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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| container_title | Acta geologica Sinica (Beijing) |
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| creator | Moazzen, Mohssen Omrani, Hadi |
| description | 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. |
| doi_str_mv | 10.1111/1755-6724.12308_41 |
| format | Article |
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| fulltext | fulltext |
| identifier | ISSN: 1000-9515 |
| ispartof | Acta geologica Sinica (Beijing), 2015-12, Vol.89 (s2), p.69-69 |
| issn | 1000-9515 1755-6724 |
| language | eng |
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| source | Wiley Online Library Journals Frontfile Complete; Alma/SFX Local Collection |
| subjects | Marine Oceanic crust 伊朗 巴基斯坦 断裂作用 新特提斯 洋壳俯冲 蓝片岩 逆冲断层 马克兰 |
| title | Iranshahr Blueschists as Results of Subduction of the Neotethys Inner Makran Oceanic Crust, SE Iran |
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