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Lungro-Verbicaro Unit

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Journal Article
Published: 01 October 2010
Italian Journal of Geosciences (2010) 129 (3): 450–456.
...Marco D’Errico; Angelida Di Staso Abstract Field and biostratigraphic data from Cenozoic metasedimentary succession (« breccia a selce », Colle Trodo and « Scisti del Fiume Lao » Formations) of Lungro-Verbicaro Unit are reported. The « Scisti del Fiume Lao » Formation, formerly included...
FIGURES
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Detailed stratigraphic columns for the <span class="search-highlight">Lungro</span>–<span class="search-highlight">Verbicaro</span> <span class="search-highlight">Unit</span> and the Pollin...
Published: 01 September 2010
Fig. 2. Detailed stratigraphic columns for the LungroVerbicaro Unit and the Pollino–Ciagola Unit. Samples described in the text are shown. SFL Fm, Scisti del Fiume Lao Formation.
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Outcrops of the studied rocks. <span class="search-highlight">Lungro</span>–<span class="search-highlight">Verbicaro</span> <span class="search-highlight">Unit</span>: ( a ) Middle Triassic...
Published: 01 September 2010
Fig. 3. Outcrops of the studied rocks. LungroVerbicaro Unit: ( a ) Middle Triassic metapelites and quarzites grading upwards to Ladinian–Carnian metalimestones and evaporites (Rosa River Valley); early quartz veins parallel to foliation (site CCL 29.1) are evident; ( b ) Maastrichtian–middle
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Mica composition for the <span class="search-highlight">Lungro</span>–<span class="search-highlight">Verbicaro</span> <span class="search-highlight">Unit</span> plotted on the ternary diagr...
Published: 01 September 2010
Fig. 6. Mica composition for the LungroVerbicaro Unit plotted on the ternary diagram of Rey & Kübler (1983 ). Vertices represent the intensities of different 00 l XRD reflections obtained from deconvoluted peaks. Data fall within the range of illite (I) and phengite (Ph) compositions.
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Microstructures from the <span class="search-highlight">Lungro</span>–<span class="search-highlight">Verbicaro</span> <span class="search-highlight">Unit</span>. ( a ) (S 1 ) LVU -related c...
Published: 01 December 2007
Fig. 7.  Microstructures from the LungroVerbicaro Unit. ( a ) (S 1 ) LVU -related chloritoid, partly preserved as rosettes (arrowed) and rotated parallel to the main (S 2 ) LVU foliation (Anisian phyllites, San Donato area). ( b ) Intrafolial (F 2 ) LVU fold and main (S 2 ) LVU foliation
Journal Article
Published: 01 December 2007
Journal of the Geological Society (2007) 164 (6): 1165–1186.
...Fig. 7.  Microstructures from the LungroVerbicaro Unit. ( a ) (S 1 ) LVU -related chloritoid, partly preserved as rosettes (arrowed) and rotated parallel to the main (S 2 ) LVU foliation (Anisian phyllites, San Donato area). ( b ) Intrafolial (F 2 ) LVU fold and main (S 2 ) LVU foliation...
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Journal Article
Published: 01 September 2010
Journal of the Geological Society (2010) 167 (5): 985–999.
...Fig. 2. Detailed stratigraphic columns for the LungroVerbicaro Unit and the Pollino–Ciagola Unit. Samples described in the text are shown. SFL Fm, Scisti del Fiume Lao Formation. ...
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Journal Article
Published: 01 June 2008
Italian Journal of Geosciences (2008) 127 (3): 357–373.
.... Moreover, the recognition in some Apennine metamorphic units (Tuscan Metamorphic and Lungro-Verbicaro Units) of HP/LT parageneses, testifying both the subduction of continental crust up to depths of some tens of kms, and a tectono-sedimentary evolution quite similar to that characterizing the Betic-Rifian...
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a ) Detailed map of Colle Trodo area;  b ) detailed map of Contrada Alberos...
Published: 01 October 2010
Fig. 2 a ) Detailed map of Colle Trodo area; b ) detailed map of Contrada Alberosa area (near Verbicaro village); c ) geological section of Contrada Alberosa locality; d ) synthetic stratigraphic column relative to the Cenozoic deposits of the Lungro-Verbicaro Unit. – a) carta geologica
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Major recumbent (F 3 ) LVU  fold in Triassic (Ladinian–Carnian) metacarbona...
Published: 01 December 2007
Fig. 6.  Major recumbent (F 3 ) LVU fold in Triassic (Ladinian–Carnian) metacarbonates and phyllites of the LungroVerbicaro Unit (La Mula Mt.).
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- Field evidences of the CGDF in the northern sample area (location of phot...
Published: 08 May 2017
Fig. 6 - Field evidences of the CGDF in the northern sample area (location of photographs reported as small rectangles in Fig. 5a ); (a, b) low-angle extensional contact between the Apennine Lungro-Verbicaro unit and the Miocene deposits near San Sosti (a) and Lungro (b); (c-g) NE-SW-trending
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Schematic reconstruction of the subduction–exhumation history of the <span class="search-highlight">Lungro</span>...
Published: 01 December 2007
Fig. 14.  Schematic reconstruction of the subduction–exhumation history of the LungroVerbicaro Unit and Pollino–Ciagola Unit. ( a – d ) Early to Middle Miocene stages. ( e ) Enlargement of box in ( d ), showing structures developed during (D 3 ) LVU deformation stage (see text). ( f ) Late
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Orientation data (lower hemisphere Schmidt projections) for the <span class="search-highlight">Lungro</span>–Verb...
Published: 01 December 2007
Fig. 10.  Orientation data (lower hemisphere Schmidt projections) for the LungroVerbicaro Unit (LVU), Pollino–Ciagola Unit (PCU) and Cetraro Unit (CU) structural elements. S, poles to foliation; SL, stretching lineations; FA, fold hinges; CL, crenulation (microfold) lineations; PA, poles
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P – T  paths calculated from petrological and compositional data on: (i) ca...
Published: 01 December 2007
Fig. 11.   P – T paths calculated from petrological and compositional data on: (i) carpholite, chloritoid and phengite contained in the Triassic phyllites and Miocene metapelites of the Lungro Verbicaro Unit, and (ii) chloritoid and phengite in the Triassic phyllites of the Cetraro Unit
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( a ) Intensely deformed calcareous conglomerate of the Pollino–Ciagola Uni...
Published: 01 December 2007
of the Pollino–Ciagola Unit (Campotenese area). ( d ) Tectonic superimposition of the LungroVerbicaro Unit onto the Pollino–Ciagola Unit north of Campotenese. The original low-angle contact (white) is offset by late faults (black lines).
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(A) Geologic sketch map of the Diamante area, modified from  Iannace et al....
Published: 01 December 2012
study. The structurally high crystalline basement units (CB) are equivalent to the upper-plate Sila Unit of the present study. LV—Lungro-Verbicaro Unit; C—Cetraro Unit; TM—Tortonian-Messinian deposits; Q—Pliocene–Holocene deposits. (B) Ar/Ar spectrum for Diamante phengite.
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( a ) Calcareous breccia (including chert clasts) at the base of the Colle ...
Published: 01 December 2007
the youngest formations of the LungroVerbicaro Unit are well preserved. Stars indicate localities of carpholite findings.
Journal Article
Published: 01 June 2014
Italian Journal of Geosciences (2014) 133 (2): 249–270.
... for the “Scisti del Fiume Lao” Fm (Lungro-Verbicaro Unit; D’E rrico & D i S taso , 2010). The nappe-stack was sutured by Serravallian (?)-Tortonian sandstones in the Longobucco Unit (V igna -R oli et alii , 2012). In the basement units of Southern Calabria many petrological and geochemical...
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Journal Article
Published: 08 May 2017
Italian Journal of Geosciences (2017) 136 (3): 434–453.
...Fig. 6 - Field evidences of the CGDF in the northern sample area (location of photographs reported as small rectangles in Fig. 5a ); (a, b) low-angle extensional contact between the Apennine Lungro-Verbicaro unit and the Miocene deposits near San Sosti (a) and Lungro (b); (c-g) NE-SW-trending...
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Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.262.01.01
EISBN: 9781862395107
... associated with the Tethys opening, cuts across both Mesozoic and Palaeozoic terrains ( Bouillin & Bellomo 1990 ). Fig. 4. Schematic geological map of the Calabrian–Peloritanian Arc. Verrucano-like deposits are present in the LungroVerbicaro, Bagni and Ali–Montagnareale Units; Pseudoverrucano-like...
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