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Rb- Sr geochronology of the Middle to Late Proterozoic Awasib Mountain terrane / B. G. Hoal; R. E. Harmer; B. M. Eglington

By: Contributor(s): Material type: TextTextLanguage: English Series: Communications of the Geological Survey of South West Africa/Namibia, Volume 2, (1986) p. 53 - 59Publication details: Windhoek : Geological Survey of South West Africa/ Namibia, 1986Description: 7 pages : tables, fig.; 30 cmISSN:
  • 0256-1697
Subject(s): DDC classification:
  • PER 553 Communications of the Geological Survey of Namibia
Summary: The Awasib Mountain terrane consists essentially of a pertly deformed amd metamorphosed volcano-sedimentary succession with associated high level plutons in a rifted basement that is probably of Namaqua age. The volcano-sedimentary sequence is correlated with the Sinclair Sequence, the type area of which is situated immediately to the east. This psper reports the initial findings of this study, in which Rb- Sr isotopes have been determidut for four suites of samples
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The Awasib Mountain terrane consists essentially of a pertly deformed amd metamorphosed volcano-sedimentary succession with associated high level plutons in a rifted basement that is probably of Namaqua age. The volcano-sedimentary sequence is correlated with the Sinclair Sequence, the type area of which is situated immediately to the east. This psper reports the initial findings of this study, in which Rb- Sr isotopes have been determidut for four suites of samples

Geological Survey of South West Africa/ Namibia Serie

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