The Plio-Pleistocene boundary; is there a case for its relocation near the Gauss-Matuyama magnetic reversal?

Author(s): Partridge, Tim
Author Affiliation(s): Primary:
University of the Witwatersrand, Climatology Research Group, Johannesburg, South Africa
Volume Title: International Union for Quaternary Research XIV international congress; abstracts
Source: Terra Nostra (Bonn), Vol.2-95, p.211; International Union for Quaternary Research XIV international congress, Berlin, Germany, Aug. 3-10, 1995. Publisher: Alfred-Wegener-Stiftung, Bonn, Germany. ISSN: 0946-8978
Note: In English
Year of Publication: 1995
Research Program: ODP Ocean Drilling Program
Key Words: 24 Surficial Geology, Quaternary Geology; Asia; Cenozoic; China; Chronostratigraphy; Clastic sediments; Far East; GSSP; Gauss Chron; Geochemistry; Global Stratotype Section and Point; Isotopes; Loess; Lower Pleistocene; Matuyama Chron; Neogene; Ocean Drilling Program; Paleoclimatology; Paleoenvironment; Paleomagnetism; Pleistocene; Pliocene; Quaternary; Sedimentation; Sediments; Stratigraphic boundary; Tertiary; Upper Cenozoic; Upper Pliocene
Record ID: 2020024986
Copyright Information: GeoRef, Copyright 2020 American Geosciences Institute.

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