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The Somali crystalline basement in northern Somalia contains a Neoproterozoic igneous suite essentially composed of gabbros with minor syenitic and granitic bodies. This Gabbro-Syenite Suite (GSS) was emplaced at a relatively high crustal level and is related to Late Precambrian crustal extension. The basic plutons are composed mostly of gabbro with petrographic and geochemical characteristics ranging...
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