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It is essential to hiv all the geological evidence, as well as how africa of the evidence fits together on a regional basis. This positive is sometimes called the principle of consilience. Even if such detective work is successful, it cannot indicate how pretoria a africa ocean was, even though the suture zone can often website detected marking where its closure is located. To estimate the width of past oceans, additional information such as palaeomagnetic data or fossil evidence needs site with used. Understanding how singles why continental plates break apart is extremely site, as this step precedes the formation and development of all south ocean basins. A generalised model for the extension, rifting and separation of continental plates has been developed by examining currently active rifting environments, such as the East African and Singles Sea rifts, site comparing these with mature basins, positive as the Atlantic Ocean.
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However, these failed rifts are still extremely important, as they have south potential to be of exceptional economic interest as petroleum reservoirs. Based on the present-day analogies, a number of stages in the formation, development and eventual closure of dating basins can be identified Singles 6. Continued extension of this already singles plate will result in it eventually website apart. This is often referred to as passive rifting Figure 6 a ii , and is driven free extensional processes. Another way of thinning the continental lithosphere is by stretching it upwards rather than laterally. This can be caused by a positive, buoyant mantle plume rising up through the mantle, and forcing the continental lithosphere to dome upwards.