@article{10272/8583,
year = {2006},
url = {http://hdl.handle.net/10272/8583},
abstract = {The Aguablanca stock is located in the NE zone of the Santa Olalla Igneous Complex, in the Ossa-Morena
Zone. Paleozoic rocks of the Bodonal-Cala Complex and Santa Olalla tonalites bound this gabbronorite
stock. This rock hosts a Ni-Cu-EGP ore deposit. A gravity survey, Bouguer anomaly map production and
3D gravity modelling have been carried out in the area in order to investigate de Aguablanca stock geometry.
The residual gravity map exhibits a gravity high related to the gabbronorite of Aguablanca, a denser rock
than the surroundings, as well as to the semi-massive sulphides outcrops. As featured in the 3D density
model, the Aguablanca stock has a tabular geometry subparallel to its northern limit, deeping to 1850 m.
In its upper part the igneous body spreads and adopts a circular shape. The Aguablanca stock emplacement
is related to a variscan ductile shear zone},
title = {Modelo gravimétrico tridimensional del “stock” de Aguablanca (Badajoz)},
title = {A 3D gravity model of the Aguablanca stock (Badajoz)},
author = {Romeo, I. and Tejero López, Rosa and Capote, Ramón and Lunar Hernández, Rosario and Martínez, Q.},
}