Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review

Shyqyri Aliaj

doi:doi:10.11648/j.earth.20211006.20

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Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review

Shyqyri Aliaj

Published in Earth Sciences (Volume 10, Issue 6)

Received: 6 December 2021 Accepted: 28 December 2021 Published: 31 December 2021

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Abstract

The Vlora-Elbasani-Dibra transversal fault zone crosses from south-west to northeast the Albanides collision zone starting from Vlora area to the Dumre diapir and continuing from Elbasani Quaternary graben to Dibra area, within the internal Albanides extensional zone. The Vlora-Elbasani-Dibra seismogenic fault zone is expressed by an alignment of important historical and instrumental seismicity with 15 Ms > 6 earthquakes. The Vlora-Berati-Elbasani segment of this fault zone during the year 1851 has been activated along all is length. The geological and neotectonic investigations and the focal mechanism solutions of earthquakes that occurred along the Vlora-Elbasani-Dibra fault zone prove its division into two distinct fault zones: a) the Mali i Kanalit Block - Dumre diapir strike-slip fault zone NNE trending in transpression, and b) the Elbasan-Dibra normal fault zone NE trending in transtension. The Mali i Kanalit Block-Dumre diapir strike-slip zone NNE trending in transpression offsets dextrally and to SW the folds and thrusts of the Çika, Kurveleshi and Berati anticlinal belts of Ionian zone. The Neogene (mainly since Middle Miocene) offset of the Çika, Kurveleshi and Berati anticlinal belts from generally NW-SE trending to near N-S one has led to thrust’s steepening and turning into high-angle strike-slip faults due to NE-SW oblique compression from the Albanides collision zone. The Othoni Island-Dhermi strike-slip fault offsets the dextrally dragged Devolli (to the east of Dumre diapir), Osumi (near to Berati town), and Vjosa (west of Shkoza village) rivers’ valleys formed from the Middle Pleistocene (180,000 years) to historic times. The Othoni Island-Dhermi dextral strike-slip fault, that reaches the maximum velocity of greater than 5 mm/year to the south of it, is the only leading fault that shaped the Mali i Kanalit Block-Dumre diapir dextral strike-slip fault zone. Focal mechanism solutions of earthquakes that occurred on the Mali i Kanalit Block - Dumre diapir dextral strike-slip zone show their generation from strike-slip faults in transpressional motions. Focal mechanism solutions of earthquakes that occurred on the Elbasan-Dibra were generated from normal faults with dextral strike-slip movements.

Published in	Earth Sciences (Volume 10, Issue 6)
DOI	10.11648/j.earth.20211006.20
Page(s)	346-357
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2021. Published by Science Publishing Group

Keywords

Geologo-neotectonic Investigations, Mali i Kanalit-Dumre Strike-slip Zone, Focal Mechanisms

References

[1]	Aliaj, 1979. Sizmotektonika dhe kriteret gjeologjike të sizmicitetit të Shqipëriseë. Teza për gradën shkencore “Kandidat i Shkencave”, Fakulteti Gjeologji-Miniera, Universiteti i Tiranës.
[2]	Aliaj, 1989. The main seismoactive faults in Albania. Proc. Gen. Ass. of ESC Sofia, 36-47.
[3]	Aliaj, 1996a. Zonimi neotektonik i Shqipërisë. Në: Aliaj et al. 1996, Kap. VIII.
[4]	Aliaj, 1996b. Neotectonics and Seismotectonics of Drini fault zone (Eastern Albania). Jour. Nat. Tech. Sci. Albania, 1: 81-93.
[5]	Aliaj, 1997. Alpine geological evolution of Albania. Albanian Jour. Nat. Tech. Sci., Acad. Sci. Albania, 3: 69-82.
[6]	Aliaj, 1998. Neotectonic structure of Albania. J. Nat. Tech. Sci., Acad. Sci. Albania, 4: 15-42.
[7]	Aliaj, 1999. Transverse Faults in Albanian Orogen Front. J. Nat. Tech. Sci., Acad. Sci. Albania, 6; 34-46.
[8]	Aliaj, 2000a. Map of active faults in Albania in scale 1: 200,000. In: 8^th Congress of Albanian Geosciences, November 6-8, 2000 in Tirana. Abstract Book, poster presentation with short text in page 267.
[9]	Aliaj, 2000b. Neotectonics and Seismicity. In: Meço S, Aliaj Sh, 2000. Geology of Albania. Scientific Publisher Gebruder Borntraeger. Berlin. Stuttgart 2000.
[10]	Aliaj, 2004. Seismic source zones in Albania. In: Kirazi and Muco (eds) NATO Science for Peace Programme, Final Report, Project “Seismotectonics and seismic hazard assessment in Albania” March 2004.
[11]	Aliaj, 2006. The Albanian Orogen: Convergence zone between Eurasia and the Adria microplate. N. Pinter et al. (eds.), The Adria Microplate: GPS Geodesy, Tectonics and Hazards. 2006 Springer. Printed in the Netherlands.
[12]	Aliaj, 2012. Neotektonika e Shqipërisë, 292 faqe. Shtypur dhe botuar nga KLEAN Tiranë.
[13]	Aliaj, 2020. Seismotectonics of the Albanides Collision Zone: Geometry of the Underthrusting Adria Microplate. J. Nat. Tech. Sci., Acad. Sci. Albania, 2 (2020): 1-40.
[14]	Aliaj et al., 1995, printed 2018. Harta Neotektonike e Shqipërisë (tokë e det) në shkallë 1: 200,000. Botimi i Sherbimit Gjeologjik Shqiptar 2018.
[15]	Aliaj et al., 1996. Struktura Neotektonike e Shqipërisë dhe Evolucioni Gjeodinamik i saj, 497 faqe. Instituti Sizmologjik Tiranë.
[16]	Aliaj et al., 2000. Seismotectonic Map of Albania in scale 1: 500,000. Archive of Institute of Seismology, Tirana, Albania.
[17]	Aliaj and Pojani, 2003. Tërmeti i 24 prillit 2002 Gjilan, Kosovë. Revista ”Ndërtuesi”, Nr. 5, Dhjetor 2002, Supplement, 3-23.
[18]	Aliaj et al., 2010, 2020 (reprinted). Sizmiciteti, Sizmotektonika dhe vlerësimi i rrezikut sizmik në Shqipëri, 317 faqe. Akademia e Shkencave e Shqipërisë. Shtypur në Shtypshkronjën “Kristalina KH” Tiranë.
[19]	Aliaj and Kodra, 2016. Albanides Setting in the Dinaric-Albanian-Hellenic Belt and Their Geological Features. J. Nat. Tech. Sci., Acad. Sci. Albania, 2 (2016): 31-73.
[20]	Arsovski, 1997. Tektonika na Makedonia. Rudarsko-Geoloshki Fakultet, Shtip, 1997.
[21]	Baker et al., 1997. Earthquake mechanisms of the Adriatic Sea and Western Greece. Geophys. J. Int. 131, 559-594.
[22]	Carcaillet et al., 2009. Uplift and active tectonics of southern Albania inferred from incision of alluvial terraces. Quaternary Research 71 (2009) 465-476.
[23]	Dumurdzanov et al., 2005. Cenozoic tectonics of Macedonia and its relation to the South Balkan extensional regime. Geosphere, v. 1, no 1, 1-22.
[24]	Elezaj, 2002. Karakteristikat sizmotektonike të Kosovës si bazë për rajonizimin sizmik të saj. Teza për gradën shkencore “Doktor i Shkencave”. Universiteti Politeknik i Tiranës, Fakulteti Gjeologji-Miniera, Tiranë.
[25]	Elezaj, 2009. Cenozoic Molasse Basins in Kosova and their Geodynamic Evolution. Muzeul Olteniei Craiova. Oltenia Studii şi Comunicari Ştiintele Naturii Craiova, 25, 348-349.
[26]	Handy et al., 2019. Coupled Crust-Mantle Response to Slab Tearing, Bending, and Rollback Along the Dinaride-Hellenide Orogen. Tectonics 38: 1-26.
[27]	Jouanne et al., 2012. GPS constraints on current tectonics of Albania. Tectonophysics 554-557 2012), 50-62.
[28]	Kiratzi, 2011. The September 2009 Mw 5.4 earthquake in Eastern Albania-FYROM border: Focal Mechanism, Slip Model, ShakeMap. Turkish Journal of Earth Sciences, 20: 475-488.
[29]	Koçi, 2008. Pasqyrimi i lëvizjeve të reja tektonike në taracat e lumejve të vendit tonë. Disertacion për gradën shkencore “Doktor i Shkencave”. Instituti i Sizmologjisë Tiranë.
[30]	Meço and Aliaj, 2000. Geology of Albania. Scientific Publisher Gebruder Borntraeger. Berlin. Stuttgart 2000.
[31]	Melo and Aliaj, 2009. Thyerjet tërthore në Shqipëri. Fjalori Enciklopedik Shqiptar, Akademia e Shkencave e Shqipërisë, 2009, f 2780-2782.
[32]	Muço, 2007. Focal mechanism solutions and stress field distribution in Albania. Jour. Nat. Tech. Sci., 1, 129-134.
[33]	Pashko and Aliaj, 2020. Stratigraphy and Tectonic Evolution of Late Miocene-Quaternary Basins in Eastern Albania: A Review. Bulletin of Geological Society of Greece 56, 317-351.
[34]	Roore et al., 2004. Kinematic evolution and petroleum systems – an appraisal of outer Albanides. In: Mc Clay, K. R. (Ed.). Thrust Tectonics and Hydrocarbon Systems, 82. AAPG memoir, pp. 474-493.
[35]	Sulstarova, 1986. The focal mechanism of Albanian earthquakes and the field of actual tectonic stress in Albania. Dr. Sc. Theses, Seismological Centre, Tirana, Albania. 230 pp. (in Albanian).
[36]	Sulstarova, 1987. The focal mechanism of earthquakes and tectonic stress in Albania. Buletini i Shkencave Gjeologjike 4, 133-170.
[37]	Sulstarova and Koçiaj, 1969. The earthquake of November 30, 1967 and Vlora-Dibra seismogenetic belt. Buletini i Universitetit të Tiranës, Ser. Shk. Nat. 2, 85-95 (in Albanian).
[38]	Sulstarova and Koçiaj, 1975. Catalogue of Albanian earthquakes. Acad. of Sci. Albania. 224 pp (in Albanian).
[39]	Sulstarova and Koçiaj, 1980. The Dibra (Albania) earthquake of November 30, 1967. Tectonophysics 67, 333-343.
[40]	Sulstarova et al., 1980. Seismic Regionalization of the PSR of Albania. Seismological Centre, Academy of Sciences of Albania (In Albanian and in English). Shtypur: Kombinati Poligrafik, Shtypshkronja “Mihal Duri” Tiranë.
[41]	Sulstarova et al., 2000. Vlora-Elbasani-Dibra (Albania) transversal fault zone and its seismic activity. Journal of Seismology, 2000, 1-15.
[42]	Shallo et al., 1985, printed and published 1999. Tectonic Map of Albania Scale 1: 200,000. Printed and published in South Africa 1999. Review by Xhomo A, Kodra A, Gjata K, and Z. Xhafa (1999).
[43]	Tagari et al., 1993. Tectonique polyphaser plio-quaternaire en Albanie orientale (region Korca-Pogradeci). Bulletin de la Societe Geologique de France 164 (5), 727-737.
[44]	Velaj, 2015a. The structural style and hydrocarbon exploration of the subthrust in the Berati anticlinal Belt, Albania. J. Petrol Explor Prod Technol (2015) 5: 123-145.
[45]	Velaj, 2015b. New ideas on the tectonic of Kurveleshi anticlinal belt in Albania, and the perspective for exploration in its subthrusts. Petroleum 1 (2015) 269-288.
[46]	Xhomo et al., 1999. Geological map of Albania (1:200.000). Tirana: Ministry of Industry and Energy, Ministry of Education and Science, Albanian Geological Survey, AlbPetrol, Polytechnical University of Tirana.
[47]	Xhomo et al., 2005. Harta gjeologjike e Shqipërisë në shkallë 1: 200,000. Publishing House “Hubber kartografie”, Munich.

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Shyqyri Aliaj. (2021). Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review. Earth Sciences, 10(6), 346-357. https://doi.org/10.11648/j.earth.20211006.20

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Shyqyri Aliaj. Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review. Earth Sci. 2021, 10(6), 346-357. doi: 10.11648/j.earth.20211006.20

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Shyqyri Aliaj. Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review. Earth Sci. 2021;10(6):346-357. doi: 10.11648/j.earth.20211006.20

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@article{10.11648/j.earth.20211006.20,
  author = {Shyqyri Aliaj},
  title = {Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review},
  journal = {Earth Sciences},
  volume = {10},
  number = {6},
  pages = {346-357},
  doi = {10.11648/j.earth.20211006.20},
  url = {https://doi.org/10.11648/j.earth.20211006.20},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20211006.20},
  abstract = {The Vlora-Elbasani-Dibra transversal fault zone crosses from south-west to northeast the Albanides collision zone starting from Vlora area to the Dumre diapir and continuing from Elbasani Quaternary graben to Dibra area, within the internal Albanides extensional zone. The Vlora-Elbasani-Dibra seismogenic fault zone is expressed by an alignment of important historical and instrumental seismicity with 15 Ms > 6 earthquakes. The Vlora-Berati-Elbasani segment of this fault zone during the year 1851 has been activated along all is length. The geological and neotectonic investigations and the focal mechanism solutions of earthquakes that occurred along the Vlora-Elbasani-Dibra fault zone prove its division into two distinct fault zones: a) the Mali i Kanalit Block - Dumre diapir strike-slip fault zone NNE trending in transpression, and b) the Elbasan-Dibra normal fault zone NE trending in transtension. The Mali i Kanalit Block-Dumre diapir strike-slip zone NNE trending in transpression offsets dextrally and to SW the folds and thrusts of the Çika, Kurveleshi and Berati anticlinal belts of Ionian zone. The Neogene (mainly since Middle Miocene) offset of the Çika, Kurveleshi and Berati anticlinal belts from generally NW-SE trending to near N-S one has led to thrust’s steepening and turning into high-angle strike-slip faults due to NE-SW oblique compression from the Albanides collision zone. The Othoni Island-Dhermi strike-slip fault offsets the dextrally dragged Devolli (to the east of Dumre diapir), Osumi (near to Berati town), and Vjosa (west of Shkoza village) rivers’ valleys formed from the Middle Pleistocene (180,000 years) to historic times. The Othoni Island-Dhermi dextral strike-slip fault, that reaches the maximum velocity of greater than 5 mm/year to the south of it, is the only leading fault that shaped the Mali i Kanalit Block-Dumre diapir dextral strike-slip fault zone. Focal mechanism solutions of earthquakes that occurred on the Mali i Kanalit Block - Dumre diapir dextral strike-slip zone show their generation from strike-slip faults in transpressional motions. Focal mechanism solutions of earthquakes that occurred on the Elbasan-Dibra were generated from normal faults with dextral strike-slip movements.},
 year = {2021}
}

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TY  - JOUR
T1  - Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review
AU  - Shyqyri Aliaj
Y1  - 2021/12/31
PY  - 2021
N1  - https://doi.org/10.11648/j.earth.20211006.20
DO  - 10.11648/j.earth.20211006.20
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 346
EP  - 357
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20211006.20
AB  - The Vlora-Elbasani-Dibra transversal fault zone crosses from south-west to northeast the Albanides collision zone starting from Vlora area to the Dumre diapir and continuing from Elbasani Quaternary graben to Dibra area, within the internal Albanides extensional zone. The Vlora-Elbasani-Dibra seismogenic fault zone is expressed by an alignment of important historical and instrumental seismicity with 15 Ms > 6 earthquakes. The Vlora-Berati-Elbasani segment of this fault zone during the year 1851 has been activated along all is length. The geological and neotectonic investigations and the focal mechanism solutions of earthquakes that occurred along the Vlora-Elbasani-Dibra fault zone prove its division into two distinct fault zones: a) the Mali i Kanalit Block - Dumre diapir strike-slip fault zone NNE trending in transpression, and b) the Elbasan-Dibra normal fault zone NE trending in transtension. The Mali i Kanalit Block-Dumre diapir strike-slip zone NNE trending in transpression offsets dextrally and to SW the folds and thrusts of the Çika, Kurveleshi and Berati anticlinal belts of Ionian zone. The Neogene (mainly since Middle Miocene) offset of the Çika, Kurveleshi and Berati anticlinal belts from generally NW-SE trending to near N-S one has led to thrust’s steepening and turning into high-angle strike-slip faults due to NE-SW oblique compression from the Albanides collision zone. The Othoni Island-Dhermi strike-slip fault offsets the dextrally dragged Devolli (to the east of Dumre diapir), Osumi (near to Berati town), and Vjosa (west of Shkoza village) rivers’ valleys formed from the Middle Pleistocene (180,000 years) to historic times. The Othoni Island-Dhermi dextral strike-slip fault, that reaches the maximum velocity of greater than 5 mm/year to the south of it, is the only leading fault that shaped the Mali i Kanalit Block-Dumre diapir dextral strike-slip fault zone. Focal mechanism solutions of earthquakes that occurred on the Mali i Kanalit Block - Dumre diapir dextral strike-slip zone show their generation from strike-slip faults in transpressional motions. Focal mechanism solutions of earthquakes that occurred on the Elbasan-Dibra were generated from normal faults with dextral strike-slip movements.
VL  - 10
IS  - 6
ER  -

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Shyqyri Aliaj

Department of Seismotectonics, Institute of Seismology, Academy of Sciences of Albania, Tiran?, Albania

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Shyqyri Aliaj. (2021). Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review. Earth Sciences, 10(6), 346-357. https://doi.org/10.11648/j.earth.20211006.20

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Shyqyri Aliaj. Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review. Earth Sci. 2021, 10(6), 346-357. doi: 10.11648/j.earth.20211006.20

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AMA Style

Shyqyri Aliaj. Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review. Earth Sci. 2021;10(6):346-357. doi: 10.11648/j.earth.20211006.20

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@article{10.11648/j.earth.20211006.20,
  author = {Shyqyri Aliaj},
  title = {Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review},
  journal = {Earth Sciences},
  volume = {10},
  number = {6},
  pages = {346-357},
  doi = {10.11648/j.earth.20211006.20},
  url = {https://doi.org/10.11648/j.earth.20211006.20},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20211006.20},
  abstract = {The Vlora-Elbasani-Dibra transversal fault zone crosses from south-west to northeast the Albanides collision zone starting from Vlora area to the Dumre diapir and continuing from Elbasani Quaternary graben to Dibra area, within the internal Albanides extensional zone. The Vlora-Elbasani-Dibra seismogenic fault zone is expressed by an alignment of important historical and instrumental seismicity with 15 Ms > 6 earthquakes. The Vlora-Berati-Elbasani segment of this fault zone during the year 1851 has been activated along all is length. The geological and neotectonic investigations and the focal mechanism solutions of earthquakes that occurred along the Vlora-Elbasani-Dibra fault zone prove its division into two distinct fault zones: a) the Mali i Kanalit Block - Dumre diapir strike-slip fault zone NNE trending in transpression, and b) the Elbasan-Dibra normal fault zone NE trending in transtension. The Mali i Kanalit Block-Dumre diapir strike-slip zone NNE trending in transpression offsets dextrally and to SW the folds and thrusts of the Çika, Kurveleshi and Berati anticlinal belts of Ionian zone. The Neogene (mainly since Middle Miocene) offset of the Çika, Kurveleshi and Berati anticlinal belts from generally NW-SE trending to near N-S one has led to thrust’s steepening and turning into high-angle strike-slip faults due to NE-SW oblique compression from the Albanides collision zone. The Othoni Island-Dhermi strike-slip fault offsets the dextrally dragged Devolli (to the east of Dumre diapir), Osumi (near to Berati town), and Vjosa (west of Shkoza village) rivers’ valleys formed from the Middle Pleistocene (180,000 years) to historic times. The Othoni Island-Dhermi dextral strike-slip fault, that reaches the maximum velocity of greater than 5 mm/year to the south of it, is the only leading fault that shaped the Mali i Kanalit Block-Dumre diapir dextral strike-slip fault zone. Focal mechanism solutions of earthquakes that occurred on the Mali i Kanalit Block - Dumre diapir dextral strike-slip zone show their generation from strike-slip faults in transpressional motions. Focal mechanism solutions of earthquakes that occurred on the Elbasan-Dibra were generated from normal faults with dextral strike-slip movements.},
 year = {2021}
}

Copy | Download

TY  - JOUR
T1  - Seismotectonics of Vlora-Elbasani-Dibra Transversal Fault Zone (Albania): A Review
AU  - Shyqyri Aliaj
Y1  - 2021/12/31
PY  - 2021
N1  - https://doi.org/10.11648/j.earth.20211006.20
DO  - 10.11648/j.earth.20211006.20
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 346
EP  - 357
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20211006.20
AB  - The Vlora-Elbasani-Dibra transversal fault zone crosses from south-west to northeast the Albanides collision zone starting from Vlora area to the Dumre diapir and continuing from Elbasani Quaternary graben to Dibra area, within the internal Albanides extensional zone. The Vlora-Elbasani-Dibra seismogenic fault zone is expressed by an alignment of important historical and instrumental seismicity with 15 Ms > 6 earthquakes. The Vlora-Berati-Elbasani segment of this fault zone during the year 1851 has been activated along all is length. The geological and neotectonic investigations and the focal mechanism solutions of earthquakes that occurred along the Vlora-Elbasani-Dibra fault zone prove its division into two distinct fault zones: a) the Mali i Kanalit Block - Dumre diapir strike-slip fault zone NNE trending in transpression, and b) the Elbasan-Dibra normal fault zone NE trending in transtension. The Mali i Kanalit Block-Dumre diapir strike-slip zone NNE trending in transpression offsets dextrally and to SW the folds and thrusts of the Çika, Kurveleshi and Berati anticlinal belts of Ionian zone. The Neogene (mainly since Middle Miocene) offset of the Çika, Kurveleshi and Berati anticlinal belts from generally NW-SE trending to near N-S one has led to thrust’s steepening and turning into high-angle strike-slip faults due to NE-SW oblique compression from the Albanides collision zone. The Othoni Island-Dhermi strike-slip fault offsets the dextrally dragged Devolli (to the east of Dumre diapir), Osumi (near to Berati town), and Vjosa (west of Shkoza village) rivers’ valleys formed from the Middle Pleistocene (180,000 years) to historic times. The Othoni Island-Dhermi dextral strike-slip fault, that reaches the maximum velocity of greater than 5 mm/year to the south of it, is the only leading fault that shaped the Mali i Kanalit Block-Dumre diapir dextral strike-slip fault zone. Focal mechanism solutions of earthquakes that occurred on the Mali i Kanalit Block - Dumre diapir dextral strike-slip zone show their generation from strike-slip faults in transpressional motions. Focal mechanism solutions of earthquakes that occurred on the Elbasan-Dibra were generated from normal faults with dextral strike-slip movements.
VL  - 10
IS  - 6
ER  -

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