2014
DOI: 10.1016/j.lithos.2013.10.010
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Lamprophyres of Italy: early Cretaceous alkaline lamprophyres of Southern Tuscany, Italy

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Cited by 49 publications
(34 citation statements)
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“…The Albian (Stoppa et al, ) alkaline lamprophyric dykes, sills, and subordinate pillow lavas sparsely cropping out in southern Tuscany (STAL) are hosted in the Sub‐Ligurian succession made of pelagic cherty micrites interbedded in siliciclastic turbidites. Their geochemical signature is again of clearly anorogenic type, displaying a strongly incompatible elements‐enriched character, which is even more marked with respect to that shown by the alkali‐richest VVP igneous rocks.…”
Section: Discussionmentioning
confidence: 99%
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“…The Albian (Stoppa et al, ) alkaline lamprophyric dykes, sills, and subordinate pillow lavas sparsely cropping out in southern Tuscany (STAL) are hosted in the Sub‐Ligurian succession made of pelagic cherty micrites interbedded in siliciclastic turbidites. Their geochemical signature is again of clearly anorogenic type, displaying a strongly incompatible elements‐enriched character, which is even more marked with respect to that shown by the alkali‐richest VVP igneous rocks.…”
Section: Discussionmentioning
confidence: 99%
“…Upper Cretaceous–Eocene anorogenic igneous rocks crop out from Sicilian Maghrebides (Hyblean–Sicilide domain) to Apennines and Apulian foreland, up to the southern Alps (Veneto area; Bellia et al, ; Bigazzi et al, ; Di Girolamo et al, , ; Grasso et al, ; Groppelli & Pasquarè, ; Lucido et al, ; Macera, Gasperini, Ranalli, & Mahatsente, ; Macera et al, ; Pierattini, Scandone, & Cortini, Beccaluva et al, ; Bianchini et al, ; Avanzinelli et al, ; Stoppa et al, ). Apart from the large (~1500 km 2 ) Veneto Volcanic Province area (VVP in Figure A) and the Capo Passero–Pachino area (CP in Figure a; up to 4,000 km 2 considering data from wells drilled in SE Sicily (Longaretti & Rocchi, ; ViDEPI, ), exposures of igneous rocks in the Adria domain are extremely localized (Figure a) and appear as scattered of dykes, sills, pillow lavas, and lava flows.…”
Section: Geological Settingmentioning
confidence: 99%
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“…(Early Cretaceous) and also cropping out a few km south of the Mt. Amiata volcano (Senna creek valley) as well as in several other localities of southern Tuscany (Passerini, 1964;Brunacci et al, 1983;Faraone and Stoppa, 1990;Brogi et al, 2000;Stoppa et al, 2014). d) The Pre-Neogene substratum of Mt.…”
Section: Introductionmentioning
confidence: 99%