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Elsevier, Global and Planetary Change, (212), p. 103794, 2022

DOI: 10.1016/j.gloplacha.2022.103794

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Mercury enrichments of the Pyrenean foreland basins sediments support enhanced volcanism during the Paleocene-Eocene thermal maximum (PETM)

This paper was not found in any repository, but could be made available legally by the author.
This paper was not found in any repository, but could be made available legally by the author.

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