Anisotropic magnetite growth in remagnetized limestones: Tectonic constraints and implications for basin history

Author:

Calvín Pablo1,Villalaín Juan J.1,Casas-Sainz Antonio M.2

Affiliation:

1. Departamento de Física, Universidad de Burgos, Av/ Cantabria s/n, 9006 Burgos, Spain

2. Geotransfer Research Group (IUCA), Universidad de Zaragoza, C/ Pedro Cerbuna 12, 50009 Zaragoza, Spain

Publisher

Geological Society of America

Subject

Geology

Reference18 articles.

1. Paleostress evolution in the Moroccan African margin from Triassic to Present;Ait-Brahim;Tectonophysics,2002

2. Diachronous folding and cleavage in an intraplate setting (Central High Atlas, Morocco) determined through the study of remagnetizations;Calvín;Journal of Structural Geology,2017

3. The origin of tectonic fabrics in “undeformed” clays: The early stages of deformation in extensional sedimentary basins;Cifelli;Geophysical Research Letters,2004

4. Remagnetization and chemical alteration of sedimentary rocks;Elmore,2012

5. Les structures “diapiriques” liasiques du Haut-Atlas central, Maroc: Example de la ride d’Ikerzi;Ettaki;Africa Geoscience Review,2007

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