Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Mario Paolieri"'
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Cave environment allows long-term processes of rock weathering and chemical deposition that cannot occur on Earth surface directly exposed to meteoric and external biochemical agents. Apart from the common carbonate speleothems, chemical precipitatio
Externí odkaz:
https://doaj.org/article/751cf62ccf3847d0822319fbcc11dc05
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Cave environment allows long-term processes of rock weathering and chemical deposition that cannot occur on Earth surface directly exposed to meteoric and external biochemical agents. Apart from the common carbonate speleothems, chemical precipitatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::dd599980c6f3a72031ba1dc94b00f5b5
https://www.frontiersin.org/articles/10.3389/feart.2021.673109/full
https://www.frontiersin.org/articles/10.3389/feart.2021.673109/full
Mercury contamination of stream sediments in the Paglia and Tiber river catchments (Central Italy) from the abandoned Monte Amiata mining district has long been documented (Rimondi et al., 2019, and references therein). Along the river courses, fluvi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::476b942b9adbb0eba78c99b7dd47e128
https://doi.org/10.5194/egusphere-egu2020-11394
https://doi.org/10.5194/egusphere-egu2020-11394
Autor:
Francesco Di Benedetto, Marc W. Beutel, Laura Chiarantini, Giulia Pattelli, Marco Benvenuti, Mario Paolieri, Enrico Pandeli, Valentina Rimondi, John E. Gray, Giovanni Ruggieri, Pilario Costagliola, G. Gabbani, Pierfranco Lattanzi, Antonella Colica
Publikováno v:
Italian Journal of Geosciences (Online) 134 (2015): 323–336. doi:10.3301/IJG.2015.02
info:cnr-pdr/source/autori:Rimondi V.[1], Chiarantini L.[1], Lattanzi P.[2], Benvenuti M.[1], Beutel M.[3], Colica A.[1], Costagliola P.[1], Di Benedetto F.[1], Gabbani G.[1], Gray J.[4], Pandeli E.[1], Patelli G.[1], Paolieri M.[1], Ruggieri G.[5]/titolo:Metallogeny, exploitation and environmental impact of the Mt. Amiata mercury ore district (Southern Tuscany, Italy)/doi:10.3301%2FIJG.2015.02/rivista:Italian Journal of Geosciences (Online)/anno:2015/pagina_da:323/pagina_a:336/intervallo_pagine:323–336/volume:134
info:cnr-pdr/source/autori:Rimondi V.[1], Chiarantini L.[1], Lattanzi P.[2], Benvenuti M.[1], Beutel M.[3], Colica A.[1], Costagliola P.[1], Di Benedetto F.[1], Gabbani G.[1], Gray J.[4], Pandeli E.[1], Patelli G.[1], Paolieri M.[1], Ruggieri G.[5]/titolo:Metallogeny, exploitation and environmental impact of the Mt. Amiata mercury ore district (Southern Tuscany, Italy)/doi:10.3301%2FIJG.2015.02/rivista:Italian Journal of Geosciences (Online)/anno:2015/pagina_da:323/pagina_a:336/intervallo_pagine:323–336/volume:134
The Mt. Amiata mining district (Southern Tuscany, Italy) is a world class Hg district, with a cumulate production of more than 100,000 tonnes of Hg, mostly occurring between 1870 and 1980. The Hg mineralization at Mt. Amiata is younger than 0.3 Ma, a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c60258b2d69a8c3b3deeef8f7f92d78d
https://doi.org/10.3301/ijg.2015.02
https://doi.org/10.3301/ijg.2015.02
Autor:
Enrico Pandeli, Elisa Petranich, Pilario Costagliola, Marco Benvenuti, Stefano Covelli, Marc W. Beutel, Laura Chiarantini, Mario Paolieri, Valentina Rimondi, Pierfranco Lattanzi, G. Gabbani
The Orcia River basin lies north of the Mt. Amiata mining district and may receive potentially harmful/toxic elements such as mercury (Hg) and arsenic (As) therefrom. The Orcia River eventually flows to the Ombrone River, which in turn flows to the T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b670d1824fb48c25b440a290eed36864
http://link.springer.com/article/10.1007/s11270-016-3110-x
http://link.springer.com/article/10.1007/s11270-016-3110-x
Autor:
Marco Benvenuti, Luca Rossato, Pilario Costagliola, Francesco Di Benedetto, Mario Paolieri, Laura Chiarantini, Sara Bianchi
Publikováno v:
Applied Geochemistry. 23:1241-1259
A significant As anomaly has been reported in the literature for stream sediments and unlithified Quaternary deposits of the Pecora River valley in Southern Tuscany, extending from the “Colline Metallifere” pyrite-base metals district to the Tyrr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7d828d9fd46c881f465275dff6b9a87c
https://doi.org/10.1016/j.apgeochem.2008.01.005
https://doi.org/10.1016/j.apgeochem.2008.01.005
Autor:
Pierfranco Lattanzi, Francesco Di Benedetto, Valentina Rimondi, Laura Chiarantini, Massimo Rinaldi, Giulia Pattelli, Antonella Colica, Pilario Costagliola, Marco Benvenuti, Mario Paolieri
Publikováno v:
Minerals; Volume 4; Issue 2; Pages: 241-256
Minerals, Vol 4, Iss 2, Pp 241-256 (2014)
Minerals, Vol 4, Iss 2, Pp 241-256 (2014)
The Mount Amiata mining district (southern Tuscany, Italy) was, for decades, one of the world’s largest mercury (Hg) producing regions, where mining activity lasted until the 1980s. The Paglia River drains the eastern part of the district and is al
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::57d0ad4a0691c184f51c84a6a3495a97
http://hdl.handle.net/11392/2482865
http://hdl.handle.net/11392/2482865
Autor:
Pierfranco Lattanzi, Mario Paolieri, A. Salvadori, John E. Gray, Pilario Costagliola, Valentina Rimondi, M. Nannucci
Publikováno v:
Environmental science and pollution research international. 21(8)
Total dissolved and particulate mercury (Hg), arsenic (As), and antimony (Sb) mass loads were estimated in different seasons (March and September 2011 and March 2012) in the Paglia River basin (PRB) (central Italy). The Paglia River drains the Mt. Am
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::abb41029b1ceef4689a7970866890fe7
https://pubmed.ncbi.nlm.nih.gov/24414225
https://pubmed.ncbi.nlm.nih.gov/24414225
Publikováno v:
Geothermics. 21:401-413
The thermal springs discharging in the Siena-Radicofani basin and the deep fluids within the geothermal systems of Piancastagnaio (Mt Amiata), Torre Alfina and Latera (Vulsini Mts) have a common origin. The chemical composition and evolution towards
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9b3101d249046c0697206ef57db6db05
https://doi.org/10.1016/0375-6505(92)90089-r
https://doi.org/10.1016/0375-6505(92)90089-r