| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4717552 | Lithos | 2008 | 24 Pages |
Abstract
Due to the fact the Western Alps do not reach the mature stage of a colliding belt, as the Central or as the Eastern Alps, the rocks of the Entrelor area can be viewed as an exhumed part of a frozen subduction channel attributed to a metamorphic mixing of rocks having different metamorphic evolution and accreted at great depths.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Romain Bousquet,