is emphasised and an explanation of its amplitude characteristics is provided in terms of a lower crust exhibiting a gradual increase of velocity with depth. The average crustal velocity along the line of the south west England peninsula and between Land's End and Brittany is about 6.1 km/sec with an upper crustal velocity of about 5.8 km/sec. The crust is about 27 to 28 km thick with an almost horizontal Moho and a sub Moho P(_n) velocity of about 8.07 km/sec.
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