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Table 1
Fig. 2. Simplified geological map with the sample locations and the U–Pb geochronological results on monazite, titanite, rutile andon one zircon fraction from the Pare and Usambara Mountains, Umba Steppe and Uluguru Moutains
Fig. 3. Concordia diagram for monazite from the Pare andUsambara Mountains and the Umba Steppe
Fig. 5. Concordia diagram for monazite, titanite and rutilefrom the Umba Steppe. Different fragments of the sametitanite grain from sample A141 yield similar 207Pb/206Pb agesclose to the207Pb/206Pb age of 609�2 Ma obtained formonazite from sample A144.
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