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Numidian Flysch

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Journal Article
Published: 01 May 2014
Bulletin de la Société Géologique de France (2014) 185 (5): 343-356.
...Marco D’errico; Angelida Di Staso; Annamaria Fornelli; Domenico Guida; Francesca Micheletti; Vincenzo Perrone; Giuliana Raffaelli Abstract The Numidian Flysch shows constant lithological features from the strait of Gibraltar to central Italy. It is characterized by quartzarenites showing grains...
FIGURES | View All (6)
Journal Article
Published: 01 June 2019
Italian Journal of Geosciences (2019) 138 (2): 216-230.
... of sandstones from five stratigraphic sections of the Numidian Flysch in Southern Italy. The purpose of this comparison is to assess the homogeneity and provenance of detritus because quartz-rich sandstones of both formations are coeval having Burdigalian p.p. - Early Langhian age. The depositional domain...
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Journal Article
Journal: Palynology
Published: 01 January 2001
Palynology (2001) 25 (1): 29-55.
...STEFANO TORRICELLI; ULDERICO BIFFI Abstract Diverse and relatively well preserved palynological assemblages from five outcrop sections sampled in the Numidian Flysch of northern Tunisia are presented and discussed. They provide valuable information for age determination and correlation within...
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Journal Article
Journal: GSA Bulletin
Published: 01 June 1979
GSA Bulletin (1979) 90 (6): 513-515.
Journal Article
Journal: GSA Bulletin
Published: 01 June 1979
GSA Bulletin (1979) 90 (6_Part_II): 886-923.
...Michael D. Carr; Elizabeth L. Miller Abstract INTRODUCTION The Oligocene-Miocene Numidian Complex forms the highest structural unit in the Mahgreb fold and thrust belt, which extends along the northern coast of Africa Major tectonic activity along this belt occurred during Miocene time. The Mahgreb...
Journal Article
Published: 01 July 1975
Geological Magazine (1975) 112 (4): 373-381.
Image
- Schematic map of quartz-rich sandstones of the <b>Numidian</b> <b>Flysch</b> in the wes...
Published: 01 June 2019
Fig. 1 - Schematic map of quartz-rich sandstones of the Numidian Flysch in the western-central Mediterranean region (modified from H oyez , 1989 ).
Image
- Petrographic and chemical composition of <b>Numidian</b> <b>Flysch</b> (AV Monteverde-A...
Published: 01 June 2019
Fig. 5 - Petrographic and chemical composition of Numidian Flysch (AV Monteverde-Aquilonia; PQZ Pietragalla from F ornelli (1998) ; GM Rotondella; VAL Valsinni) and Bifurto sandstones (FNF1 and fNp2). a) QFL diagram showing the principal compositions of Numidian Flysch sandstones ranging from
Image
<b>Numidian</b> <b>Flysch</b> quartzarenites cropping out along the Campomaggiore road (P...
Published: 01 May 2014
Fig. 3 Numidian Flysch quartzarenites cropping out along the Campomaggiore road (Potenza).
Image
Decametric fold in the <b>Numidian</b> <b>Flysch</b> (Valle Lavarone quarry, near Castel ...
Published: 01 May 2014
Fig. 4 Decametric fold in the Numidian Flysch (Valle Lavarone quarry, near Castel Lagopesole, Potenza).
Image
Calcareous nannofossils in the lowermost levels of the <b>Numidian</b> <b>Flysch</b>.
Published: 01 May 2014
Table II Calcareous nannofossils in the lowermost levels of the Numidian Flysch.
Image
<b>Numidian</b> <b>Flysch</b>: a) quartzarenite, Rotondella road, polarized light, 350X; ...
Published: 01 May 2014
Fig. 5 Numidian Flysch: a) quartzarenite, Rotondella road, polarized light, 350X; b) arkose, Pietragalla cemetery, polarized light, 350X; Bifurto Fm: c) quartzarenite, Pergola, polarized light, 350X; d) sub-arkose, mount Raparello, polarized light, 350X.
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Composition of the <b>Numidian</b> <b>Flysch</b> sandstones along the Maghrebian-Apennine...
Published: 20 December 2013
Table 2 Composition of the Numidian Flysch sandstones along the Maghrebian-Apennine Chain. Q=total quartzose grains; F=P+K, where: F=total feldspar grains, P and K=plagioclase and k-feldspar single grains, respectively; L=Lc+Ls+Ch, where: L=unstable fine-grained rock fragments (<0.06 mm
Image
The <b>numidian</b> <b>flysch</b> lithofacies:  a ) shales (Portella Colla mb) with iron-...
Published: 01 February 2011
Fig. 2 The numidian flysch lithofacies: a ) shales (Portella Colla mb) with iron-manganiferous crusts (Pizzo Candreo); b ) hectometres turbiditic succession of the Geraci Siculo mb (Bosco della Ficuzza); c ) massive thick-bedded coarse and well-rounded quartz-conglomerates, alternated
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Lithostratigraphic characters of the Sicilidi deposits and <b>numidian</b> <b>flysch</b> ...
Published: 01 February 2011
Table 1 Lithostratigraphic characters of the Sicilidi deposits and numidian flysch formation.
Image
Large blocks  (knockers)  of <b>Numidian</b> <b>Flysch</b> quartzarenites enclosed within...
Published: 01 November 2010
Figure 7. Large blocks (knockers) of Numidian Flysch quartzarenites enclosed within the mélange of the varicolored clays near the village of Platì (see Fig. 2 for location). View looking northeastward.
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a ) <b>Numidian</b> <b>Flysch</b> sequence at the front of the Maghrebian Chain (Mt. Etna...
Published: 01 October 2010
Fig. 3 a ) Numidian Flysch sequence at the front of the Maghrebian Chain (Mt. Etna on the background); b ) 1879 eruptive fissure along the NE Rift; c ) Aerial view of the 200 m high scarp («timpa») of the Acireale fault between Acireale (on the footwall) and Santa Tecla (on the hangingwall
Journal Article
Published: 01 February 2011
Italian Journal of Geosciences (2011) 130 (1): 42-60.
...Fig. 2 The numidian flysch lithofacies: a ) shales (Portella Colla mb) with iron-manganiferous crusts (Pizzo Candreo); b ) hectometres turbiditic succession of the Geraci Siculo mb (Bosco della Ficuzza); c ) massive thick-bedded coarse and well-rounded quartz-conglomerates, alternated...
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Journal Article
Published: 01 January 2001
Italian Journal of Geosciences (2001) 120 (1): 3-14.
... samnitic units Auct. p.p.), composed of the Flysch Rosso Auct. Formation, and the Numidian Flysch, and the Fortore Unit, formed by the Argille Varicolori Auct. Formation and Frigento Formation p.p. The Numidian Flysch, not previously mapped in the area, outcrops along the "Vallone dei Bagni" talweg and our...
Journal Article
Published: 01 January 1953
Bulletin de la Société Géologique de France (1953) S6-III (9): 775-783.
...Charles Gottis Abstract Describes some of the most typical of the intraformational sandstone dikes in the Numidian Flysch (Tertiary) deposits of the Kroumirie region, Tunisia. The dikes originate in sandy strata, and the youngest bed which they traverse is always argillaceous and always succeeded...