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Isimani Suite

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Geological map of the Usagaran Belt demonstrating location of the main tect...
Published: 06 June 2019
Fig. 2. Geological map of the Usagaran Belt demonstrating location of the main tectonic units: Isimani Suite, Konse Group and Ndembera Group. The map is modified after the compilation of 56 available quarter degree sheets (QDS) by Fritz et al. (2005 ).
Image
( a ) Sketch map and evolution model of the Usagaran Belt with profile X–X′...
Published: 06 June 2019
Fig. 10. ( a ) Sketch map and evolution model of the Usagaran Belt with profile X–X′ through the Isimani Suite and profile Y–Y′ through the Ndembera Group adopted from Fritz et al. (2005) . ( b ) The Isimani Suite and northern Usagaran Belt evolved by subduction of an oceanic crust at c
Image
The chemical variation of calcic amphiboles in the basement rocks from the ...
Published: 01 June 2001
Figure 7. The chemical variation of calcic amphiboles in the basement rocks from the Kilombero Valley area and from the Isimani Suite ( Mruma, 1989 ) and from the Msolwa-, Ruhembe- and Mikumi Groups of the Kilombero Valley Karoo expressed as numbers of (Na + K) in A sites and Si atoms per
Journal Article
Published: 06 June 2019
Journal of the Geological Society (2019) 176 (5): 1007-1021.
...Fig. 2. Geological map of the Usagaran Belt demonstrating location of the main tectonic units: Isimani Suite, Konse Group and Ndembera Group. The map is modified after the compilation of 56 available quarter degree sheets (QDS) by Fritz et al. (2005 ). ...
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Journal Article
Published: 01 June 2001
South African Journal of Geology (2001) 104 (2): 137-150.
...Figure 7. The chemical variation of calcic amphiboles in the basement rocks from the Kilombero Valley area and from the Isimani Suite ( Mruma, 1989 ) and from the Msolwa-, Ruhembe- and Mikumi Groups of the Kilombero Valley Karoo expressed as numbers of (Na + K) in A sites and Si atoms per...
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Journal Article
Published: 01 September 2005
South African Journal of Geology (2005) 108 (2): 247-256.
... and amphibolites of the Isimani unit. These rocks are strongly deformed and metamorphosed under granulite-facies conditions ( Priem et al. , 1979 ; Gabert, 1984; Shackleton, 1986 ; Mruma 1989 ; Reddy et al. , 2004 ) and contain tectonically interlayered lenses of mafic and eclogitic rocks ( Möller et al...
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Journal Article
Published: 01 February 2014
American Mineralogist (2014) 99 (2-3): 443-457.
... the picked minerals; and that samples should cover a range of ferromagnesian assemblages, with the expectation that this would produce a range of ferric:ferrous ratios in the biotites. Three samples were chosen from a suite of partially retrogressed eclogites and granulites from western Tanzania. Samples T01...
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