Gisburn Anticline - Highland Geology Limited
14978
page-template-default,page,page-id-14978,page-child,parent-pageid-15268,bridge-core-2.8.7,qode-page-transition-enabled,ajax_fade,page_not_loaded,,qode-child-theme-ver-1.0,qode-theme-ver-27.1,qode-theme-bridge,disabled_footer_top,disabled_footer_bottom,wpb-js-composer js-comp-ver-6.6.0,vc_responsive

Gisburn Anticline

Prospectivity in Ribblesdale Fold Belt. The strike line E86E-39 trending SW-NE across Gisburn Anticline (axis red dashed) is interpreted here using the classic model of Boyer and Elliott (1982).

Two lateral ramps connected by a floor-fault form a shape which forces the observed fold geometry into the northward-pushed cover sequence. Even where the seismic is difficult to pick at depth, the geometry at intra-Chatburn level (blue) is a good guide to structure style at basement level.

Bowland/Craven trends map

Previous page