Article ID Journal Published Year Pages File Type
6445135 Journal of Structural Geology 2011 13 Pages PDF
Abstract
► Separation of paramagnetic and diamagnetic subfabrics in highly deformed carbonates. ► Strong correlation between calcite CPO and strength of the diamagnetic sub fabric. ► Separated subfabrics are linked to Neogene orogen parallel extensional deformation. ► Partial tectonic overprint weakens the overall magnetic anisotropy and texture intensity
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Preview
Magnetic anisotropy reveals Neogene tectonic overprint in highly strained carbonate mylonites from the Morcles nappe, Switzerland
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