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Volatile-bearing ultramafic to mafic xenoliths from the Kerguelen archipelago (southern Indian ocean): evidence for carbonatites in the mantle

✍ Scribed by B. Moine; M. Gregoire; J.-Y. Cottin; S.M.F. Sheppard; S.Y. O'Reilly; A. Giret


Book ID
104354087
Publisher
Elsevier Science
Year
2001
Tongue
English
Weight
116 KB
Volume
32
Category
Article
ISSN
1464-343X

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✦ Synopsis


Carbonatites in Southern

Malawi belong to the late stage intrusion of the Chilwa Alkaline Province of Upper Jurassic to Lower Cretaceous. They are characterised by a circular zone of fenitised rocks in which carbonate rocks, ijolites and alkaline rocks derived from nephelinitic lavas intruded forming igneous ring complex structures. Major Economic minerals, which are found in the carbonatites, are rare earth minerals, apatite and pyrochlore.