An East Africa origin for Madagascar: evidence from zircon U-Pb geochronology and geochemistry of Neoarchean gneisses and granitoids from the Maevatanana greenstone belt in Madagascar

<strong>Table 1 </strong>Results of zircon U–Pb dating of sample G1 from the melanosome bands in the gneiss <strong>Table 2 </strong>Results of zircon U–Pb dating of sample M33 from the Neoarchean granitoids <strong>Table 3 </strong>Zircon Hf isotopic data for the melanosome bands in the gneiss <strong>Table 4 </strong>Zircon Hf isotopic data for Neoarchean granitoids <strong>Table 5 </strong>Major element (wt%), trace element (ppm), and REE (ppm) composition of the melanosome bands in the gneiss <strong>Table 6 </strong>Major element (wt%), trace element (ppm), and REE (ppm) composition of the Neoarchean granitoids