Implications from a new continuous astronomically calibrated geological time scale back to ~42 Myrs (abstract of invited talk presented at AGU Fall Meeting, San Francisco, 8-12 Dec 2003)

Precise, orbitally calibrated geological time scales form a pre-requisite to further our understanding of phase relationships between orbitally driven climatic processes, and to decipher the detailed mechanisms that interact to encode orbitally forced (Milankovitch) processes in the geological recor...

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Bibliographic Details
Main Authors: Pälike, H. (Author), Moore, T.C (Author), Backman, J. (Author), Raffi, I. (Author), Parés, J.M (Author), Lanci, L. (Author), Shackleton, N.J (Author)
Format: Article
Language:English
Published: 2003.
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