Bioclastic wackestone represents the major part of the formation. In the lower part of the formation also iron-coated bioclasts and micritic oncoids occur abundantly. The bedding is mostly obliterated by bioturbation (Schönlaub et al., 2004; Hüneke, 2006, 2007).
Spalletta, C., Schönlaub, H., Pondrelli, M., Corradini C. (2015). Valentin Formation. ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT, 69, 133-136.
Valentin Formation
SPALLETTA, CLAUDIA;
2015
Abstract
Bioclastic wackestone represents the major part of the formation. In the lower part of the formation also iron-coated bioclasts and micritic oncoids occur abundantly. The bedding is mostly obliterated by bioturbation (Schönlaub et al., 2004; Hüneke, 2006, 2007).File in questo prodotto:
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