Abstract
The Sistan Suture Zone of eastern Iran is a Cretaceous to Tertiary orogenic belt that formed by closure of a northwards-projecting arm of the Neo-Tethys ocean. Disrupted ophiolitic rocks within the subduction complex include a tectonic mélange of metamorphic rocks dominated by metabasites, metacherts, and metaspilites. The latter rocks occur as small (
Original language | English |
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Pages (from-to) | 1-24 |
Number of pages | 23 |
Journal | Lithos |
Volume | 84 |
Issue number | 1-2 |
DOIs | |
Publication status | Published - Sept 2005 |
Keywords
- Blueschist
- Eclogite
- Metachert
- Ophiolite
- P-T path