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Agnano Breccia

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Journal Article
Published: 01 March 2002
European Journal of Mineralogy (2002) 14 (2): 447–451.
...Marco FRANZINI; Marco LEZZERINI Abstract The chemical, mineralogical and main physical properties of 20 samples belonging to the polygenic sedimentary “Agnano breccias” were determined within the framework of a wide-ranging research study on the building stones and mortars used in the cities...
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Chemical and normative compositions of <span class="search-highlight">Agnano</span> <span class="search-highlight">breccias</span>.
Published: 01 March 2002
Table 2. Chemical and normative compositions of Agnano breccias.
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Physical data on <span class="search-highlight">Agnano</span> <span class="search-highlight">breccias</span> (data measured on 17 samples).
Published: 01 March 2002
Table 4. Physical data on Agnano breccias (data measured on 17 samples).
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Northeastern corner of the Solfatara volcano. (A) Sharp contact between pip...
Published: 01 September 2015
Figure 5. Northeastern corner of the Solfatara volcano. (A) Sharp contact between pipe breccias and Agnano–Monte Spina (AMS) deposits (host rock). (B) Centimeter-sized accretionary lapilli in the injection breccias. (C) Highly deformed host rock along the contact with the breccias. (D) Panoramic
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Volcanic and tectonic sketch of the CF and the BFP areas (after  Russo  et ...
Published: 01 February 2002
 ybp); (4) pyroclastics of Agnano volcanic field (4000–3500 ybp); (5) S. Teresa volcanics (5500–3500 ybp); (6) pyroclastics and volcanic breccias of Monte Spina–Agnano eruption ( c. 4400 ybp); (7) pyroclastics of Cella–Monte S. Angelo unit (5500–5000 ybp); (8) Yellow Tuff of Nisida; (9) Yellow Tuff
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(A) Ring fault of the <span class="search-highlight">Agnano</span>–Monte Spina (AMS) caldera sealed by the Solfat...
Published: 01 September 2015
Figure 7. (A) Ring fault of the Agnano–Monte Spina (AMS) caldera sealed by the Solfatara deposits (Pisciarelli). (B) NE-SW normal fault in pre-AMS and AMS deposits sealed by Solfatara deposits (Pisciarelli). (C) Mud pools and fumaroles localized along the northeast continuation of the fault shown
Journal Article
Journal: GSA Bulletin
Published: 01 September 2015
GSA Bulletin (2015) 127 (9-10): 1485–1504.
...Figure 5. Northeastern corner of the Solfatara volcano. (A) Sharp contact between pipe breccias and Agnano–Monte Spina (AMS) deposits (host rock). (B) Centimeter-sized accretionary lapilli in the injection breccias. (C) Highly deformed host rock along the contact with the breccias. (D) Panoramic...
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Journal Article
Published: 31 October 2012
Geological Magazine (2013) 150 (3): 412–425.
... (Scarpati, Cole & Perrotta, 1993 ; Deino et al . 2004 ). Most deposits exposed within the city of Naples precede both ignimbrites, whereas the Santa Teresa, Minopoli, Agnano-Monte Spina, Pisani (Di Vito et al . 1999 ), Nisida Island and Mt Echia tuff (Cole, Perrotta...
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Journal Article
Published: 01 January 2001
European Journal of Mineralogy (2001) 13 (1): 187–195.
... (Lucca).w Seventy-two samples (26 QG and 46 QWP) have been collected ( Table 1 ). Sampling areas ( Fig. 1 ) were chosen so as to cover the whole quartzite outcropping (about 50 km 2 ), with special regard to those sites (Crespignano, Guamo and San Allago — Agnano) where stone quarrying was carried...
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Journal Article
Published: 01 February 2002
Geochemistry: Exploration, Environment, Analysis (2002) 2 (1): 45–56.
... ybp); (4) pyroclastics of Agnano volcanic field (4000–3500 ybp); (5) S. Teresa volcanics (5500–3500 ybp); (6) pyroclastics and volcanic breccias of Monte Spina–Agnano eruption ( c. 4400 ybp); (7) pyroclastics of Cella–Monte S. Angelo unit (5500–5000 ybp); (8) Yellow Tuff of Nisida; (9) Yellow Tuff...
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Journal Article
Published: 01 November 2011
Geological Magazine (2012) 149 (3): 532–550.
... was emplaced at c . 3.9 ka (K–Ar; Di Girolamo et al . 1984 ) in the central part of the Phlegrean volcanic area, close to the Solfatara crater, the Agnano plain and in front of the roughly coeval Nisida tuff cone (3.9 ka Ar–Ar; Fedele et al . 2011 ). This paper is the first report of the occurrence...
Journal Article
Journal: Geology
Published: 01 November 2006
Geology (2006) 34 (11): 937–940.
... and surrounding hills ( Barberi et al., 1978 ). The lithic-rich Breccia Museo Unit is present at the top of the eruption deposits along the caldera margins and is interpreted as a proximal deposit related to the final caldera- forming phase ( Rosi and Sbrana, 1987 ; Rosi et al., 1996 ). The objective...
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Journal Article
Journal: Geology
Published: 01 June 2016
Geology (2016) 44 (6): 487–490.
... from the underlying deposits of the Agnano Monte Spina eruption (4482–4625 yr B.P.; Smith et al., 2011 ) by a thick (>15 cm) paleosol, and from ash beds belonging to the Astroni volcano (4153–4345 yr B.P.; Smith et al., 2011 ) by an upper, 3-cm-thick humified horizon ( Figs. 1A and 1B...
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Journal Article
Published: 15 September 2014
Journal of the Geological Society (2014) 171 (6): 765–778.
... and Strombolian deposits, as well as to palagonitized hyaloclastite breccia. The shield-related units are overlain unconformably by a thick sequence of massive ignimbrites and minor pyroclastic surge deposits of basaltic to andesitic composition, which represent the syn-caldera deposits ( Martí et al . 2013...
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Journal Article
Journal: Geophysics
Published: 16 October 2015
Geophysics (2015) 80 (6): B203–B214.
... an unconfined aquifer, which is recharged by rainfall and by condensation of magmatic fluids, as also occurs at Solfatara and Agnano ( Bruno et al., 2007 ). The water table in the brownfield site is generally found at approximately 2 m deep. The granulometric composition of the sediments hosting the unconfined...
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Journal Article
Published: 01 August 2010
European Journal of Mineralogy (2010) 22 (4): 485–493.
... this period generated the Astroni tuff ring and the tephra of the complex Agnano–Monte Spina. This epoch ended 3.8 ka ago with the Senga, Averno and Astroni eruptions. The last eruption which occurred in this area is the Monte Nuovo one, in 1538. This eruption, with the widespread fumarolic and hydrothermal...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2016
GSA Bulletin (2016) 128 (7-8): 1147–1159.
... lapilli deposit [LCD]) and stratified in the upper part (upper stratified deposit [USD]); ash layers in upper stratified deposit were emplaced by pyroclastic density currents. The succession is topped by a proximal lithic breccia (Breccia Museo [BM]). Base is not exposed. (B) Representative medial Plinian...
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Journal Article
Published: 01 January 2009
European Journal of Mineralogy (2009) 21 (1): 107–116.
... ( a annite ) for the experimental biotite. Crystallization experiments were carried out on a representative sample of trachytic Breccia Museo eruption, Naples, Italy. Experiments were performed in the temperature and pressure range of 725–870 °C and 50–200 MPa, and redox conditions ranging from NNO (nickel...
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Series: Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP391.5
EISBN: 9781862396678
... lithotypes that will be discussed are: Calcare Cavernoso, which is used in Siena, San Gimignano and more sporadically in Pisa; travertine that is used in central Tuscany; Breccia of Agnano and Breccia of Caprona that are used in Pisa; and Rosso Ammonitico, which is used in some villages of the Apennines...
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Journal Article
Published: 10 June 2016
Journal of the Geological Society (2016) 173 (6): 875–888.
... explosion, might produce a small tephra ring with proximal ballistic fall deposits and numerous layers of bedded ash fall. A pronounced proximal ring would be associated with tuff breccias and numerous large blocks interbedded with occasional ash fall and density current deposits. A topographically subdued...
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