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by saracarena1 in nature-plants
Lowstand (cross-bedded oolitic alcarenites and then fining upward sequence) and highstand (carbonatic turbidites) system tracts in the more marginal part of the Agua Amarga sedimentary basin. The transgressive system tract, present in basinward outcrops, here is absent. Los Pacos hill, Agua Amarga, Almeria region, southern Spain.