Image from OpenLibrary

The geology of the Goboboseb Mountain volcanics and their relationship to the Messum Complex, Namibia / S. C. Milner; A. Ewart

By: Contributor(s): Material type: TextTextLanguage: English Series: Communications of the Geological Survey of Namibia, Volume 5, (1989) p. 31 - 40Publication details: Windhoek : Geological Survey of Namibia, 1989,: John MeinertDescription: 10 pages : tables, fig.; 30 cmISSN:
  • 0256-1697
Subject(s): DDC classification:
  • PER 553 Communications of the Geological Survey of Namibia
Summary: The volcanics of the Goboboseb region consist of basaltic and minor intermediate lavas interbedded with silicic quartz latite units. The volcanics normally directly overlie Karoo sediments which include coarse arkosic grits, sandstones, siltsrones and shales, but occasionally overlie pre-Karoo basement schists and granites of Damaran age. This work has enabled the authors to define the stratigraphy of the Goboboseb succession, a summary of which is illustrated in this study
Tags from this library: No tags from this library for this title.
Star ratings
    Average rating: 0.0 (0 votes)
Holdings
Item type Current library Call number Status Date due Barcode
Books Books Namibia Scientific Society Library Not for loan

References

The volcanics of the Goboboseb region consist of basaltic and minor intermediate lavas interbedded with silicic quartz latite units. The volcanics normally directly overlie Karoo sediments which include coarse arkosic grits, sandstones, siltsrones and shales, but occasionally overlie pre-Karoo basement schists and granites of Damaran age. This work has enabled the authors to define the stratigraphy of the Goboboseb succession, a summary of which is illustrated in this study

A. Brückner Serie

There are no comments on this title.

to post a comment.