| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4727047 | Gondwana Research | 2013 | 10 Pages |
Abstract
⺠High grade gneisses thought to be Precambrian crust are shown to be younger. ⺠Queen Maud batholith magmatism commenced by ~ 535 Ma and stretched into Ordovician. ⺠Documented events coincide with widespread tectonic changes in Gondwana.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
T.S. Paulsen, J. Encarnación, A.M. Grunow, V.A. Valencia, M. Pecha, P.W. Layer, C. Rasoazanamparany,