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THE FRAMEWORK OF PLATE TECTONICS  93






















            Figure 5.1  Block diagram summarizing the principal features of plate tectonics. Arrows on lithosphere represent

            relative motions. Arrows in asthenosphere may represent complementary flow in the mantle (redrawn from Isacks et
            al., 1968, by permission of the American Geophysical Union. Copyright © 1968 American Geophysical Union).
































            Figure 5.2  Worldwide distribution of epicenters of large magnitude earthquakes (m b  > 4) for the period 1961–67
            (after Barazangi & Dorman, 1969, with permission from the Seismological Society of America).



            The significance of 1961, as the start of this time   Earthquakes are classified according to their focal

            window, is that prior to the setting up of the World   depths: 0–70 km shallow focus, 70–300 km intermediate
            Wide Standardized Seismograph Network in 1961   focus, greater than 300 km deep focus.
            (Section 2.1.4), epicentral locations, particularly in   An important belt of shallow focus earthquakes
            oceanic areas, were very poorly determined. For a more   follows the crest of the ocean ridge system (Fig. 5.2),
            detailed discussion of earthquake distribution see   where focal mechanism solutions indicate tensional
            Engdahl et al. (1998).                       events associated with plate accretion and strike-slip
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