The north cliff of Cala Pedrosa: a unique example of multiple granitoid emplacement by the magmatic stoping mechanism in the Variscan Costa Brava batholith. The darkest rocks (hornfels) were first intruded by a granodioritic magma (grey) and both the hornfels and the solidified granodiorite were subsequently intruded by leucogranites (light coloured rocks). Moreover, the whole set of rocks is cut by a lamprophyric dyke (lower left). PhotoID151<\/p>\n
Photograph: Elena Druguet<\/p>\n
Reference: mediambient.gencat.cat\/Images\/43_39667.pdf<\/p>\n","modified":"2018-06-15T10:14:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Magmatic-stoping-Costa-Brava-768x576.jpg","taxonomy":{"webmapp_category":[219]},"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\/1179","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1179&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/magmatic-stoping-costa-brava\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.218657,41.935562]}}