Alpetar orogenia

Alpetar orogenia Mesozoikoaren bukaeran eta Zenozoikoan zehar,^[1] Europan, Afrika iparraldean eta Asian barrena, Afrikako, Indiako eta txikiagoa den Cimmeriako plaken eta iparraldeko Eurasiako plakaren arteko konbergentziaren ondorioz garatutako orogenia da. Europaren hegoaldean, Afrika iparraldean eta Asian ezagutzen diren mendikate garrantzitsuenak sortu zituen: Atlas, Rif, sistema Betikoa, Pirinioak^[2], Alpeak, Apeninoak^[3], Dinarideak, Helenideak, Karpatoak, Balkanak, Taurus, Kaukasoa^[4], Alborz, Zagros, Hindu Kush, Pamir, Karakorum eta Himalaia^[5].

↑ (Ingelesez) Moores, E.M. Fairbridge, R. w.. (2006). Encyclopedia of European and Asian Regional Geology. Springer Verlag ISBN 9781402048654. PMC 144223092. (Noiz kontsultatua: 2019-06-04).
↑ (Ingelesez) Muñoz, Josep Anton. (2019). Quesada, Cecilio ed. «Alpine Orogeny: Deformation and Structure in the Northern Iberian Margin (Pyrenees s.l.)» The Geology of Iberia: A Geodynamic Approach (Springer International Publishing): 433–451. doi:10.1007/978-3-030-11295-0_9. ISBN 978-3-030-11294-3. (Noiz kontsultatua: 2022-06-08).
↑ (Ingelesez) Rossetti, Federico; Goffé, Bruno; Monié, Patrick; Faccenna, Claudio; Vignaroli, Gianluca. (2004-12). «Alpine orogenic P-T-t-deformation history of the Catena Costiera area and surrounding regions (Calabrian Arc, southern Italy): The nappe edifice of north Calabria revised with insights on the Tyrrhenian-Apennine system formation: ALPINE TECTONICS IN NORTH CALABRIA» Tectonics 23 (6): n/a–n/a. doi:10.1029/2003TC001560. (Noiz kontsultatua: 2022-06-08).
↑ (Ingelesez) Adamia, Sh.A.; Lordkipanidze, M.B.; Zakariadze, G.S.. (1977-07). «Evolution of an active continental margin as exemplified by the Alpine history of the Caucasus» Tectonophysics 40 (3-4): 183–199. doi:10.1016/0040-1951(77)90065-8. (Noiz kontsultatua: 2022-06-08).
↑ (Ingelesez) Şengör, A.M.C.. (1986-08). «The dual nature of the Alpine-Himalayan system: Progress, problems and prospects» Tectonophysics 127 (3-4): 177–195. doi:10.1016/0040-1951(86)90060-0. (Noiz kontsultatua: 2022-06-08).

[1] (Ingelesez) Moores, E.M. Fairbridge, R. w.. (2006). Encyclopedia of European and Asian Regional Geology. Springer Verlag ISBN 9781402048654. PMC 144223092. (Noiz kontsultatua: 2019-06-04).

[2] (Ingelesez) Muñoz, Josep Anton. (2019). Quesada, Cecilio ed. «Alpine Orogeny: Deformation and Structure in the Northern Iberian Margin (Pyrenees s.l.)» The Geology of Iberia: A Geodynamic Approach (Springer International Publishing): 433–451. doi:10.1007/978-3-030-11295-0_9. ISBN 978-3-030-11294-3. (Noiz kontsultatua: 2022-06-08).

[3] (Ingelesez) Rossetti, Federico; Goffé, Bruno; Monié, Patrick; Faccenna, Claudio; Vignaroli, Gianluca. (2004-12). «Alpine orogenic P-T-t-deformation history of the Catena Costiera area and surrounding regions (Calabrian Arc, southern Italy): The nappe edifice of north Calabria revised with insights on the Tyrrhenian-Apennine system formation: ALPINE TECTONICS IN NORTH CALABRIA» Tectonics 23 (6): n/a–n/a. doi:10.1029/2003TC001560. (Noiz kontsultatua: 2022-06-08).

[4] (Ingelesez) Adamia, Sh.A.; Lordkipanidze, M.B.; Zakariadze, G.S.. (1977-07). «Evolution of an active continental margin as exemplified by the Alpine history of the Caucasus» Tectonophysics 40 (3-4): 183–199. doi:10.1016/0040-1951(77)90065-8. (Noiz kontsultatua: 2022-06-08).

[5] (Ingelesez) Şengör, A.M.C.. (1986-08). «The dual nature of the Alpine-Himalayan system: Progress, problems and prospects» Tectonophysics 127 (3-4): 177–195. doi:10.1016/0040-1951(86)90060-0. (Noiz kontsultatua: 2022-06-08).

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