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- W1891541954 abstract "The catchment of the Pecora River is located between the townsof Follonica and Massa Marittima (Southern Tuscany, Italy) and ischaracterized by Neogene-Quaternary strata resting unconformablyon a pre-Neogene substratum. A critical geological re-interpretationof this area indicates that the Quaternary succession, composed by arelatively thin veneer of terrigenous deposits and by calcareous tufas,is the result of five major stages of drainage reorganization. The datafrom this study indicate that, similarly to present, the paleo-catchmentof the Pecora River included the Arsenti Mount area, locatedfew km eastward from Massa Marittima, and that was constantlyseparated from the nearby Bruna River.This new re-interpretation of the Quaternary evolution of thePecora River area has several implications, in particular on thenature of the arsenic anomaly known in this area and mainly confinedto the fluvial terrigenous deposits. Specifically, the erosion anddispersal of As-bearing mineralization emplaced between the latePliocene and the Quaternary in fractures and faults affecting thebedrock of the Arsenti Mount area, was possibly driven by the sedimentarydevelopment of the Pecora River catchment resulting in thelandforms and deposits described in this study. As a consequence,the As anomaly known in this area may have resulted from fully naturalphenomena such as relief denudation and sediment dispersal." @default.
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- W1891541954 date "2009-02-01" @default.
- W1891541954 modified "2023-09-26" @default.
- W1891541954 title "Quaternary evolution of the Pecora River (southern Tuscany, Italy): paleohydrography and sediments provenance" @default.
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- W1891541954 doi "https://doi.org/10.3301/ijg.2009.128.1.61" @default.
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