Biogenic and physical sedimentary structures in latest Cambrian-earliest Ordovician mudrock facies (Famatina Range, Northwestern Argentina)

Lamination is a common feature in shales and other mud-dominated rocks. When combined with other geological evidence, the diverse lamination types can provide important information about sedimentary processes and depositional environments. Petrographic and Scanning Electron Microscope studies perfor...

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Bibliographic Details
Main Author: Susana B. Esteban
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2003-01-01
Series:Geologica Acta
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/1805