The structure of western Serra do Curral, Quadrilátero Ferrífero, and tectonic control of the high-grade iron hard bodies

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The structure of western Serra do Curral, Quadrilátero Ferrífero, and tectonic control of the high-grade iron hard bodies

The structure of western Serra do Curral, Quadrilátero Ferrífero, represents the partial exposure of a syncline that verges to NNW - Piedade Syncline. This regional structure has parasitic folds denominated as B1A which are refolded by folds B1B that also have vergence to NNW. Both of them have ENE-...

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Bibliographic Details
Main Authors:	Sanglard, J., Rosiere, C., Santos, J., McNaughton, Neal, Fletcher, Ian
Format:	Journal Article
Published:	Universidade de Sao Paulo 2014
Subjects:	Serra do Curral Quadrilátero Ferrífero Structural geology Iron ore
Online Access:	http://hdl.handle.net/20.500.11937/12794

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