Výsledky vyhledávání - "Benvenuti M.[2]"

Black pine (Pinus nigra) barks as biomonitors of airborne mercury pollution

Autor: Chiarantini L.[1, Rimondi V.[1, Benvenuti M.[2], Beutel M.W.[3], Costagliola P.[2], Gonnelli C.[4], Lattanzi P.[5], Paolieri M.[2]

Publikováno v: Science of the total environment 569-570 (2016): 105–113. doi:10.1016/j.scitotenv.2016.06.029
info:cnr-pdr/source/autori:Chiarantini L.[1,2], Rimondi V.[1,2], Benvenuti M.[2], Beutel M.W.[3], Costagliola P.[2], Gonnelli C.[4], Lattanzi P.[5], Paolieri M.[2]/titolo:Black pine (Pinus nigra) barks as biomonitors of airborne mercury pollution./doi:10.1016%2Fj.scitotenv.2016.06.029/rivista:Science of the total environment/anno:2016/pagina_da:105/pagina_a:113/intervallo_pagine:105–113/volume:569-570

Tree barks are relevant interfaces between plants and the external environment, and can effectively retain airborne particles and elements at their surface. In this paper we have studied the distribution of mercury (Hg) in soils and in black pine (Pi

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fd98ff89f57905abf80ee4755719a705
https://doi.org/10.1016/j.scitotenv.2016.06.029

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Mercury dispersion through streams draining the Mt. Amiata district, southern Tuscany, Italy

Autor: Lattanzi P.[1], Rimodia V.[1], Chiarantini L.[1], Colica A.[2], Benvenuti M.[2], Costagliola P.[2], Ruggieri G.[1]

Publikováno v: Procedia earth and planetary science 17 (2017): 468–471.
info:cnr-pdr/source/autori:Lattanzi P.[1], Rimodia V.[1], Chiarantini L.[1], Colica A.[2], Benvenuti M.[2], Costagliola P.[2], Ruggieri G.[1]/titolo:Mercury dispersion through streams draining the Mt. Amiata district, southern Tuscany, Italy/doi:/rivista:Procedia earth and planetary science/anno:2017/pagina_da:468/pagina_a:471/intervallo_pagine:468–471/volume:17

The Mt. Amiata area hosts the 3rd largest Hg district in the world, overlapping with a present-day geothermal system that is exploited for energy production. Mining activity ceased in 1980; remediation of mining areas was only partial, and is still u

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::63eef257a591f1db297ee6c9ff7eeaa8
https://www.journals.elsevier.com/procedia-earth-and-planetary-science/

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Analisi archeometriche su un frammento in marmo proveniente da Chiusi (SI): contributo alle conoscenze sugli scambi commerciali tra Etruria e mondo greco-orientale nel periodo arcaico

Autor: Cappuccini L.[1], Aminti F.[1], Benvenuti M.[2], Lazzarini L.[3], Iozzo M.[4]

Publikováno v: Atti III Congresso Nazionale AIAr "L'archeometria in Italia La scienza per i beni culturali", pp. 141–149, Bressanone, Italia, 11-12 febbraio 2004
info:cnr-pdr/source/autori:Cappuccini L.[1], Aminti F.[1], Benvenuti M.[2], Lazzarini L.[3], Iozzo M.[4]/congresso_nome:Atti III Congresso Nazionale AIAr "L'archeometria in Italia La scienza per i beni culturali"/congresso_luogo:Bressanone, Italia/congresso_data:11-12 febbraio 2004/anno:2005/pagina_da:141/pagina_a:149/intervallo_pagine:141–149

no presente

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::22f413977fa3e3fecad55ad2365c0a41
https://publications.cnr.it/doc/111834

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Magmatic versus hydrothermal processes in the formation of raw ceramic material deposits in southern Tuscany

Autor: Lattanzi P. (1), Benvenuti M. (2), Costagliola P. (2), Maineri C. (2), Mascaro I. (2), Tanelli G. (2), Dini A. (3), Ruggieri G. (4)

Publikováno v: Tenth International Symposium on Water-Rock Interaction, pp. 725–728, Villasimius, Italy, 10-15 July 2001
info:cnr-pdr/source/autori:Lattanzi P. (1), Benvenuti M. (2), Costagliola P. (2), Maineri C. (2), Mascaro I. (2), Tanelli G. (2), Dini A. (3), Ruggieri G. (4)/congresso_nome:Tenth International Symposium on Water-Rock Interaction/congresso_luogo:Villasimius, Italy/congresso_data:10-15 July 2001/anno:2001/pagina_da:725/pagina_a:728/intervallo_pagine:725–728

Ceramic raw material in Tuscany is currently mined in four main deposits (Marciana and La Crocetta in Elba Island, Botro ai Marmi near Campiglia Marittima, and Piloni di Torniella near Roccastrada). The deposits are associated with magmatic rocks of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::1ae1f036673f2c22a3315d9c50678a64
https://publications.cnr.it/doc/214076

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Mineral assemblages in the Hg-Zn-(Fe)-S system at Levigliani, Tuscany, Italy

Autor: Dini A. (1), Benvenuti M. (2), Lattanzi P. (2),Tanelli G. (3)

Publikováno v: European journal of mineralogy
7 (1995): 417–427.
info:cnr-pdr/source/autori:Dini A. (1); Benvenuti M. (2), Lattanzi P. (2),Tanelli G. (3)/titolo:Mineral assemblages in the Hg-Zn-(Fe)-S system at Levigliani, Tuscany, Italy/doi:/rivista:European journal of mineralogy (Print)/anno:1995/pagina_da:417/pagina_a:427/intervallo_pagine:417–427/volume:7

A number of minerals of the Hg-Zn-(Fe)-S system occur in the Hg deposit at Levigliani (Apuane Alps, northern Tuscany). The deposit is hosted within phyllitic and metavolcanic rocks of Paleozoic age, which were intensely deformed and metamorphosed to

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::5ab70b231922bda7dcc1bcd528e59554
http://eurjmin.geoscienceworld.org/content/7/2/417.extract

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Fluid circulation in the Apuane Alps core complex; evidence from extension veins in the Carrara Marble

Autor: Costagliola P. (1), Benvenuti M. (2, Maineri C. (2, Lattanzi P. (3, Ruggieri G. (5)

Publikováno v: Mineralogical magazine
63 (1999): 111–122. doi:10.1180/minmag.1999.063.1.11
info:cnr-pdr/source/autori:Costagliola P. (1), Benvenuti M. (2,3), Maineri C. (2,3), Lattanzi P. (3,4), Ruggieri G. (5)/titolo:Fluid circulation in the Apuane Alps core complex; evidence from extension veins in the Carrara Marble/doi:10.1180%2Fminmag.1999.063.1.11/rivista:Mineralogical magazine (Print)/anno:1999/pagina_da:111/pagina_a:122/intervallo_pagine:111–122/volume:63

In the Apuane Alps (AA) metamorphic core complex, syn-metamorphic mineral deposits are mainly restricted to extensional shear zones in the Lower Plate Palaeozoic basement. By contrast, the extension structures at upper levels, such as the detachment

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Kniha

Author Index.

Autor: Knipe, A. C., Watts, W. E.

Publikováno v: Organic Reaction Mechanisms Series (9780471937944); 1993, p551-593, 43p

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Unravelling basin shoulder dynamics through detrital apatite fission-track signature: the case of the Quaternary Mugello Basin, Italy

Autor: Maria Laura Balestrieri, Rita Catanzariti, Marco Benvenuti

Publikováno v: Geological magazine (Online) (2017). doi:10.1017/S0016756817000073
info:cnr-pdr/source/autori:Balestrieri M.L.[1], Benvenuti M.[2], Catanzariti R.[3]/titolo:Unravelling basin shoulder dynamics through detrital apatite fission-track signature: the case of quaternary Mugello basin, Italy./doi:10.1017%2FS0016756817000073/rivista:Geological magazine (Online)/anno:2017/pagina_da:/pagina_a:/intervallo_pagine:/volume

Detrital apatite fission-track (AFT) thermochronology has been applied to lower Pleistocene lacustrine fan-delta sediments of the NE shoulder of the Mugello Basin, the youngest and closest to the main watershed among the Northern Apennines intermonta

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0255c23b62c4dc864b90dd818515819c
https://doi.org/10.1017/s0016756817000073

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The structural hinge of a chain-foreland basin: Quaternary activity of the Pede-Apennine Thrust front (Northern Italy)

Autor: Daniele Maestrelli, Stefano Carnicelli, Federico Sani, Marco Bonini, Luigi Piccardi, Marco Benvenuti

Publikováno v: Tectonophysics (Amst. Online) 723 (2018): 117–135. doi:10.1016/j.tecto.2017.12.006
info:cnr-pdr/source/autori:Maestrelli D.[1,2] Benvenuti M.[2] Bonini M.[3], Carnicelli S.[2], Piccardi L.[3], Sani F. [2,3]/titolo:The structural hinge of a chain-foreland basin: Quaternary activity of the Pede-Apennine Thrust front (Northern Italy)/doi:10.1016%2Fj.tecto.2017.12.006/rivista:Tectonophysics (Amst. Online)/anno:2018/pagina_da:117/pagina_a:135/intervallo_pagine:117–135/volume:723

The Pede-Apennine margin (Northern Italy) is a major WNW-ESE-trending morpho-structural element that delimits the Po Plain to the southwest and consists of a system of southwest dipping thrusts, generally referred to as Pede-Apennine Thrust (PAT). Th

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Late Miocene shortening of the Northern Apennines back-arc

Autor: Federico Sani, Marco Benvenuti, Giovanni Menanno, Marco Bonini, Chiara Tanini, Eusebio Stucchi, Giovanna Moratti

Publikováno v: Journal of geodynamics 74 (2014): 1–31. doi:10.1016/j.jog.2013.11.002
info:cnr-pdr/source/autori:Bonini M.[1], Sani F.[2], Stucchi E.M.[3], Moratti G.[1], Benvenuti M.[2], Menanno G.[3], Tanini C.[4]/titolo:Late Miocene shortening of the Northern Apennines back-arc/doi:10.1016%2Fj.jog.2013.11.002/rivista:Journal of geodynamics/anno:2014/pagina_da:1/pagina_a:31/intervallo_pagine:1–31/volume:74

The inner Northern Apennines (western Tuscany and Tyrrhenian basin) is characterized by a relatively thin continental crust (∼20–25 km), high heat flow (>100 mW m−2), and the presence of relevant tectonic elision of stratigraphic sequences, a s

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