2008
DOI: 10.1016/j.apgeochem.2008.01.005
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Impact of ancient metal smelting on arsenic pollution in the Pecora River Valley, Southern Tuscany, Italy

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Cited by 54 publications
(34 citation statements)
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“…For a detailed mineralogical and geological description, the reader is referred to Costagliola et al (2004Costagliola et al ( , 2008Costagliola et al ( , 2010, Di Benedetto et al (2006), andBenvenuti et al (2009).…”
Section: Background Information For Natural Samplesmentioning
confidence: 98%
“…For a detailed mineralogical and geological description, the reader is referred to Costagliola et al (2004Costagliola et al ( , 2008Costagliola et al ( , 2010, Di Benedetto et al (2006), andBenvenuti et al (2009).…”
Section: Background Information For Natural Samplesmentioning
confidence: 98%
“…Thus, the Tuscan mining district (Italy), which is primarily known for its Etruscan and Medieval activities (Chiarantini et al 2009;Costagliola et al 2008), appears to be a good candidate for the provenance of the copper of the lunulae from group A(I). The discovery of a copper ingot related to the Early Bronze Age near Serrabottini (Massa Marittima, Tuscany) proves that this mining district was in all likelihood exploited earlier (Aranguren and Sozzi 2005;Aranguren et al 2007).…”
Section: Evidence Of Circulation Network During the Beginning Of Thementioning
confidence: 99%
“…Amiata geothermal fields (Batini et al, 2003 and references therein) and a large number of gas(CO 2 -H 2 S)-rich thermo-mineral springs (Minissale, 2004;Minissale et al, 1997, and references therein). This tectonic setting results from the convergence and collision (CretaceousEarly Miocene) between the Adria Plate and the SardiniaCorsica Massif with the consequent stacking of the tectonic units and their subsequent compression (to the East) and extension (to the West) from the Early-Middle Miocene to Present (Elter et al, 1975;Carmignani et al, 1995Carmignani et al, , 2001, and references therein) and late-Apenninic magmatism Lattanzi et al, 1994;Costagliola et al, 2008). Historically-exploited base metal-sulfur ore deposits and S-bearing mineralizations that form the mining district of Colline Metallifere, are hosted within sedimentary and Palaezoic (phyllites) and Triassic (dolostone and gypsum/anhydrite) rocks that are covered by Ligurian Units produced by an extensional detachment occurring in Middle-Late Miocene (Arisi Rota and Vighi, 1971;.…”
Section: Geostructural Outlines Of the Study Areamentioning
confidence: 99%