Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4728065 | Gondwana Research | 2006 | 24 Pages |
Abstract
The lithological association and the available isotopic data registered in the Carecuru Domain suggests a geodynamic evolution model based on the development of a magmatic arc system during the Transamazonian orogenic cycle, which was accreted to the southwestern border of the Archean Amapá Block.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Lúcia T. da Rosa-Costa, Jean M. Lafon, Claude Delor,