The Kellerwand Formation consists of four well-bedded facies listed in order of decreasing abundance. Facies A: medium dark gray, thin to medium-bedded, wackestone to packstone with moderate yellow thin laminae of silt; Facies B: medium dark gray, thin to thick bedded, often fining upward, moderately to well sorted and locally laminated grainstone (from very coarse up to granules to fine-grained) to packstone; Facies C: medium light gray, medium to thick bedded, moderately to well sorted crinoidal-bearing grainstone (biosparite); Facies D: medium dark gray, thick bedded, poorly sorted coral-bearing rudstone with clasts up to about 10 cm of diameter and poorly sorted very coarse to fine grainstone matrix.
Pondrelli, M., Corradini, C., Corriga, M., Schönlaub, H., Spalletta, C., Pohler, S., et al. (2015). Kellerwand Formation. ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT, 69, 109-112.
Kellerwand Formation
SPALLETTA, CLAUDIA;PERRI, MARIA CRISTINA;
2015
Abstract
The Kellerwand Formation consists of four well-bedded facies listed in order of decreasing abundance. Facies A: medium dark gray, thin to medium-bedded, wackestone to packstone with moderate yellow thin laminae of silt; Facies B: medium dark gray, thin to thick bedded, often fining upward, moderately to well sorted and locally laminated grainstone (from very coarse up to granules to fine-grained) to packstone; Facies C: medium light gray, medium to thick bedded, moderately to well sorted crinoidal-bearing grainstone (biosparite); Facies D: medium dark gray, thick bedded, poorly sorted coral-bearing rudstone with clasts up to about 10 cm of diameter and poorly sorted very coarse to fine grainstone matrix.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
