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Magmatic evolution and REE mineralization in the early Cambrian Jbel Boho igneous complex in the Bou Azzer inlier (Anti-Atlas/Morocco).
Benaouda, Rachid
(2015)
Magmatic evolution and REE mineralization in the early Cambrian Jbel Boho igneous complex in the Bou Azzer inlier (Anti-Atlas/Morocco).
(PhD/ Doctoral thesis), Christian-Albrechts-Universität zu Kiel, Kiel, Germany, XXI, 140 pp.
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Abstract
The igneous rocks of Jbel Boho emerged in three phases: an initial phase with alkaline volcanism followed by the intrusion of a syenitic pluton and later the emplacement of a dyke swarm. The Jbel Boho alkaline complex shows some interesting aspects of hydrothermal REE mineralization in the late differentiation stage. REE mineralization is found in a rhyolitic dyke and some late hydrothermal veins. Synchysite-(Ce), which was identified by EPMA analysis, is the main REE mineral.
Document Type: | Thesis (PhD/ Doctoral thesis) |
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Thesis Advisor: | Devey, Colin and Geldmacher, Jörg |
Keywords: | Jbel Boho, REE mineralization, synchisite, alkaline complex, Bou Azzer, Anti-Atlas |
Research affiliation: | OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-MUHS Magmatic and Hydrothermal Systems |
Date Deposited: | 15 Nov 2016 13:37 |
Last Modified: | 25 Oct 2022 09:46 |
URI: | https://oceanrep.geomar.de/id/eprint/34714 |
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