| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6443722 | Gondwana Research | 2013 | 14 Pages |
Abstract
⺠Northern protoliths were Carboniferous, whereas in the south deposition was Permian. ⺠Detrital zircon LuHf and O isotopes indicate mature crustal igneous source rocks. ⺠Devonian accretion north of 39°S was coeval with subduction to the south.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
F. Hervé, M. Calderón, C.M. Fanning, R.J. Pankhurst, E. Godoy,