The opening of Sirte basin: Result of slab avalanching?

Fabio Antonio Capitanio, Claudio Faccenna, R Funiciello

Research output: Contribution to journalArticleResearchpeer-review

30 Citations (Scopus)

Abstract

North Africa s Sirte basin opening is an enigmatic feature in the complex Meso-Cenozoic rearrangement of Mediterranean tectonics. New borehole data inversion constrains its deformation history showing a stretching event starting 70 Ma and terminating in a further abrupt increase at 50 Ma, rapidly fading afterwards. The timing of this event hardly reconciles with the Mesozoic major plates reorganization following the spreading of the Atlantic, and the Neogene Central Mediterranean tectonics, active at different times. Here, we propose that Sirte rifting could have been driven by the pull exerted by the Hellenic subduction. Reconstructions of Hellenic convergence and slab deep subduction, as constrained by plate kinematics and tomography, show that large slab mass accumulates in the upper mantle by late Cretaceous?Paleogene, eventually forcing further sinking in the lower mantle, coeval to the growing strain evolution recorded in Sirte. Furthermore, the 20 m.y. phase of large pull here recorded, the consequent rapid growth over 10 m.y. and following decay are compatible with the dynamics of slab avalanche as revealed by numerical models, showing that the Sirte basin opened in response to the large pull force developed during the mass flush, and transferred from deep slab to surface.
Original languageEnglish
Pages (from-to)210 - 216
Number of pages7
JournalEarth and Planetary Science Letters
Volume285
Publication statusPublished - 2009

Cite this

Capitanio, Fabio Antonio ; Faccenna, Claudio ; Funiciello, R. / The opening of Sirte basin: Result of slab avalanching?. In: Earth and Planetary Science Letters. 2009 ; Vol. 285. pp. 210 - 216.
@article{c8c54eb0c7714434b4118b29eff88b78,
title = "The opening of Sirte basin: Result of slab avalanching?",
abstract = "North Africa s Sirte basin opening is an enigmatic feature in the complex Meso-Cenozoic rearrangement of Mediterranean tectonics. New borehole data inversion constrains its deformation history showing a stretching event starting 70 Ma and terminating in a further abrupt increase at 50 Ma, rapidly fading afterwards. The timing of this event hardly reconciles with the Mesozoic major plates reorganization following the spreading of the Atlantic, and the Neogene Central Mediterranean tectonics, active at different times. Here, we propose that Sirte rifting could have been driven by the pull exerted by the Hellenic subduction. Reconstructions of Hellenic convergence and slab deep subduction, as constrained by plate kinematics and tomography, show that large slab mass accumulates in the upper mantle by late Cretaceous?Paleogene, eventually forcing further sinking in the lower mantle, coeval to the growing strain evolution recorded in Sirte. Furthermore, the 20 m.y. phase of large pull here recorded, the consequent rapid growth over 10 m.y. and following decay are compatible with the dynamics of slab avalanche as revealed by numerical models, showing that the Sirte basin opened in response to the large pull force developed during the mass flush, and transferred from deep slab to surface.",
author = "Capitanio, {Fabio Antonio} and Claudio Faccenna and R Funiciello",
year = "2009",
language = "English",
volume = "285",
pages = "210 -- 216",
journal = "Earth and Planetary Science Letters",
issn = "0012-821X",
publisher = "Elsevier",

}

The opening of Sirte basin: Result of slab avalanching? / Capitanio, Fabio Antonio; Faccenna, Claudio; Funiciello, R.

In: Earth and Planetary Science Letters, Vol. 285, 2009, p. 210 - 216.

Research output: Contribution to journalArticleResearchpeer-review

TY - JOUR

T1 - The opening of Sirte basin: Result of slab avalanching?

AU - Capitanio, Fabio Antonio

AU - Faccenna, Claudio

AU - Funiciello, R

PY - 2009

Y1 - 2009

N2 - North Africa s Sirte basin opening is an enigmatic feature in the complex Meso-Cenozoic rearrangement of Mediterranean tectonics. New borehole data inversion constrains its deformation history showing a stretching event starting 70 Ma and terminating in a further abrupt increase at 50 Ma, rapidly fading afterwards. The timing of this event hardly reconciles with the Mesozoic major plates reorganization following the spreading of the Atlantic, and the Neogene Central Mediterranean tectonics, active at different times. Here, we propose that Sirte rifting could have been driven by the pull exerted by the Hellenic subduction. Reconstructions of Hellenic convergence and slab deep subduction, as constrained by plate kinematics and tomography, show that large slab mass accumulates in the upper mantle by late Cretaceous?Paleogene, eventually forcing further sinking in the lower mantle, coeval to the growing strain evolution recorded in Sirte. Furthermore, the 20 m.y. phase of large pull here recorded, the consequent rapid growth over 10 m.y. and following decay are compatible with the dynamics of slab avalanche as revealed by numerical models, showing that the Sirte basin opened in response to the large pull force developed during the mass flush, and transferred from deep slab to surface.

AB - North Africa s Sirte basin opening is an enigmatic feature in the complex Meso-Cenozoic rearrangement of Mediterranean tectonics. New borehole data inversion constrains its deformation history showing a stretching event starting 70 Ma and terminating in a further abrupt increase at 50 Ma, rapidly fading afterwards. The timing of this event hardly reconciles with the Mesozoic major plates reorganization following the spreading of the Atlantic, and the Neogene Central Mediterranean tectonics, active at different times. Here, we propose that Sirte rifting could have been driven by the pull exerted by the Hellenic subduction. Reconstructions of Hellenic convergence and slab deep subduction, as constrained by plate kinematics and tomography, show that large slab mass accumulates in the upper mantle by late Cretaceous?Paleogene, eventually forcing further sinking in the lower mantle, coeval to the growing strain evolution recorded in Sirte. Furthermore, the 20 m.y. phase of large pull here recorded, the consequent rapid growth over 10 m.y. and following decay are compatible with the dynamics of slab avalanche as revealed by numerical models, showing that the Sirte basin opened in response to the large pull force developed during the mass flush, and transferred from deep slab to surface.

UR - http://www.sciencedirect.com/science?_ob=MImg&_imagekey=B6V61-4WS226C-1-J&_cdi=5801&_user=542840&_pii=S0012821X0900363X&_orig=search&_coverDate=07%2Ff

M3 - Article

VL - 285

SP - 210

EP - 216

JO - Earth and Planetary Science Letters

JF - Earth and Planetary Science Letters

SN - 0012-821X

ER -