| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8911783 | Lithos | 2018 | 67 Pages |
Abstract
Rates and durations obtained for seafloor spreading (175 ± 25 Ma), subduction (125 ± 75 Ma) and continental collision (ca. 60 Ma) are similar to those observed in Phanerozoic Wilson Cycle but differ from what was estimated for Archean terrains. Therefore, timespans of the different steps of a Wilson cycle might have progressively changed over time as a response to the progressive cratonization of the lithosphere.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Gautier Nicoli, Emilie Thomassot, Mathias Schannor, Adrien Vezinet, Ivan Jovovic,