{"type":"Feature","properties":{"id":1727,"name":"ivan zibra","description":"
Layered gabbro sheared under granulite-facies conditions. The tectonic foliation is nearly parallel to the primary compositional layering. White layers are anorthositic; dark layers are hornblenitic and layers with intermediate color index are gabbroic to gabbro-noritic. A brown-weathered Opx porphyroclast occur in the central hornblendite layer.
\nPhotoID443<\/p>\n
Photograph: Ivan Zibra<\/p>\n
Reference: Reference: Zibra I, Kruhl JH, Braga R (2010). Late Palaeozoic deformation of post-Variscan lower crust: shear zone widening due to strain localization during retrograde shearing. Int J Earth Sci (Geol Rundsch) DOI 10.1007\/s00531-009-0441-5<\/p>\n","modified":"2018-09-16T10:32:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/ivan-zibra-5-768x552.jpg","taxonomy":{"webmapp_category":[232,234]},"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\/1727","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1727&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/ivan-zibra-6\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.212851524353027,42.31287792063872]}}