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Reverse magnetic anomaly controlled by Permian Igneous rocks in the Iberian Chain (N Spain)

Two important reverse dipolar magnetic anomalies in the Iberian Chain (Spain) are located over Permian igneous rocks. A detailed study of one of them, the Loscos magnetic anomaly, where the geological structure is well constrained, reveals that source of the anomaly must be a reverse remanent magnet...

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發表在:Geologica Acta: an international earth science journal
Principais autores: P. Calvín, A. M. Casas, J.J. Villalaín, P. Tierz
格式: Artigo
語言:Inglês
出版: Universitat de Barcelona 2014
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在線閱讀:https://www.redalyc.org/articulo.oa?id=50531655004
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