Sub-basaltic weathering, damsites, palaeomagnetism, and the age of lateritization

P. W. Schmidt, D. T. Currey, C. D. Oilier

    Research output: Contribution to journalArticlepeer-review

    49 Citations (Scopus)

    Abstract

    Investigations described from three Victorian damsites indicate that weathering of Ordovician bedrock is increased where it is overlain by basalt, even though the basalt is little weathered. Sub-basaltic weathering may account for the fact that weathered rock beneath a Jurassic lava flow gives a weathering remagnetization age of Mid-Cainozoic, consistent with palaeomagnetically determined ages of lateritization from elsewhere in Australia.

    Original languageEnglish
    Pages (from-to)367-370
    Number of pages4
    JournalJournal of the Geological Society of Australia
    Volume23
    Issue number4
    DOIs
    Publication statusPublished - 1976

    Fingerprint Dive into the research topics of 'Sub-basaltic weathering, damsites, palaeomagnetism, and the age of lateritization'. Together they form a unique fingerprint.

    Cite this