| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4729588 | Journal of African Earth Sciences | 2006 | 21 Pages |
Abstract
The crust of the Arabian-Nubian Shield (ANS) was formed in oceanic settings in the Mozambique Ocean during the Neoproterozoic (c. 0.9–0.6 Ga). Convergence started to coalesce island arcs, closed the ocean, and continental collision followed (
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
U.B. Andersson, W. Ghebreab, M. Teklay,