| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6442179 | Precambrian Research | 2016 | 8 Pages |
Abstract
The most likely interpretation is that these successions predate the Pampean orogeny and deposition of the Cambrian Puncoviscana Formation. Consequently, the rocks could either have been deposited within the (passive) margin of the Arequipa-Antofalla-Western Pampeanas terrane (western Gondwana) or MARA block; or are unusual, reworked sedimentary rocks related to the active continental margin of the Pampean orogen.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
T. Naidoo, U. Zimmermann, J. Vervoort,