Age of the Batoka basalts, northern Zimbabwe, and the duration of Karoo Large Igneous Province magmatism-Reference-Cited by-同舟云学术

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Age of the Batoka basalts, northern Zimbabwe, and the duration of Karoo Large Igneous Province magmatism

Published:2001-02 Issue:2 Volume:2 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Jones D. L.¹,Duncan R. A.,Briden J. C.²,Randall D. E.³⁴,MacNiocaill C.⁴

Affiliation:

1. Department of Physics; University of Zimbabwe; Harare Zimbabwe

2. Environmental Change Institute; University of Oxford; Oxford, England United Kingdom

3. British Antarctic Survey, High Cross; Madingley Road, Cambridge, England United Kingdom

4. Department of Earth Sciences; University of Oxford; Oxford, England United Kingdom

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference21 articles.

1. Paleomagnetism of the Nuanetsi igneous province and its bearing upon the sequence of Karroo igneous activity in southern Africa;Brock;J. Geophys. Res.,1968

2. The geology of the Nuanetsi igneous province;Cox;Philos. Trans. R. Soc. London, Ser. A,1965

3. Geochemical and petrological provinces in the Karoo basalts of southern Africa;Cox;Am. Mineral.,1967

4. The timing and duration of the Karoo igneous event, southern Gondwana;Duncan;J. Geophys. Res.,1997

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