Results 171 to 180 of about 14,756 (198)
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Geology, 1989
Several features of the Alboran Sea suggest that it may have been a high collisional ridge in Paleogene time that subsequently underwent extensional-collapse, driving radial thrusting around the Gibraltar arc. (1) The basin is underlain by thin (13-20 km) continental crust, has an east-west-trending horst and graben morphology, was the locus of Neogene
J. P. Platt, R.L.M. Vissers
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Several features of the Alboran Sea suggest that it may have been a high collisional ridge in Paleogene time that subsequently underwent extensional-collapse, driving radial thrusting around the Gibraltar arc. (1) The basin is underlain by thin (13-20 km) continental crust, has an east-west-trending horst and graben morphology, was the locus of Neogene
J. P. Platt, R.L.M. Vissers
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Journal of Geodynamics, 2015
Abstract The intermontane Ronda Basin, currently located in the Western Betics External Zones, started as an embayment of the Betic foreland basin during the Tortonian. We have characterized a post-Serravallian, basin-related deformation event that overprinted the former fold-and-thrust belt. Updated structural and kinematic maps allow us to identify
A. Jiménez-Bonilla +4 more
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Abstract The intermontane Ronda Basin, currently located in the Western Betics External Zones, started as an embayment of the Betic foreland basin during the Tortonian. We have characterized a post-Serravallian, basin-related deformation event that overprinted the former fold-and-thrust belt. Updated structural and kinematic maps allow us to identify
A. Jiménez-Bonilla +4 more
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Abschlussbericht : Sonne SO175 ; GAP: Gibraltar Arc Processes ; [Laufzeit: 01.10.2003 - 31.03.2005 ]
2005Ill., graph ...
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Contrasting fault reactivation patterns along the Betic foreland (Gibraltar arc, southern Spain)
During the Miocene formation of the Gibraltar Arc (western Mediterranean), the orogenic load on the SSE margin of the Betics (northern branch) foreland basin led to the formation of an ENE-WSW flexural relief on the foreland (forebulge), producing orthogonal extension accommodated by normal faults oriented parallel to the forebulge strike.Alejandro Jiménez-Bonilla +7 more
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Geological adventures and misadventures of the Gibraltar Arc
Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, 2006openaire +1 more source
Plio-Pleistocene Sequence Stratigraphy and Tectonics of the Gibraltar Arc
1999Joan F. Flinch, Peter R. Vail
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