What is the crustal thickness in the Zagros region?
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The crustal thickness in the Zagros region varies across different areas. In the southwestern most Zagros Fold-Thrust Belt, the crustal thickness is around 30-35 km, increasing northeastward to 48 km. The maximum Moho depth is estimated to be around 62 km below the Zagros Mountains belt along the Main Zagros Thrust. In the Urumieh-Dokhtar magmatic arc and central Iran, the average crustal thickness is around 46 km. The crustal thickness beneath the Sanandaj-Sirjan zone varies from approximately 46 km in Western and Central Zagros to around 50 km in the easternmost part of the Zagros. Towards the northeast, the Moho depth increases to around 58 km in the Sanandaj-Sirjan zone. The crustal thickness beneath the Urumieh-Dokhtar magmatic assemblage ranges from around 50 km in the western parts to approximately 58 km in the central parts. The crustal thickness decreases again to around 47 km in Central Iran.
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| Papers (4) | Insight |
|---|---|
| The crustal thickness beneath the Ghir region in the Central Zagros is estimated to be 46 ± 2 km. | |
| The crustal thickness in the Zagros region is approximately 45-47 km, according to the seismological and gravity data presented in the paper. | |
| The crustal thickness in the Zagros region varies from approximately 46 km in the western and central parts to around 50 km in the easternmost part. There is also an increase in Moho depth to about 58 km in the Sanandaj-Sirjan zone. | |
5 Citations | The crustal thickness in the Zagros region ranges from approximately 30-35 km in the southwestern most Zagros Fold-Thrust Belt to 62 km along the Main Zagros Thrust. |
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