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The Kal-e-Kafi intrusive complex is located in the Central Iran magmatic zone and includes a series of granitoid rocks ranging in composition from gabbro to granite. These granitoids show some affinities with adakites, e.g., high Sr/Y and La/Yb ratios coupled with low Yb and Y, enrichment in LREE and LILE with no Eu anomalies, similar to products from all of which are compatible with derivation from...
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