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The Mediterranean region represents a complex mosaic of continental, microcontinental and ophiolitic terranes, whose overall evolution has been controlled by relative movements between the African and Eurasian plates. Palaeomagnetic studies have played an important part in deciphering the sequence of tectonic events in this region. The 33 papers presented here span the full width of the Mediterranean basin and present results from Permian to Quaternary rocks.
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Not some eldrich Lovecrafted monster or high-tech Hollywood virtual creation, nor even de-hibernating earth itself has made the most impact when it rose from the ocean depths, says Lawrence, a freelance journalist with a background in biology and geology. It has been the theories of the geological history of the plant. He narrates the development of the theory of plate tectonics from its continental- drift larval stage to its mainstream triumph in the later 1960s. Annotation copyrighted by Book News Inc., Portland, OR.