{"id":1174,"date":"2023-12-04T20:44:33","date_gmt":"2023-12-04T20:44:33","guid":{"rendered":"https:\/\/books.gw-project.org\/structural-geology-applied-to-fractured-aquifer-characterization\/?post_type=part&#038;p=1174"},"modified":"2023-12-10T17:20:25","modified_gmt":"2023-12-10T17:20:25","slug":"1174-2","status":"publish","type":"part","link":"https:\/\/books.gw-project.org\/structural-geology-applied-to-fractured-aquifer-characterization\/part\/1174-2\/","title":{"raw":"3 Tectonic regimes, Fracture Patterns and Reactivation","rendered":"3 Tectonic regimes, Fracture Patterns and Reactivation"},"content":{"raw":"This section discusses\r\n<ul>\r\n \t<li>how the orientation of tectonic stresses near the Earth\u2019s surface, and the<\/li>\r\n \t<li>respective tectonic regimes, control the fracture orientation patterns;<\/li>\r\n \t<li>how joints, hybrid fractures and faults can be recognized on rock exposures; and,<\/li>\r\n \t<li>the reason why reactivation of existing weakness planes is a very common mechanism, causing the lithological types to strongly influence the configuration of the fracture system in a rock mass. Planes susceptible to being reactivated include an existing anisotropic feature, such as foliation, and discontinuities, such as veins or fractures.<\/li>\r\n<\/ul>","rendered":"<p>This section discusses<\/p>\n<ul>\n<li>how the orientation of tectonic stresses near the Earth\u2019s surface, and the<\/li>\n<li>respective tectonic regimes, control the fracture orientation patterns;<\/li>\n<li>how joints, hybrid fractures and faults can be recognized on rock exposures; and,<\/li>\n<li>the reason why reactivation of existing weakness planes is a very common mechanism, causing the lithological types to strongly influence the configuration of the fracture system in a rock mass. Planes susceptible to being reactivated include an existing anisotropic feature, such as foliation, and discontinuities, such as veins or fractures.<\/li>\n<\/ul>\n","protected":false},"parent":0,"menu_order":3,"template":"","meta":{"pb_part_invisible":false,"pb_part_invisible_string":""},"contributor":[],"license":[],"class_list":["post-1174","part","type-part","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/books.gw-project.org\/structural-geology-applied-to-fractured-aquifer-characterization\/wp-json\/pressbooks\/v2\/parts\/1174","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/books.gw-project.org\/structural-geology-applied-to-fractured-aquifer-characterization\/wp-json\/pressbooks\/v2\/parts"}],"about":[{"href":"https:\/\/books.gw-project.org\/structural-geology-applied-to-fractured-aquifer-characterization\/wp-json\/wp\/v2\/types\/part"}],"version-history":[{"count":11,"href":"https:\/\/books.gw-project.org\/structural-geology-applied-to-fractured-aquifer-characterization\/wp-json\/pressbooks\/v2\/parts\/1174\/revisions"}],"predecessor-version":[{"id":1879,"href":"https:\/\/books.gw-project.org\/structural-geology-applied-to-fractured-aquifer-characterization\/wp-json\/pressbooks\/v2\/parts\/1174\/revisions\/1879"}],"wp:attachment":[{"href":"https:\/\/books.gw-project.org\/structural-geology-applied-to-fractured-aquifer-characterization\/wp-json\/wp\/v2\/media?parent=1174"}],"wp:term":[{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/books.gw-project.org\/structural-geology-applied-to-fractured-aquifer-characterization\/wp-json\/wp\/v2\/contributor?post=1174"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/books.gw-project.org\/structural-geology-applied-to-fractured-aquifer-characterization\/wp-json\/wp\/v2\/license?post=1174"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}