1996
DOI: 10.1016/0040-1951(95)00197-2
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UPb and RbSr geochronological evidence for late Hercynian tectonic and Alpine overthrusting in Kabylian metamorphic basement massifs (northeastern Algeria)

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Cited by 36 publications
(26 citation statements)
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“…The folds are NW-SE and E-W and their vergence is variable. In Kabylia, late Hercynian granitoids were emplaced around 270-280 Ma (U-Pb on zircons, Peucat et al, 1996).…”
Section: The Rifian-kabylian Zonementioning
confidence: 99%
“…The folds are NW-SE and E-W and their vergence is variable. In Kabylia, late Hercynian granitoids were emplaced around 270-280 Ma (U-Pb on zircons, Peucat et al, 1996).…”
Section: The Rifian-kabylian Zonementioning
confidence: 99%
“…These fragments also contain large masses of orthogneisses, which occur in Sardinia, Calabria (Italy) and northern Algeria. A few available age data show that these orthogneisses range from lower Ordovician in Sardinia (Giacomini et al 2006) and Petite Kabylie (Peucat et al 1996), to Neoproterozoic-Early Cambrian in Calabria (Aspromonte and Serre; Schenk and Todt 1989;Senesi 1999). Middle Ordovician silicic and mafic metavolcanic rocks are also present in southern Calabria and in the Peloritani Mountains (paleontological records: Acquafredda et al 1994; U-Pb zircon ages: Trombetta et al 2004).…”
Section: Introductionmentioning
confidence: 97%
“…A possible example is the deep crustal shear synchronous with the emplacement of granitoids (dated at V280 and V270 Ma) from the Petite and Grande Kabylie of northern Algeria [71]. The Kabylies, together with Calabria and Corsica-Sardinia, were attached to the French^Catalan margin before the Cenozoic [15].…”
Section: Driving Forces and Plate Boundariesmentioning
confidence: 99%