Publication: Análisis gravimétrico y magnético de estructuras diapíricas en el offshore de la cuenca de Asturias
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Publication Date
2021
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Sociedad Geológica de España
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Abstract
En este trabajo se analizan mediante campos potenciales (gravimetría y magnetismo) las estructuras salinas interpretadas previamente en el offshore de la Cuenca de Asturias. Para ello se han realizado los mapas de anomalías y tres modelos en 2+3/4D GRAV/MAG con datos coincidentes con un cubo sísmico 3D adquirido por Repsol en 2008. El análisis cuantitativo de los mapas y la modelización en 2+3/4D ha permitido reinterpretar la estructura del basamento y de las estructuras salinas hasta ajustar la señal GRAV/MAG. Estas modificaciones son significativas por debajo de los niveles de evaporitas, destacando la necesidad de introducir menor cantidad de sal, y una reinterpretación de la geometría del techo del basamento.
In this work a potential field analysis (gravimetry and magnetism) of the salt structures interpreted in the offshore of the Asturias Basin. For this purpose, 2D processing of the anomaly maps and three models in 2+3/4D GRAV/MAG have been carried out with the data that coincide with a 3D seismic cube acquired by Repsol in 2008. The quantitative analysis of the maps and modeling has allowed the revaluation of the structure of the basement and salt structures until adjusting the GRAV/MAG signal. These modifications are significant below the levels of evaporites, highlighting the need to introduce less salt, and a new geometry of the basement top.
In this work a potential field analysis (gravimetry and magnetism) of the salt structures interpreted in the offshore of the Asturias Basin. For this purpose, 2D processing of the anomaly maps and three models in 2+3/4D GRAV/MAG have been carried out with the data that coincide with a 3D seismic cube acquired by Repsol in 2008. The quantitative analysis of the maps and modeling has allowed the revaluation of the structure of the basement and salt structures until adjusting the GRAV/MAG signal. These modifications are significant below the levels of evaporites, highlighting the need to introduce less salt, and a new geometry of the basement top.