| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9531954 | Lithos | 2005 | 24 Pages |
Abstract
Significant differences exist between the peak-metamorphic P-T conditions recorded by samples from different lenses in the mélange, indicating that the lenses were detached from subducting lithosphere at different depths. P-T paths of eclogite-facies rocks were 'clockwise' with ca. 1.5 GPa of almost isothermal decompression.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
G.R. Fotoohi Rad, G.T.R. Droop, S. Amini, M. Moazzen,