Iranshahr Blueschists as Results of Subduction of the Neotethys Inner Makran Oceanic Crust, SE Iran
The Makran accretionary prism extensive subduction accretions characterized by intense folding, is one of the most on Earth. It is thrust dislocation of the Cenozoic units faulting and consisted of sedimentary, igneous and metamorphic rocks. It is located in the southeast of Iran and southwest of Pa...
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| Veröffentlicht in: | Acta geologica Sinica (Beijing) 2015-12, Vol.89 (s2), p.69-69 |
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| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng |
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| Online-Zugang: | Volltext |
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| Zusammenfassung: | The Makran accretionary prism extensive subduction accretions characterized by intense folding, is one of the most on Earth. It is thrust dislocation of the Cenozoic units faulting and consisted of sedimentary, igneous and metamorphic rocks. It is located in the southeast of Iran and southwest of Pakistan. |
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| ISSN: | 1000-9515 1755-6724 |
| DOI: | 10.1111/1755-6724.12308_41 |