In the Calabrian Arc, NW–SE oriented left lateral strikeslip faults and associated jog-related features (i.e. folds, reverse/normal faults), have controlled the evolution of the mountain belt since Late Miocene times (KNOTT & TURCO, 1991; VAN DIJK et alii, 2000, and references therein). Segmentation in strike- and oblique-slip fault systems has been the subject of detailed research (e.g. Tchalenko,1970; TCHALENKO & AMBRASEYS, 1970; WALLACE, 1973; AYDIN & NUR, 1982, 1985; AYDIN & PAGE, 1984; BILHAM & WILLIAMS, 1985; SYLVESTER, 1988; VAN DIJK et alii, 2000). In the southern Calabrian Arc, oblique slip fault systems, displacement generates important topographic gradients with associated uplift and subsidence forming both uplifted ranges and sedimentary depocentres (Sylvester, 1988). All these data allow us to propose a detailed tectonic evolution for the Siderno strait from its initial formation during the Serravallian until the present-day, as well as to evaluate the influence of strike-slip fault and reverse fault present

Tectono-stratigraphic evolution of the Siderno Basin, southern Calabrian Arc, Italy / Tripodi V.; Muto F; Critelli S.. - In: RENDICONTI ONLINE DELLA SOCIETÀ GEOLOGICA ITALIANA. - ISSN 2035-8008. - 21(2012), pp. 109-111.

Tectono-stratigraphic evolution of the Siderno Basin, southern Calabrian Arc, Italy

MUTO, Francesco;CRITELLI, Salvatore
2012

Abstract

In the Calabrian Arc, NW–SE oriented left lateral strikeslip faults and associated jog-related features (i.e. folds, reverse/normal faults), have controlled the evolution of the mountain belt since Late Miocene times (KNOTT & TURCO, 1991; VAN DIJK et alii, 2000, and references therein). Segmentation in strike- and oblique-slip fault systems has been the subject of detailed research (e.g. Tchalenko,1970; TCHALENKO & AMBRASEYS, 1970; WALLACE, 1973; AYDIN & NUR, 1982, 1985; AYDIN & PAGE, 1984; BILHAM & WILLIAMS, 1985; SYLVESTER, 1988; VAN DIJK et alii, 2000). In the southern Calabrian Arc, oblique slip fault systems, displacement generates important topographic gradients with associated uplift and subsidence forming both uplifted ranges and sedimentary depocentres (Sylvester, 1988). All these data allow us to propose a detailed tectonic evolution for the Siderno strait from its initial formation during the Serravallian until the present-day, as well as to evaluate the influence of strike-slip fault and reverse fault present
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Utilizza questo identificativo per citare o creare un link a questo documento: http://hdl.handle.net/20.500.11770/147889
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