Zobrazeno 1 - 10
of 61
pro vyhledávání: '"Schönlaub, H. P."'
Autor:
Pondrelli, M., Corradini, C., Spalletta, C., Suttner, T. J., Simonetto, L., Perri, M. C., Corriga, M. G., Venturini, C., Schönlaub, H. P.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::c35e9604a5f50a7193e8cda195209660
https://hdl.handle.net/11368/2950668
https://hdl.handle.net/11368/2950668
Autor:
Pondrelli, M., Corradini, C., Spalletta, C., Suttner, T. J., Schönlaub, H. P., Pas, D., Kido, E., Corriga, M. G., Mossoni, A., Simonetto, L., Pohler, S. M. L., Perri, M. C., Farabegoli, E., Da Silva Ac, Dojen, C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::712a1d584dffecf473a0a421c36aacdb
https://hdl.handle.net/11368/2950621
https://hdl.handle.net/11368/2950621
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::479c5b3bf708e67af4d86cb8943589cd
https://hdl.handle.net/11368/2950564
https://hdl.handle.net/11368/2950564
Autor:
Pondrelli, M., Schönlaub, H. P., Corradini, C., Spalletta, C., Suttner, T. J., Kido, E., Perri, M. C., Simonetto, L., Corriga, M. G., Mossoni, A., Pohler, S. M. L., Hüneke, H
The Hoher Trieb Formation consists of five well-bedded facies listed below: Facies A: medium dark gray very thick-bedded rudstone and floatstone; matrix consists mainly of grainstone; silicified corals are common among the clasts; Facies B: medium da
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::3ea9c55f241a7c29769d15962cd88402
http://hdl.handle.net/11585/545591
http://hdl.handle.net/11585/545591
Autor:
Suttner, T. J., Bandel, K., Corradini, C., Corriga, M. G., Kido, E., Pohler, S. M. L., Pondrelli, M., Schönlaub, H. P., Simonetto, L., Vai, G. B.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::cb46b1c53159aa50f64de557bc4558c7
https://www.geologie.ac.at/produkte-shop/detail/?id=1729&seo=band_69
https://www.geologie.ac.at/produkte-shop/detail/?id=1729&seo=band_69
Autor:
Corradini, C., Corriga, M. G., Pondrelli, M., Schönlaub, H. P., Simonetto, L., Spalletta, C., Ferretti, A
The Rauchkofel Formation mainly consists of dark gray to black laminated and well-bedded, partly platy limestones intercalated with black shales and marls of various thickness. Lateral variations are common. Thickness of beds varies from very thin to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::bfa3090273b5c90476687f8df54e0352
https://hdl.handle.net/11380/1076616
https://hdl.handle.net/11380/1076616