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...
Sábháilte in:
| Foilsithe in: | Geologica Acta: an international earth science journal |
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| Príomhchruthaitheoir: | |
| Formáid: | Artigo |
| Teanga: | Inglês |
| Foilsithe / Cruthaithe: |
Universitat de Barcelona
2003
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| Ábhair: | |
| Rochtain ar líne: | https://www.redalyc.org/articulo.oa?id=50510108 |
| Clibeanna: |
Níl clibeanna ann, Bí ar an gcéad duine le clib a chur leis an taifead seo!
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