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.
Kellerwand Formation / Pondrelli, M.; Corradini, C.; Corriga, M.G.; Schönlaub, H.P.; Spalletta, C.; Pohler, S.M.L.; Mossoni, A.; Simonetto, L.; Suttner, T.J.; Perri, M.C.; Kido, E.. - In: ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT. - ISSN 0378-0864. - STAMPA. - 69:(2015), pp. 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.
