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Título

Constraining the geometry at depth of La Maladeta and Andorra-Mont Louis granites (Central Pyrenees) through gravity modelling

AutorAyala, C. CSIC ORCID ; Clariana, Pilar; Soto, Ruth CSIC ORCID ; Martí Molist, Joan CSIC ORCID ; Margalef, A.; Pueyo Morer, Emilio Luis CSIC ORCID; Rubio Sánchez-Aguililla, Félix Manuel; Rey Moral, María del Carmen; Bach-Oller, Nuria CSIC ; Schamuells, Stefania CSIC; Cires, J.
Palabras claveCentral Pyrenees
La Maladeta
Andorra-Mont Louis granites
Fecha de publicación4-may-2020
CitaciónEGU General Assembly 2020: EGU2020-5688 (2020)
ResumenIn the Central Pyrenees, where density contrast between the Paleozoic rocks and the intruded granitic bodies is measurable, geological cross-sections constrained with gravity data help to unravel the subsurface geometry of the granites. With this goal in mind, during 2018 and 2019 several gravimetric surveys were carried out in the Central Pyrenees to improve the existent spatial resolution of the gravity data from the databases of the Spanish and Catalan Geological Surveys, especially in La Maladeta and Andorra Mont-Louis granites¿ area. After the gravity reductions, we obtained the Bouguer gravity anomaly from which we calculated the residual gravity anomaly by subtracting a third degree polynomial which represents the regional anomaly in agreement with the geometry of the crust in this region. The gravimetric response over La Maladeta and Andorra Mont-Louis granites is markedly dissimilar pointing out differences in the composition and geometry at depth of the two granites. La Maladeta granite shows a gravimetric zonation with small variations in its amplitude from one zone to the next, consistent with small lateral changes in its composition, predominantly granodioritic. By contrast, the Andorra Mont-Louis pluton is characterized by a relative minimum suggesting a more granitic composition. With respect to the inferred geometry at depth, the results obtained from gravity modelling show that the La Maladeta granite displays a laccolithic shape with its basal contact deeping to the North whereas the Andorra Mont-Louis granite has a more batholitic shape. Although the emplacement age of both granites is similar (Late Carboniferous ¿ Early Permian), their different geometry at depth suggests that either (1) their emplacement mechanisms were different or (2) the subsequent Alpine orogeny affected both granites in different ways better preserving the original geometry of the Andorra Mont-Louis granite.
DescripciónEGU General Assembly 2020, Online, 4-8 may 2020
Versión del editorhttps://doi.org/10.5194/egusphere-egu2020-5688
URIhttp://hdl.handle.net/10261/232582
DOI10.5194/egusphere-egu2020-5688
Identificadoresdoi: 10.5194/egusphere-egu2020-5688
Aparece en las colecciones: (Geo3Bcn) Comunicaciones congresos
(IGME) Comunicaciones congresos




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