The paleo-lacustrine diatomaceous deposits of Monte Amiata volcano (Tuscany, Italy) and the Ezio Tongiorgi paleontological collection in the Museum of Natural History of the University of Pisa

Autor: Vezzoli L.[1, Principe C.[1], Sorbini C.[3]

Publikováno v: Annals of geophysics (Testo stamp.) 64 (2021): 1–25. doi:10.4401/ag-8634
info:cnr-pdr/source/autori:Vezzoli L.[1,2], Principe C.[1], Sorbini C.[3]/titolo:The paleo-lacustrine diatomaceous deposits of Monte Amiata volcano (Tuscany, Italy) and the Ezio Tongiorgi paleontological collection in the Museum of Natural History of the University of Pisa/doi:10.4401%2Fag-8634/rivista:Annals of geophysics (Testo stamp.)/anno:2021/pagina_da:1/pagina_a:25/intervallo_pagine:1–25/volume:64

At the foothillof Monte Amiata volcano (southern Tuscany, Italy), small extinct lake basins of late Pleistocene age are documented. These lake basins were characterized by the deposition of two very different types of sediment: a) derived from the au

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d2f85dfa73746c27fd142497c2297be8
https://doi.org/10.4401/ag-8634