GC8RN6X-#1 PR4-MAC - SOS1 - MEIOS TERRESTRES
In this place it can be observed in the metassediments of the metagrave and mycasis unit, focused on the previous point, the intrusion of a very fine granitic (aplitic) lode, composed, in general, by quartz, feldspars and muscovite.
This lode has a morphology close to vertical and a thickness of a few metres. It is characterized by not being deformed and was dated 308 million years through the isotopes uranium lead.
N 39º 29' 3.721'' W 8º 2' 39.721''
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