{"type":"Feature","properties":{"id":7005,"name":"syntectonic granite sheets","description":"<div id=\"attachment_7002\" style=\"width: 310px\" class=\"wp-caption alignnone\"><img aria-describedby=\"caption-attachment-7002\" loading=\"lazy\" class=\"size-medium wp-image-7002\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-1080x810.jpg 1080w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-7002\" class=\"wp-caption-text\">Syntectonic granite sheets Salknappen, Antarctica.<\/p><\/div>\n<div id=\"attachment_7006\" style=\"width: 310px\" class=\"wp-caption alignnone\"><img aria-describedby=\"caption-attachment-7006\" loading=\"lazy\" class=\"size-medium wp-image-7006\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-1080x810.jpg 1080w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-7006\" class=\"wp-caption-text\">Syntectonic granite sheets at Salknappen, Antarctica<\/p><\/div>\n<p>Steeply dipping discordant pegmatite veins are crosscut by layering parallel granite sheets along which extensional top to South syntectonic displacement has occurred at ~490Ma. Person at bottom for scale. Extensional shears parallel to the pegmatite veins are evident.<\/p>\n","modified":"2019-06-07T22:53:34","color":"","icon":"","noDetails":false,"noInteraction":false,"taxonomy":{"webmapp_category":[224,219,231]},"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\/7005","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7005&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/syntectonic-granite-sheets\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[1.00582449859985,-72.323492195148]}}