Ordovician magnetostratigraphy - A correlation of global data

Allan Trench, W.S. Mckerrow, Trond Torsvik

Research output: Contribution to journalArticle

21 Citations (Scopus)

Abstract

Palaeomagnetic studies where primary magnetizations are established from well-dated rocks have been compiled to construct a magnetostratigraphic time-scale for the Ordovician period. An excellent correlation of magnetozones is observed between independent studies of the Baltic and South Siberian platform sequences. Supplemental datasets from other continents concur with the Baltic and Siberian polarity data.

Early Ordovician times were mainly characterized by a reverse field. Rapid reversals then occurred during Llanvirn and Llandeilo times. Late Ordovician times were dominated by a normal polarity field.

Some gaps remain in the polarity record, notably for late Caradoc-early Ashgill and mid-Tremadoc times.
Original languageEnglish
Pages (from-to)949-957
Number of pages9
JournalJournal of the Geological Society, London
Volume148
Publication statusPublished - 1991

Fingerprint Dive into the research topics of 'Ordovician magnetostratigraphy - A correlation of global data'. Together they form a unique fingerprint.

  • Cite this