| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5784276 | Lithos | 2017 | 72 Pages |
Abstract
The migmatization and the low pressure metamorphic overprint are related here to two main tectonic events: an early Paleozoic tectonic pulse produced by subduction of the oceanic crust of the Iapetus Ocean beneath northwestern Gondwana, and an Upper Triassic to Lower Jurassic tectonic pulse produced by subduction of oceanic crust of the proto-Pacific ocean beneath western Pangaea.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
C.A. Zuluaga, S. Amaya, C. Urueña, M. Bernet,