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).
Valentin Formation / Spalletta, C.; Schönlaub, H.P.; Pondrelli, M.; Corradini C.. - In: ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT. - ISSN 0378-0864. - STAMPA. - 69:(2015), pp. 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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