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English

Field data indicate that the dolomitization of the Middle Aptian to Early Albian shallow marine carbonates in the Benicàssim area (SE Maestrat Basin) resulted in massive stratiform to sub-stratiform tabular bodies, up to 150-m-thick, that extend for several thousand square meters.

Spanish

Los datos de campo indican que la dolomitización de los carbonatos marinos de edad Aptiense Medio-Albiense Inferior de la zona de Benicàssim (SE Cuenca del Maestrat) originó cuerpos tabulares, estratiformes a sub-estratiformes, que alcanzan 150 m de espesor.