Strymon and Strymonikos Gulf basins (Northern Greece): Implications on their formation and evolution from faulting

• Published in: Journal of geodynamics 2011-04, Vol.51 (4), p.285-305
• Main Author: Tranos, Markos D.
• Format: Article
• Language: English
• Subjects: Fault kinematics; Late-stage collision; Stress tensors; Transpressional s.l. tectonics; Wrench tectonics
• ISSN: 0264-3707
• DOI: 10.1016/j.jog.2010.10.002

▶ Stress-inverse methods for finding deformational path. ▶ Deformation of elastic material with “no memory”—co-axial stress and strain axes. ▶ Finding stress regime from heterogeneous fault-slip data. ▶ Wrench tectonics responsible for Strymon basin in the Hellenic hinterland. In Central and Eastern Macedonia of Northern Greece large NW–SE trending basins filled up mainly with terrestrial sediments developed during the Neogene over the Alpine basement rocks. Among them, the Strymon basin was established along the NNW–SSE trending Strouma/Strymon Lineament which formed over the tectonic boundary of the Serbomacedonian and Rhodope massifs, both representing the hinterland of the Hellenic orogen. The present study suggests that the Strymon basin was not formed as a syn-detachment basin over the Strymon Valley Detachment Fault, considered to have caused exhumation of the Rhodope massif metamorphic complex. Instead, transpressional s.l. tectonics dominated the region in the Late Oligocene-Early Miocene and it progressively changed into a wrench tectonics under which the Strymon basin has been initiated in the Middle Miocene. The basin continued to develop further under a short-lived NW–SE extension in the Middle-Late Miocene. The whole deformation is attributed to the late-stage collisional processes between the Apulia and Eurasia plates. The prevalent NE–SW extension has been constrained later on in the Late Miocene and Pliocene times activating both low-angle and high-angle NW–SE trending faults and causing the regional tilting towards the SW of the mountain fault blocks (i.e., mountain chains). From Quaternary onwards, the Strymon basin has been separated from the Strymonikos Gulf basin due to an N–S extension that mainly activates E–W striking normal faults.