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Geological and geodynamic models of the mantle often rely on joint interpretations of published seismic tomography images and petrological/geochemical data. This approach tends to neglect the fundamental limitations of, and uncertainties in, seismic tomography results. These limitations and uncertainties involve theory, correcting for the crust, the lack of rays throughout much of the mantle, the...
Terra Nova, 00, 1–7, 2010
AbstractThe C‐isotope composition of a Miocene carbonate succession from the Latium‐Abruzzi sector of the Central Apennines was studied to evaluate the influence of local vs. global factors in changing δ13C. We propose that the Oligo‐Miocene igneous activity of the Western Mediterranean and the closure of the Indo‐Pacific connection influenced climate change and Mediterranean...
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