Abstract
Examination of the provisional metamorphic map of Zambia shows the existence of two major metamorphic belts. One, the ‘Lufilian Belt’, parallels the Lufilian structural arc, while the other, the ‘LuangwaKariba Belt’, includes parts of the ‘Zambezi’, ‘Irumide’ and ‘Mozambique’ tectonic belts. Structural, metamorphic and geochronological considerations suggest that the whole of the Luangwa-Kariba Belt forms part of the Mozambique orogenic belt.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
