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Formations penetrated at Site 372 are compared with series cropping out on land in the Balearic Islands, Southern Spain, and Sardinia. The comparison is extended to wells drilled in the Gulf of Lion. The margin at Menorca and the North Balearic Provencal Basin appear to be at least of Burdigalian age. The entire Miocene is undisturbed at Site 372 in contrast to Mallorca and continental Spain where important tectonic events occurred during middle and upper Miocene.

Comparison between Formations Drilled at DSDP Site 372 in the Western Mediterranean and Exposed Series on Land