Wind-pattern circulation as a palaeogeographic indicator: Case study of the 1.5–1.6 Ga Mangabeira Formation, São Francisco Craton, Northeast Brazil

Author:

Bállico M.B.,Scherer C.M.S.,Mountney N.P.,Souza E.G.,Chemale F.,Pisarevsky S.A.,Reis A.D.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference111 articles.

1. Proterozoic first-order sedimentary sequences of the São Francisco craton, eastern Brazil;Alkmim;Marine Petrol. Geol.,2012

2. A classification scheme for fluvial–aeolian system interaction in desert-margin settings;Al-Masrahy;Aeolian Res.,2015

3. O Cráton do São Francisco;Almeida;Rev. Bras. Geociências,1977

4. Babinski, M., Pedreira, A.J., Brito Neves, B.B., Van Schmus, W.R., 1999. Contribuição à geocronologia da Chapada Diamantina. In: Pedreira, A.J. (Ed.). VII Simpósio Nacional de Estudos Tectônicos. Brazilian Geological Society, pp. 118–120.

5. Drying-upward cycles in a Mesoproterozoic aeolian erg-margin succession: Mangabeira Formation, Espinhaço Supergroup, Brazil;Bállico;Sed. Geol.,2017

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