Application of Experimental Configurations of Seismic and Electric Tomographic Techniques to the Investigation of Complex Geological Structures
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| Pubblicato in: | Geosciences vol. 14, no. 10 (2024), p. 258 |
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MDPI AG
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| 100 | 1 | |a Gkosios, Vasileios |u Geophysical Laboratory, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece; <email>vgkosios@geol.uoa.gr</email> (V.G.); <email>jalexopoulos@geol.uoa.gr</email> (J.D.A.); <email>sdilalos@geol.uoa.gr</email> (S.D.); <email>dimitrios.michelioudakis@gmail.com</email> (D.M.); <email>voulgaris@geol.uoa.gr</email> (N.V.) | |
| 245 | 1 | |a Application of Experimental Configurations of Seismic and Electric Tomographic Techniques to the Investigation of Complex Geological Structures | |
| 260 | |b MDPI AG |c 2024 | ||
| 513 | |a Journal Article | ||
| 520 | 3 | |a The main purpose of this study is the subsurface investigation of two complex geological environments focusing on the improvement of data acquisition and processing parameters regarding electric and seismic tomographic techniques. Two different study areas, in central–east Peloponnese and SE Attica, were selected, where detailed geological mapping and surface geophysical survey were carried out. The applied geophysical survey included the application of electrical resistivity tomography (ERT), seismic refraction tomography (SRT) and ground penetrating radar (GPR). The geoelectrical measurements were acquired with different arrays and electrode configurations. Moreover, various types of seismic sources were used at seventeen shot locations along the seismic arrays. For the processing of geoelectrical data, clustered datasets were created, increasing the depth of investigation and discriminatory capability. The seismic data processing included the following: (a) the creation of synthetic models and seismic records to determine the effectiveness and capabilities of the technique, (b) spectral analysis of the seismic records to determine the optimal seismic source type and (c) inversion of the field data to create representative subsurface velocity models. The results of the two techniques successfully delineated the complex subsurface structure that characterizes these two geological environments. The application of the ERT combined with the SRT are the two dominant, high-resolution techniques for the elucidation of complex subsurface structures. | |
| 653 | |a Subsurface investigations | ||
| 653 | |a Data acquisition | ||
| 653 | |a Tomography | ||
| 653 | |a Geological mapping | ||
| 653 | |a Geological structures | ||
| 653 | |a Electrical resistivity | ||
| 653 | |a Spectral analysis | ||
| 653 | |a Metamorphism | ||
| 653 | |a Arrays | ||
| 653 | |a Configurations | ||
| 653 | |a Velocity | ||
| 653 | |a Geoelectricity | ||
| 653 | |a Geological surveys | ||
| 653 | |a Seismic arrays | ||
| 653 | |a Geophysics | ||
| 653 | |a Seismological data | ||
| 653 | |a Seismic refraction | ||
| 653 | |a Algorithms | ||
| 653 | |a Process parameters | ||
| 653 | |a Seismic activity | ||
| 653 | |a Data processing | ||
| 653 | |a Geophysical surveys | ||
| 653 | |a Fault lines | ||
| 653 | |a Radar arrays | ||
| 653 | |a Spectrum analysis | ||
| 653 | |a Data analysis | ||
| 653 | |a Lithology | ||
| 653 | |a Seismic surveys | ||
| 653 | |a Radar | ||
| 653 | |a Geology | ||
| 653 | |a Seismic data processing | ||
| 653 | |a Seismograms | ||
| 653 | |a Ground penetrating radar | ||
| 653 | |a Surveys | ||
| 653 | |a Geologic mapping | ||
| 653 | |a Seismic data | ||
| 700 | 1 | |a Alexopoulos, John D |u Geophysical Laboratory, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece; <email>vgkosios@geol.uoa.gr</email> (V.G.); <email>jalexopoulos@geol.uoa.gr</email> (J.D.A.); <email>sdilalos@geol.uoa.gr</email> (S.D.); <email>dimitrios.michelioudakis@gmail.com</email> (D.M.); <email>voulgaris@geol.uoa.gr</email> (N.V.) | |
| 700 | 1 | |a Soukis, Konstantinos |u Section of Dynamic Tectonic and Applied Geology, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece; <email>soukis@geol.uoa.gr</email> | |
| 700 | 1 | |a Ioannis-Konstantinos Giannopoulos |u Geophysical Laboratory, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece; <email>vgkosios@geol.uoa.gr</email> (V.G.); <email>jalexopoulos@geol.uoa.gr</email> (J.D.A.); <email>sdilalos@geol.uoa.gr</email> (S.D.); <email>dimitrios.michelioudakis@gmail.com</email> (D.M.); <email>voulgaris@geol.uoa.gr</email> (N.V.) | |
| 700 | 1 | |a Dilalos, Spyridon |u Geophysical Laboratory, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece; <email>vgkosios@geol.uoa.gr</email> (V.G.); <email>jalexopoulos@geol.uoa.gr</email> (J.D.A.); <email>sdilalos@geol.uoa.gr</email> (S.D.); <email>dimitrios.michelioudakis@gmail.com</email> (D.M.); <email>voulgaris@geol.uoa.gr</email> (N.V.) | |
| 700 | 1 | |a Michelioudakis, Dimitrios |u Geophysical Laboratory, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece; <email>vgkosios@geol.uoa.gr</email> (V.G.); <email>jalexopoulos@geol.uoa.gr</email> (J.D.A.); <email>sdilalos@geol.uoa.gr</email> (S.D.); <email>dimitrios.michelioudakis@gmail.com</email> (D.M.); <email>voulgaris@geol.uoa.gr</email> (N.V.) | |
| 700 | 1 | |a Voulgaris, Nicholas |u Geophysical Laboratory, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece; <email>vgkosios@geol.uoa.gr</email> (V.G.); <email>jalexopoulos@geol.uoa.gr</email> (J.D.A.); <email>sdilalos@geol.uoa.gr</email> (S.D.); <email>dimitrios.michelioudakis@gmail.com</email> (D.M.); <email>voulgaris@geol.uoa.gr</email> (N.V.) | |
| 700 | 1 | |a Sphicopoulos, Thomas |u Department of Informatics and Telecommunications, National and Kapodistrian University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece; <email>thomas@di.uoa.gr</email> | |
| 773 | 0 | |t Geosciences |g vol. 14, no. 10 (2024), p. 258 | |
| 786 | 0 | |d ProQuest |t Publicly Available Content Database | |
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