Overview

B. Pillans*

*Corresponding author for this work

    Research output: Chapter in Book/Report/Conference proceedingChapterpeer-review

    Abstract

    The general scope of stratigraphy includes all rocks, both consolidated and unconsolidated, and their organization into distinctive stratigraphic units based on their properties. Stratigraphic correlation is the process by which stratigraphic units in different places are shown to be similar in character and/or stratigraphic position. Correlation may be made on the basis of lithology, fossil content, age, or any other property, as demonstrated by the correlation of the Plio-Pleistocene boundary from its Global Stratotype Section and Point in Italy to other sections around the world. Correlation on the basis of age is dependent on evaluation of dating uncertainties and limitations. Although Quaternary stratigraphy was originally founded on the study of continental deposits, the oxygen isotope stratigraphy of deep-sea cores is the template against which almost all other stratigraphic records are now compared. Astronomical calibration provides an accurate and precise chronology of the marine isotope record. Examples of marine-terrestrial correlation are given from Wanganui Basin, New Zealand, and elsewhere in Australasia, as well as from China and western Europe.

    Original languageEnglish
    Title of host publicationEncyclopedia of Quaternary Science
    Subtitle of host publicationSecond Edition
    PublisherElsevier Inc.
    Pages189-205
    Number of pages17
    ISBN (Electronic)9780444536433
    ISBN (Print)9780444536426
    DOIs
    Publication statusPublished - 1 Jan 2013

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