Associate Professor,Department of Geosciences
Telephone: +971 (0)2 60 75761
Sotirios Kokkalas is currently an Associate Professor in Structural Geology at the Petroleum Institute (PI), Khalifa University of Science and Technology, in Abu Dhabi. From the start of his academic career and for a decade (2003-2013) he lectured several courses and conducted research on the brittle deformation of the upper Aegean crust at the University of Patras (Greece). As a pure field geoscientist, he led several field trips on various tectonic settings in Europe and the Middle East. During 2006-2007 he was a visiting researcher at the Rock Fracture project in Stanford University, California (USA), where he participated in several field trips in Nevada and California. His main research interests are in the area of brittle and ductile faulting and fracturing in the upper crust with applications to the oil and gas industry, orogenic evolution of fold-and-thrust belts, strike-slip tectonics, magmatic intrusions, tectonic geomorphology and earthquake geology-paleoseismology.
During his academic career he has published numerous articles in peer reviewed journals and conference proceedings on various research subject areas such as, fracture and fault zone analysis, strain analysis of shear zones, orogenic deformation, active tectonics and paleoseismology. He also delivered several presentations and invited talks in international conferences and workshops and is the co-author of two books on Earthquake Geology and Geodynamics-Plate Tectonics for Greek university students. Furthermore, he serves as a reviewer for a great number of high-impact international journals in the area of Earth Sciences and Geodynamics. He is member of several professional organizations (GSA, AGU, EAGE etc.)
- PGEG230 Geological Maps
- PGEG321 Structural Geology
- PGEG397 Field Petroleum Geology
- PGEG394, 471 Special and Research topics in Petroleum Geosciences
- Research projects“Magnetic Nanoparticles (MNPs) for Reservoir Characterization”“Fracture Characterization and fold-fracture relationships from the combination of LiDAR high resolution topographic data and outcrop analog data”“Scaling effect of fracture distribution on heterogeneity and anisotropy in carbonate rocks”Research Interests
- Fault/fracture geometry, fault/fracture interaction and linkage
- Orogenic evolution of fold-and-thrust belts and strike-slip tectonics
- Active faulting, seismotectonics, Earthquake geology
- Bruno PPG, DuRoss CB, Kokkalas S*. High-resolution seismic profiling reveals faulting associated with the 1934 Ms 6.6 Hansel Valley earthquake (Utah, USA). GEOLOGICAL SOCIETY OF AMERICA BULLETIN 2017: https://doi.org/10.1130/B31516.1
- Wilkinson MW, Jones RR, Woods CE, Gilment SR, McCaffrey KJW, Kokkalas S*, Long JJ.A Comparison of Terrestrial Laser Scanning and Structure-from-Motion Photogrammetry as Methods for Digital Outcrop Acquisition.GEOSPHERE2016:12; 6, 1-16.
- Zygouri V, Koukouvelas I, Kokkalas S*, Xypolias P, Papadopoulos G. The Nisi fault as a key structure for understanding the active deformation of the NW-Peloponnese, Greece. Geomorphology 2015: 237; 142-156.
- Chatzaras V, Xypolias P, Kokkalas S*, Koukouvelas I. Tectonic evolution of a crustal-scale oblique ramp, Hellenides thrust belt, Greece. Journal of Structural Geology 2013: 57; 16-37.
- Kokkalas S*, Aydin A. Is there a link between faulting and magmatism in south-central Aegean Sea? Geological Magazine 2013: 150 (2); 193-224.
- Kaplanis A, Koukouvelas I, Xypolias P, Kokkalas S*. Kinematics and ophiolite obduction in Gerania and Helicon Mountains, central Greece. Tectonophysics 2013: 595-596; 215-234.
- Kokkalas S*, Kamberis E, Xypolias P, Sotiropoulos S, Koukouvelas I. Coexistence of thin- and thick-skinned tectonics in Zakynthos area (Western Greece): insights from seismic sections and regional seismicity. Tectonophysics 2013: 597-598; 73-84.
- P. Xypolias, I.,Iliopoulos, V. Chatzaras, and S. Kokkalas*, “Subduction- and exhumation-related structures in the Cycladic Blueschists: insights from the south Evia Island (Aegean region, Greece),” Tectonics, 31 (2), art.no. TC2001, 2012.
- V. Chatzaras, P. Xypolias, S. Kokkalas*, and I. Koukouvelas,“Oligocene-Miocene thrusting in central Aegean: insights from the Cycladic island of Amorgos,” Geological Journal, 46, (6), 619-636, DOI: 10.1002/gj.1304, 2011.
- I. Koukouvelas, S. Kokkalas*, and P. Xypolias, “Surface deformation during the Mw 6.4 (June 08, 2008) Movri Mt earthquake, Peloponnese and its implications for the seismotectonics of Western Greece,” International Geology Review, 52, 2-3, 249-268, 2010.
- P. Xypolias, D. Spanos, V. Chatzaras, S. Kokkalas*, and I. Koukouvelas, “Vorticity of flow in ductile thrust zones: examples from the Attico-Cycladic Massif (Internal Hellenides, Greece),” Geological Society, London, Special Publication 335, “Continental Tectonics and Mountain Building”, 687-714, 2010.
- G. Pe-Piper, D.J. Piper, I. Koukouvelas, L. Dolansky, and S. Kokkalas*, “Post-orogenic shoshonitic rocks and their origin by melting underplated basalts: the Miocene of Limnos, Greece,” Geological Society of America Bulletin v. 121, p.17-38, 2009.
- Xypolias, P. Spanos D., Chatzaras, V., Kokkalas S*., Koukouvelas I., 2010 Vorticity of flow in ductile thrust zones: examples from the Attico-Cycladic Massif (Internal Hellenides, Greece). Geological Society, London, Special Publication 335, “Continental Tectonics and Mountain Building”, 687-714.
- Koukouvelas. I., Kokkalas, S*., Xypolias, P. 2010. Surface deformation during the Mw 6.4 (June 08, 2008) Movri Mt earthquake, Peloponnese and its implications for the seismotectonics of Western Greece. International Geology Review, 52, 2-3, 249-268.
- G. Pe-Piper, D.J. Piper, Koukouvelas I., Dolansky L & Kokkalas S 2009. Post-orogenic shoshonitic rocks and their origin by melting underplated basalts: the Miocene of Limnos, Greece. Geological Society of America Bulletin v. 121, p.17-38.
- Jones R.R., Kokkalas S*., McCaffrey, K.J.W.. 2009. Quantitative Analysis and Visualisation of non-planar fault surfaces using Terrestrial Laser Scanning (“LiDAR”) – the Arkitsa Fault, central Greece as a case study. Geosphere,v.5, no.6, p.465-482, doi: 10.1130/GES00216.1
- Parcharidis, I., Kokkalas, S*., Fountoulis, I., Foumelis, M., 2009. Detection and Monitoring of Active Faults in Urban Environments: Time Series Interferometry on the Cities of Patras and Pyrgos (Peloponnese, Greece). Remote Sensing, 1, 676-696; doi: 103390/rs1040676
- Zygouri,V., Verroios, S., Kokkalas,S*., Xypolias, P., Koukouvelas.I., 2008 Scaling properties within the Gulf of Corinth; (Greece) comparison between onshore and offshore active faults. Tectonophysics 453, (1-4), 193-210.
- Kokkalas S*., Jones R.R., McCaffrey K.J.W., Clegg P. 2007. Quantitative fault analysis at Arkitsa, Central Greece, using terrestrial Laser-Scanning (LiDAR). Bulletin of the Geological Society of Greece, vol. XXXX, 1959-1972.
- Kokkalas, S*., Pavlides, S., Koukouvelas, I., Ganas, A., Tsodoulos I., Stamatopoulos, L., Gountromichou, C., Valkaniotis S. 2007 Preliminary Palaeoseismological results from Kapareli Fault (Central Greece): evidence of seismic events for the past 10.000 years. Hellenic Journal of Geoscience vol.42, 65-74.
- Kokkalas S*., Pavlides, S., Koukouvelas, I., Ganas, A., & Stamatopoulos, L., 2007. Paleoseismicity of the Kaparelli Fault (Eastern Corinth gulf): Evidence for Earthquake Recurrence and Fault Behavior. Bollettino della Societa Geologica Italiana, 126 (2), 387-395.
- Xypolias P., Kokkalas S*. (2006). Heterogeneous ductile deformation along a mid-crustal extruding shear zone: an example from External Hellenides (Greece). Geological Society of London, Special Publ., 268, 497-516.
- Kokkalas S*. Xypolias P. Koukouvelas I. Doutsos T. (2006) Post-Collisional Contractional and Extensional Deformation in the Aegean region. In: Dilek. Y. Pavlides S (eds) Post Collisional Tectonics & Magmatism in the Mediterranean Region and Asia,. Geological Society of America Special Paper, 97-123
- Pavlides, S., Caputo R., Koukouvelas I., Kokkalas S*. and Chatzipetros A. (2005) Paleoseismological investigation of the Aegean-type active faults. In: Dilek. Y. Pavlides S (eds) Post Collisional Tectonics & Magmatism in the Mediterranean Region and Asia. Geological Society of America Special Paper,175-188.
- Kokkalas S*., Koukouvelas IK. (2005) Fault-scarp degradation modeling in central Greece: the Kaparelli and Eliki faults (Gulf of Corinth) as a case example. Journal of Geodynamics 40 (2-3), 200-215.
- Chatzipetros A., Kokkalas S*., Pavlides SB, Koukouvelas IK.(2005). Palaeoseismic data and their implication for active deformation in Greece. Journal of Geodynamics 40 (2-3), 170-188.
- Kokkalas, S*., Doutsos, T. 2004. Kinematics and strain partitioning in the southeast Hellenides, Greece. Geological Journal 39, (2), 121-140.
- Pavlides, S., Koukouvelas, I., Kokkalas, S*., Stamatopoulos, L., Keramydas D., Tsodoulos I. 2003. Late Holocene evolution of the East Eliki fault, Gulf of Corinth (Central Greece). Quaternary International 115, 139-154.
- Xypolias, P., Kokkalas, S*., Skourlis, K., (2003). Upward extrusion and subsequent transpression as a possible mechanism for the exhumation of HP/LT rocks in Evia Island (Aegean Sea, Greece). Journal of Geodynamics 35, 303-332.
- Koukouvelas, I., Kokkalas, S*. (2003). Emplacement of the Miocene west Naxos pluton, (Aegean Sea, Greece): a structural study. Geological Magazine 140, 45-61.
- Kokkalas, S*., Xypolias, P., Koukouvelas, I., Doutsos, T. 2003. Relationships between folding and fracturing in orogenic belts: Examples from the Rhenohercynian zone (Germany) and the External Hellenides (Greece). Geologica Carpathica54 (3), 153-162.
- Kokkalas, S*., Doutsos, T. 2001. Strain-dependent stress field and plate motion in the south-east Aegean region. Journal of Geodynamics32, 311-332.
- Doutsos, T., Kokkalas, S*. 2001. Stress and deformation in the Aegean region. Journal of Structural Geology 23, 455-472.
- Doutsos, T., Koukouvelas, I., Poulimenos, G., Kokkalas, S*., Xypolias, P., Skourlis, K. 2000. An exhumation model of the south Peloponnesus, Greece. International Journal of Earth Sciences 89, 350-365.