zone between the Eastern Alps and the Pannonian basin imaged by ambient noise tomography. Tectonophysics 805,228770.

Brixová, B., Mosná, A., Putiška, R. , 2018: Applications of Shallow Seismic Refraction Measurements in the Western Carpathians (Slovakia): Case Studies. Contributions to Geophysics and Geodesy,48(1), pp. 1–21. citation: Md Yunus,M.A., Mohd Khairi, M.T., Ibrahim, S., 2020: Narrow Band Vibration Measurement System with Electrodynamic Transducer Seismograph and Modeling Verification. IEEE Sensors Journal 20(9),8960294, pp. 4768-4777.

Brixová, B., Mosná, A., Putiška, R. , 2018: Applications of Shallow Seismic Refraction Measurements in the Western Carpathians (Slovakia): Case Studies. Contributions to Geophysics and Geodesy,48(1), pp. 1–21. citation: Modified satellite remote sensing technique for hydrocarbon deposit detection. Emetere, M.E. (2019),Journal of Petroleum Science and Engineering,181,106228

Brixová, B., Mosná, A., Putiška, R. , 2018: Applications of Shallow Seismic Refraction Measurements in the Western Carpathians (Slovakia): Case Studies. Contributions to Geophysics and Geodesy,48(1), pp. 1–21. Blazej, P., Julian, K., Martin, K., Ivan, B. 2022: A Method to Reduce the Impact of Technical Seismicity Generated by Blasting on Natural Objects (Case Study of the Gombasek Quarry). International Journal of ExplorationGeophysics, Remote Sensing and Environment, Vol. 29, No. 2, s. 56-69.

APVV-16-0146 (2017-2021, co-investigator) "Multidisciplinary research of geophysical and structural parameters, and environmental impacts of faults of the Western Carpathians". Annotation: To localize the trace and to identify some spatial, structural, physical, dynamic and age parameters of selected dislocations using combination of multidisciplinary field research methods. The faults are mapped by geophysical field survey methods and investigated structurally and some of them will be dated. The recent activity of the faults is monitored by measurements of seismic events and by periodical geodetic measurements based on GNSS technology. First time, for the detection of recent vertical movement along specific fault (the Vikartovce fault in the Tatra region), the very accurate measurements of gravity values and satellite radar interferometry will be applied in the Western Carpathians.

APVV-19-0150 (2020-2024, co-investigator) "New Bouguer anomaly map of the Alpine-Carpathian area: a tool for gravity and tectonic applications." Annotation: Exact calculation of the complete Bouguer anomalies (CBA) plays an important role in applied gravimetry, whereas these serve as the main input into geological, structural and tectonic interpretation (in CBA maps all non-geological influences – mainly the manifestation of relief - are suppresed and the density inhomogeneities in lithosphere structure are displayed). The team of investigators of the submitted project was invited in the frame of an European initiative (AlpArray Gravity Research Group) with the aim to create a new map of CBA from the Alpine-Carpathian area. Up to day published solutions, coming from the so-called „Slovak gravimetric school“ (e.g.: reambulation of gravimetric databases on the national level, calculation of near and distant topographic effects, regularized, transformations of potential fields, 3D complex density modelling with the introduction of the geological corrections, stripping of gravimetric fields) could be further developed and applied during the tectonic interpretation of the new CBA map from the Alpine-Carpathian region with the aim to improve the knowledge about Alpine orogenesis and its relation to the upper-mantle dynamics. As a part of the project, there are planned also verification field measurements, which can contribute to the improvement of the precision of the gravimetrical dataset of the Alpine-Carpathian area. Project has chance to develop the methodics of CBA calculation in high-mountains environment using the concept of ellipsoidal heights and to deliver to other experts an unique new gravimetric map from the region of Western and Central Europe. Main output of the project will be the new CBA map from the Alpine-Carpathian region in a digital format (grid 4x4 km), which will be provided for a realisation of gravimetric, geodynamic, exploration, geothermal and other studies and researches. Additional outputs of the project will be the transformed maps (grids) of CBA field.

APVV 21-0159 (2024 - 2026, co-investigator) "Atlas of Tectonic Dislocations of the Earth´s Crust in the Territory of Slovakia." Annotation:The knowledge of tectonic dislocations (faults) is essential for various areas of economic activity (e.g. largetransport constructions, dams, nuclear power plants, mineral exploration and exploration of geothermal waters),land it has an impact on environmental issues (e.g. seismic risks, slope deformations, sites for radioactive waste storage). The systematic processing of data on the dislocations of crust in Slovakia in the form of a comprehensive monograph is highly needed. This is the aim of our DISLOCAT project. Based on the excerption of available published and archived data, all significant tectonic dislocations of crust will be characterized according to uniform criteria. We will focus on the faults from the youngest Neoalpine tectonic development, many of which are still active today. The basic parameters of the faults will include the manifestations of the faults in the geological map and/or aerial and satellite images, its course, inclination and depth, thickness of the disturbed zone, structural data and kinematics, age, seismicity, available geodetic measurements of recent movements, geomorphological manifestations and springs of water or emanations. Great attention will be paid to seismoactive fault zones. The information about selected faults will be collected and made more precise by field research into the geological structure and geophysical, mainly magnetotelluric measurements. Here, the project builds on the methodology of fault research, which was tested in the recently completed APVV WECAFARE project, which was focused mainly on the creation of a methodology to examine the faults and tested in the selected faults in Slovakia. The characteristics of faults will be supplemented by geological sections or photo documentation. The monograph – a catalog of tectonic dislocations with a map of faults in printed and electronic (GIS) version – will be the project output.

VEGA grant 1/0559/17 (2017 - 2019, co-investigator) "Application of seismic measurements in landslide areas, principal investigator." Annotation: Project was focused on the study of mechanical properties of rocks, which can be derived from shallow refraction seismic measurements in the case of landslides.

VEGA 1/0107/23 (co-investigator 2023 - 2026) "Integrated geophysical and geological detection of the Vikartovce and Muráň fault lines and characterization of their parameters combined with morphotectonic and structural analysis and fault filling dating (Hornádska kotlina Basin, Levočské vrchy Mts.)." Annotation: The detection of accurate fault route, its spatial orientation, depth, width, character and filling age based on geophysical and geological methods application.

VEGA 1/0180/24 (2024 - 2027, co-investigator ) "Application and evaluation of the results of multifunctional analysis of surface seismic waves (MASW) in geological engineering and geotechnical tasks." Annotation: The nature of the project is to create a methodology for obtaining geotechnical parameters of the environment using seismic methods (mainly MASW). Geotechnical parameters are used in engineering geological, geotechnical, or environmental tasks. Now they are mainly gained from laboratory tests performed on field samples from drilling. This approach is spot-based and requires drilling.Therefore, it is important to have other options available. This option can be dependence of geotechnical modules on the seismic velocities. Seismic measurements enable to obtain values of geotechnical parameters over the entire length of the measured profile. This methodology can minimize the possibility of obtaining an unrepresentative drilling sample and also reduce the amount of drilling works, especially in areas with difficult approach. The ambition of the project is to correlate the results obtained from seismic measurements with the results of field engineering geological tests as well as laboratory tests.