Parallel fold in the Cretaceous Tralonca Flysch. This fold belongs to the D3 local deformation event, occurring after the main greenschist-facies metamorphic peak. Axial-plane spaced cleavage is well-developed in shale layers, while it is nearly absent in limestone-rich layers.
\nPhotoID438<\/p>\n
Photograph: Ivan Zibra<\/p>\n
Reference: Zibra (2006). Late-Hercynian granitoid plutons emplaced along a deep crustal shear zone. A case study from the S. Lucia nappe (Alpine Corsica, France). PhD. thesis<\/p>\n","modified":"2018-06-30T13:01:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/ivan-zibra-768x483.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1717","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1717&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/ivan-zibra\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.227056503295898,42.30986302053201]}}