1887

Abstract

In onshore Almada Basin, northeast Brazil, sandy and/or conglomeratic turbidites and shales outcrops of Urucutuca Formation occur. These rocks are part of an exhumed portion of the filling-section of the Almada Canyon, which is well mapped by seismic studies in offshore part.

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/content/papers/10.3997/2214-4609-pdb.160.SBGF129
2005-09-11
2020-02-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.160.SBGF129
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