STRUCTURAL-KINEMATIC INTERPRETATION OF SMALL-AMPLITUDE TECTONIC DEFORMATIONS SPREAD WITHIN SABURTALO SYNCLINE AND LISI ANTICLINE

Authors

DOI:

https://doi.org/10.52340/pajig.2024.136.06

Keywords:

tectonic deformation, kinematics, faults

Abstract

Of the existing deformation structures identified by us within the Saburtalo syncline and Lisi anticline, small faults of latitudinal and meridional strike prevail, which by their kinematics correspond to upcast and downcast faults. Several gentle faults are noted across  the pitch of layers, which then pass into folded deformations. All these deformations point to the leading role of north-directed vectors of horizontal compression and at the same time, since their intensity increases to the east, it is thought to be caused by the dynamic influence of the Tbilisi meridional deep fault on a certain area.

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Author Biographies

Levan Basheleishvili, Tbilisi State University

Candidate of Geologic-Mineralogical Sciences, Senior Researcher of Department of Regional Geology and Tectonics of Alexandre Janelidze Institute of  Geology of  Ivane Javakhishvili Tbilisi State University.

Giorgi Beridze, Tbilisi State University

PhD of Geology, Senior Scientist of Complex Laboratory of Geological Research of Alexandre Janelidze Institute of Geology of Ivane Javakhishvili Tbilisi State University.

Mariam Kumelashvili, Georgian Technical University

PhD, Assistant professor of Department of oil and gas technology of Georgian Technical university.

Gvantsa Kanchashvili, Tbilisi State University

Master Student, Department of Geology of Faculty of Exact and Natural Sciences of Ivane Javakhishvili Tbilisi State University.

References

Basheleishvili L., Gabarashvili K. (2022). Structural-kinematic interpretation of secondary horizon¬tal and parasitic folds. Proc Al. Janelidze Institute of Geology, vol. 134, pp. 80-87 (in Georgian).

Devdariani E.I. (1971). Geology and oil and gas potential of the eastern subsidence of the Adjara-Tria¬le¬ti folded system. Diss. for candidate of geol- miner. sci. Geol. Inst., pp. 1-143. (in Russian).

Gamkrelidze I., Nadareishvili G., Tsamalashvili T., Basheleishvili L., Nadareishvili S. (2008). On Ge¬nesis of Tbilisi olistostromes. Proc. Al. Janelidze Institute of Geology, vol. 124, pp. 24-29.

Gamkrelidze I., Tsamalashvili T., Nikolaeva E., Godoladze T., Javakhishvili Z., Elashvili M. (2008). Tbilisi Fault and seismic activity of Tbilisi environs (Georgia). Proc. Al. Janelidze Institute of Geology, vol. 124, pp. 30-35.

Laliev A.G. (1964). Maikop series of Georgia. “Nauka”, Moscow, pp. 1-295 (in Russian).

Papava D., Devdariani E., Ageev V. (1971). The results of geological survey works and structural drilling within the eastern subduction of the Adjara-Trialeti folded system. Geological report according to the works of 1968-1970, 209 p. in Russian.

Patalakha E.I. (1985). Tectonofacies analysis of folded structures of the Phanerozoic. “Nedra”, Moscow, pp. 1-168 (in Russian).

Sherman S.I., Bornyakov S.F., Buddo V.Yu. (1983). Areas of dynamic influence of faults (mode-ling results). “Nauka”, Moscow, pp. 1-112 (in Russian).

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Published

2024-12-11

How to Cite

Basheleishvili, L., Beridze, G., Kumelashvili, M., & Kanchashvili, G. (2024). STRUCTURAL-KINEMATIC INTERPRETATION OF SMALL-AMPLITUDE TECTONIC DEFORMATIONS SPREAD WITHIN SABURTALO SYNCLINE AND LISI ANTICLINE. Proceedings of Alexandre Janelidze Institute of Geology of I. Javakhishvili Tbilisi State University, (136), 68–77. https://doi.org/10.52340/pajig.2024.136.06

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