{"type":"Feature","properties":{"id":1783,"name":"shear bands in calcsilicate","description":"<p>Calcsilicates (top and bottom) of the Camel Hills metamorphics, with an age of appr. 2000 Ma. The deformation fabric is a weak steep foliation and weak subhorizontal E-W trending lineation in calcsilicate. A granite vein (centre) is affected by ductile dextral D1-shear bands, which grade into brittle dextral shear fractures in the calcsilicate. Granite is of Wooramel or Moorarie age. Width of view 1m<br \/>\nPhotoID476<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:05:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/shear-bands-in-calcsilicate-768x502.jpg","taxonomy":{"webmapp_category":[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\/1783","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1783&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/shear-bands-in-calcsilicate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.574667,-25.575333]}}