Kinematic Analysis of the Nain and Darrech Deh Faults and Their Structural Position in the Western Side of the Central Iranian Range
The western margin of Central Iran – the Nain area – is composed of the Mesozoic ophiolitic mélanges deposited during the Late Cretaceous. The Nain and Darrech Deh faults whose trace indicators can be seen in the study area are among the largest faults therein. These faults have a north-northwest s...
| Main Authors: | , , , |
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| Formato: | Artigo |
| Idioma: | English |
| Publicado: |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2024-06-01
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| Series: | Геодинамика и тектонофизика |
| Subjects: | |
| Acceso en liña: | https://www.gt-crust.ru/jour/article/view/1854 |