{"type":"Feature","properties":{"id":7514,"name":"S-C mylonites in the Calamita Schists","description":"<p><img loading=\"lazy\" class=\"wp-image-7515 aligncenter\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-300x225.jpg\" alt=\"\" width=\"793\" height=\"595\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-1536x1152.jpg 1536w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-2048x1536.jpg 2048w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-1080x810.jpg 1080w\" sizes=\"(max-width: 793px) 100vw, 793px\" \/><br \/>\nS-C mylonites developed in andalusite-cordierite micaschist (Calamita Schists) in the contact aureole of the Porto Azzurro pluton. The white layers are made of quartz, while the brown layers consist predominantly of white mica and biotite. Top-to-left (East) sense of shear.<\/p>\n<p><strong>Photo credits:<\/strong> Samuele Papeschi<\/p>\n<p><strong>References:<\/strong><br \/>\nPapeschi, S., Musumeci, G., &amp; Mazzarini, F. (2017). Heterogeneous brittle-ductile deformation at shallow crustal levels under high thermal conditions: The case of a synkinematic contact aureole in the inner northern Apennines, southeastern Elba Island, Italy.\u00a0<i>Tectonophysics<\/i>,\u00a0<i>717<\/i>, 547-564. https:\/\/doi.org\/10.1016\/j.tecto.2017.08.020<\/p>\n<p>Papeschi, S., Musumeci, G., &amp; Mazzarini, F. (2018). Evolution of shear zones through the brittle-ductile transition: The Calamita Schists (Elba Island, Italy).\u00a0<i>Journal of Structural Geology<\/i>,\u00a0<i>113<\/i>, 100-114. https:\/\/doi.org\/10.1016\/j.jsg.2018.05.023<\/p>\n","modified":"2020-07-04T14:40:47","color":"","icon":"","noDetails":false,"noInteraction":false,"imageGallery":[{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-1024x768.jpg","id":7515,"caption":""}],"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-1024x768.jpg","taxonomy":{"webmapp_category":[234,231]},"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\/7514","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7514&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/s-c-mylonites-in-the-calamita-schists\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.382609525860213,42.71506838353767]}}