Published March 31, 2012 | Version v1
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FIG. 3 in Rudist-bearing rhodalgal facies in the post- Turonian recovery of peri-Tethyan carbonate systems: a case history from the Nurra region (northwestern Sardinia, Italy)

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FIG. 3. — Capo Caccia section, Nurra region (northwestern Sardinia). Upper Cretaceous rudistid limestone (Cr2) disconformably over- lying the gentle karst surface of the pre-bauxite Lower Cretaceous limestone of the "Urgonian facies" (Cr1). Bauxitiferous clay (bx) fill the fault-related karst network that cuts into the bedrock.

Notes

Published as part of Simone, Lucia, Carannante, Gabriele, Bassi, Davide & Cherchi, Antonietta, 2012, Geodiversitas 34 (1) on pages 167-187, DOI: 10.5252/g2012n1a10, http://zenodo.org/record/4597287

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Journal article: 10.5252/g2012n1a10 (DOI)
Journal article: urn:lsid:plazi.org:pub:BA55B2321942275C806E405FCD71FFC8 (LSID)
Journal article: https://zenodo.org/record/4597287 (URL)