p. 1−1
2645-4963
Vol.18/No.71
p. 3−8
2645-4963
Vol.18/No.71
0.60) suggests that this complex can be considered to contain a significant potential for economic and metallurgical chromite. Furthermore, the complex does not contain chromitites of uniform composition in chalcophile elements. PGE patterns of peridotites in the study area also show that these units in upper parts of the Gaft area are similar to ultramafic cumulates of oceanic crust, while in lower parts of Faroumad area related to mantle sequences.]]>
p. 9−12
2645-4963
Vol.18/No.71
p. 13−19
2645-4963
Vol.18/No.71
p. 19−30
2645-4963
Vol.18/No.71
p. 31−44
2645-4963
Vol.18/No.71
p. 45−52
2645-4963
Vol.18/No.71
p. 53−62
2645-4963
Vol.18/No.71
p. 63−68
2645-4963
Vol.18/No.71
p. 69−80
2645-4963
Vol.18/No.71
p. 81−84
2645-4963
Vol.18/No.71
p. 85−90
2645-4963
Vol.18/No.71
p. 91−96
2645-4963
Vol.18/No.71
p. 97−104
2645-4963
Vol.18/No.71
p. 105−114
2645-4963
Vol.18/No.71
p. 115−122
2645-4963
Vol.18/No.71
p. 123−128
2645-4963
Vol.18/No.71
p. 129−136
2645-4963
Vol.18/No.71
p. 137−142
2645-4963
Vol.18/No.71
p. 143−148
2645-4963
Vol.18/No.71
p. 149−154
2645-4963
Vol.18/No.71
p. 155−159
2645-4963
Vol.18/No.71
p. 160−166
2645-4963
Vol.18/No.71
p. 167−172
2645-4963
Vol.18/No.71
p. 173−177
2645-4963
Vol.18/No.71