Titlebook: São Francisco Craton, Eastern Brazil; Tectonic Genealogy o Monica‘Heilbron,Umberto G. Cordani,Fernando F. Alk Book 2017 Springer Internatio

Somber

个人长篇演说

Nucleate

DRAFT

不溶解

The Paleoproterozoic Mineiro Belt and the Quadrilátero Ferríferof a Paleoproterozoic orogen preserved in the southern São Francisco craton. Siderian to Rhyacian juvenile granitoids associated with volcanic and sedimentary rocks are the main rock assemblages involved in the evolution of the Mineiro belt. The plutonic rocks characterize four distinct groups of sub

Subjugate

The Paramirim Aulacogenwn as the Chapada Diamantina in the northeastern Brazilian state Bahia. Corresponding to a long-lived and partially inverted rift-sag basin, the aulacogen hosts and exposes the most complete section of the cratonic cover complex accumulated between the Statherian and Edicaran periods. The sedimentar

跳动

轻快带来危险

Generosity

The Recôncavo-Tucano-Jatobá Rift and Associated Atlantic Continental Margin Basinspe continental margin basins, developed on the São Francisco cratonic cold lithosphere. This tectonic event finally dismembered the São Francisco-Congo cratonic bridge. The rifting tectonics reactivated Precambrian fabrics of the São Francisco Craton (the Paleoproterozoic Salvador-Itabuna-Curaçá bel

水獭

The Southern Brasília Beltrgin of the São Francisco craton in the context of the Neoproterozoic Brasiliano orogenic collage of West Gondwana. The belt is characterized by a stack of W-vergent nappes of passive margin units bounded to the west by the Archean-Paleoproterozoic Goiás microcontinent and the Neoproterozoic Mara Ro