Biogenic and physical sedimentary structures in latest Cambrian-earliest Ordovician mudrock facies (Famatina Range, Northwestern Argentina)
Esteban, S. B. (Universidad Nacional de Tucumán. Facultad de Ciencias Naturales)

Date:	2003
Abstract:	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 performed in the latest Cambrian- earliest Ordovician lower Member of the Volcancito Formation (Famatina Range) have revealed three distinct types of lamination in mudrocks. Thick horizontal lamination (.
Rights:	Aquest document està subjecte a una llicència d'ús Creative Commons. Es permet la reproducció total o parcial, la distribució, la comunicació pública de l'obra i la creació d'obres derivades, sempre i quan aquestes es distribueixin sota la mateixa llicència que regula l'obra original i es reconegui l'autoria.
Language:	Anglès
Document:	Article ; recerca ; Versió publicada
Subject:	Late Cambrian-Early Ordovician ; Mudrocks ; Biogenic and physical lamination ; Famatina Range ; NW Argentina
Published in:	Geologica acta, Vol. 1, Num. 1 (2003) , p. 85-94, ISSN 1696-5728

Adreça alternativa: https://raco.cat/index.php/GeologicaActa/article/view/82156
Adreça alternativa: https://revistes.ub.edu/index.php/GEOACTA/article/view/1805
DOI: 10.1344/105.000001594

10 p, 6.9 MB

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