https://commons.ru.ac.za/vital/access/manager/Index ${session.getAttribute("locale")} 5 https://commons.ru.ac.za/vital/access/manager/Repository/vital:4358 Wed 12 May 2021 20:02:38 SAST ]]> https://commons.ru.ac.za/vital/access/manager/Repository/vital:3759 Wed 12 May 2021 19:03:28 SAST ]]> https://commons.ru.ac.za/vital/access/manager/Repository/vital:5012 the major evolutionary changes in response to thickening and a greater rigidity of the sialic crust. Rifts are penetrative taphrogenic faults in the earths crust which act as major conduits for the transfer of magmas, from the mantle and lower crustal levels, to the upper crust and the surface. Rifts are also permeable zones for the migration of metalliferous brines, generated by magmatic differentiation. These metalliferous brines would either be exhaled at surface to form stratiform volcanogenic and volcanosedimentary ore deposits , or would interact with preferential host horizons to form stratabound ore deposits . The associat ion between rifting and stratiform and stratabound ore deposits is illustrated by examining :he tectonic setting, and st ratigraphic relationships of typical ore deposit types .]]> Wed 12 May 2021 18:01:51 SAST ]]> https://commons.ru.ac.za/vital/access/manager/Repository/vital:3363 Wed 12 May 2021 17:05:27 SAST ]]> https://commons.ru.ac.za/vital/access/manager/Repository/vital:5718 Thu 13 May 2021 05:56:54 SAST ]]> https://commons.ru.ac.za/vital/access/manager/Repository/vital:4370 Thu 13 May 2021 04:48:05 SAST ]]> https://commons.ru.ac.za/vital/access/manager/Repository/vital:5542 Thu 13 May 2021 04:32:04 SAST ]]>