Abstract (EN):
The aim of this study was to establish the three-dimensional shape of Águas Frias (AF) pluton
using the interpretation of the gravity data and the modelling of the obtained residual anomaly.
The relationship between the granites from AF pluton and Vila Pouca de Aguiar laccolith, which
is located SSW from the former, is also discussed, in order to understand its emplacement mechanisms.
AF pluton is a thick and deeply rooted body and its main volume is located under the
outcrop of the two-mica granite. The AF granite was fed through a deep conduit located at the
centre of the pluton, and then the biotitic granite and the two-mica granite are two different
facies, which probably had the same feed zone. VPA and AF plutons, similar in mineralogical,
chronological and magnetic features, are joined together in depth and were fed through feeding
zones located within the NNE-SSW Penacova-Régua -Verin Fault (PRVF).
The shapes from the two granite plutons are quite different: VPA pluton is laccolithic and AF
pluton belongs to the wedge-floored pluton type. Gravity data also suggest that AF pluton is
more rooted than VPA pluton. We consider that this difference can be related to the great depth
of PRVF in the sector of Chaves
Language:
English
Type (Professor's evaluation):
Scientific
Notes:
Key words: granite, post-tectonic, gravimetric, and modelling