
141 Whitish rock at the base are proximal fore-reef talus of antecedent AST and HST, which are overlain by thin (intenssely truncated) reef core (platty corals) of subsequent OST. Beds above the reef core correspond to outer-lagoon lithofacies of the HST of the subsequent 5th-order sequence. South of Cala Carril on the south east coast of Mallorca, Spain (Kendall and Pomar 2004).
| Miocene Platform Reefs of Mallorca and other Balearic
Islands / 141 South of Cala Carril Luis Pomar & Christopher Kendall 6/23/2004 http://strata.geol.sc.edu/ kendall@sc.edu |