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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 geologicalevidence, the diverse lamination types can provide important information about sedimentary processes anddepositional environments. Petrographic and Scanning Electron Microscope studies performe...
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| Pubblicato in: | Geologica Acta: an international earth science journal |
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| Autore principale: | |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Universitat de Barcelona
2003
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| Soggetti: | |
| Accesso online: | https://www.redalyc.org/articulo.oa?id=50510108 |
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