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Structural geology and stratigraphy at the junction of the curral anticline and the moeda syncline, Quadrilatero Ferrifero, Minas Gerais, Brazil
In the map area the rocks are divided into two large subdivisions: the Archaean Nova Lima greenstone and the Bonfim granitoid gneisses, and the overlying Proterozoic Minas metasedimentary and metavolcanic rocks, including abundant iron formation. These groups are separated by a major unconformity. T...
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| Autor principal: | |
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| Formato: | Tese |
| Idioma: | Inglês |
| Publicado em: |
Michigan Technological University
1979
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| Assuntos: | |
| Acesso em linha: | http://hdl.handle.net/11422/1688 |
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