Existence of Kfeldspar megacrysts and mafic microgranitoid inclusions in this intrusion, high abundances of La and Ce, V enrichement in mafic terms and low whole rock 87Sr/86Sr ratios of this body, suggested a partial melting of mantle wedge, subducted oceanic crust (metabasaltic sources) or lower continental crust (metatonalitic sources ...
![whatsapp](/images/whatsapp.png)