Sedimentation and pedogenic features in a clay deposit in Quadrilátero Ferrífero, Minas Gerais, Brazil
The clay deposit of Caxambu Hill occurs in a NW/SE oriented graben originated by syntectonic sedimentation during Cenozoic. Four facies were identified (fragmentary, nodular, massive and friable) and their differentiation is related to gravity mass-flow processes. The fragmentary facies is composed...
Na minha lista:
| Udgivet i: | Anais da Academia Brasileira de Ciências |
|---|---|
| Principais autores: | , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Academia Brasileira de Ciências
2004
|
| Fag: | |
| Online adgang: | https://www.redalyc.org/articulo.oa?id=32776113 |
| Tags: |
Ingen Tags, Vær først til at tagge denne postø!
|