 |
| |||
| under amphibolite-facies conditions, at amphibolite facies (Later steeply dipping mylonite zones, formed under lower amphibolite-facies conditions, strike 75° and locally truncate earlier structures.; We present data from the Lewisian Complex, NW Scotland, where a suite of mafic dykes have undergone metamorphism and deformation at amphibolite facies. ArcticFox) | |||
The server is undergoing maintenance and the site is working in read-only mode. Please check back later.">Add | The server is undergoing maintenance and the site is working in read-only mode. Please check back later.">Report an error
| Get short URL | Language Selection Tips