Large-Scale Crustal-Block-Extrusion During Late Alpine Collision
Abstract The crustal-scale geometry of the European Alps has been explained by a classical subduction-scenario comprising thrust-and-fold-related compressional wedge tectonics and isostatic rebound. However, massive blocks of crystalline basement (External Crystalline Massifs) vertically disrupt the...
Saved in:
Main Authors: | , , , , |
---|---|
Format: | article |
Language: | EN |
Published: |
Nature Portfolio
2017
|
Subjects: | |
Online Access: | https://doaj.org/article/a0dfb31a2f0841e3a64f5f43a90182f3 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|