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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)

appsOther research productkeyboard_double_arrow_right Image 31 Mar 2012Publisher:Zenodo
Authors: Simone, Lucia; Carannante, Gabriele; Bassi, Davide; Cherchi, Antonietta;

doi: 10.5281/zenodo.4597294 , 10.5281/zenodo.4597293

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)

Abstract

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.

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

Keywords

Biodiversity, Taxonomy

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popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
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