2003
DOI: 10.3809/jvirtex.2003.00064
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Some Aspects Of The Italian Geology Not Fitting With A Subduction Scenario

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Cited by 31 publications
(23 citation statements)
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“…In contrast to the widely accepted subduction-related models, a sharply different geodynamic scenario, i.e. a relationship with continental extension and/or upwelling mantle plume, has also been suggested to explain the evolution of the Central Mediterranean (Vollmer 1989;Lavecchia & Stoppa 1996;Ayuso et al 1998;Lavecchia et al 2003;Bell et al 2004). Lavecchia et al (2003) argued that the deformation style of the central Apennine fold-and-thrust belt, the absence of an accretionary wedge above the assumed subduction plane and the occurrence of ultra-alkaline and carbonatitic magmas within the Apennine mountain chain are evidence against the classic subduction-related models.…”
Section: Cenozoic Subduction Zones In the Alpine-mediterranean Regionmentioning
confidence: 99%
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“…In contrast to the widely accepted subduction-related models, a sharply different geodynamic scenario, i.e. a relationship with continental extension and/or upwelling mantle plume, has also been suggested to explain the evolution of the Central Mediterranean (Vollmer 1989;Lavecchia & Stoppa 1996;Ayuso et al 1998;Lavecchia et al 2003;Bell et al 2004). Lavecchia et al (2003) argued that the deformation style of the central Apennine fold-and-thrust belt, the absence of an accretionary wedge above the assumed subduction plane and the occurrence of ultra-alkaline and carbonatitic magmas within the Apennine mountain chain are evidence against the classic subduction-related models.…”
Section: Cenozoic Subduction Zones In the Alpine-mediterranean Regionmentioning
confidence: 99%
“…a relationship with continental extension and/or upwelling mantle plume, has also been suggested to explain the evolution of the Central Mediterranean (Vollmer 1989;Lavecchia & Stoppa 1996;Ayuso et al 1998;Lavecchia et al 2003;Bell et al 2004). Lavecchia et al (2003) argued that the deformation style of the central Apennine fold-and-thrust belt, the absence of an accretionary wedge above the assumed subduction plane and the occurrence of ultra-alkaline and carbonatitic magmas within the Apennine mountain chain are evidence against the classic subduction-related models. They proposed that plume-induced lithospheric stretching and local-scale rift push-induced crustal shortening form a viable alternative model for the evolution of the Central Mediterranean region (Lavecchia et al 2003;Bell et al 2004).…”
Section: Cenozoic Subduction Zones In the Alpine-mediterranean Regionmentioning
confidence: 99%
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