DIAGENESIS OF A RHAETIAN PATCH REEF (LOMBARDIAN BASIN, SOUTHERN ALPS)
Alternations of marine and meteoric diagenetic conditions, most probably caused by relative sea level fluctuations, are recorded in an Upper Triassic (Rhaetian) patch reef in the Calcare di Zu Formation, Lombardian Basin. Three main types of cements have been distinguished: 1)isopachous fibrous calc...
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| Formaat: | Artigo |
| Taal: | Inglês |
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Milano University Press
2017-06-01
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| Reeks: | Rivista Italiana di Paleontologia e Stratigrafia |
| Onderwerpen: | |
| Online toegang: | https://riviste.unimi.it/index.php/RIPS/article/view/8619 |
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