Diachronous initiation of Arabia–Eurasia collision from eastern Anatolia to the southeastern Zagros Mountains since middle Eocene time

Keyphrases

• Middle Eocene 100%
• Eastern Anatolia 100%
• Zagros Mountains 100%
• Late Eocene 50%
• Suture Zone 50%
• Central Anatolia 50%
• Plate Tectonic Reconstructions 50%
• Bitlis 50%
• Microcontinent 50%
• Caucasus 50%
• Northwestern Iran 50%
• Zagros 50%
• Orogen 25%
• Passive Margin 25%
• Middle Miocene 25%
• Subduction 25%
• Upper Plate 25%
• Late Oligocene 25%
• Pre-collision 25%
• Eurasia 25%
• Crustal Shortening 25%
• Continental Arc 25%
• Back-arc 25%
• Arabia 25%
• Soft Collision 25%
• Magmatic Lull 25%
• Initial Collision 25%
• Preferred Models 25%
• Early Oligocene 25%
• Zagros Suture Zone 25%
• Kinematic Constraints 25%
• Continental Underthrusting 25%
• Late Middle Eocene 25%
• Central Zagros 25%
• Eurasian Continental Margin 25%
• Plate Model 25%
• Diachroneity 25%

Earth and Planetary Sciences

• Eocene 100%
• Oligocene 50%
• Tectonic Reconstruction 50%
• Iran 50%
• Miocene 25%
• Continental Shelf 25%
• Passive Margin 25%
• Eurasia 25%
• Plate (Tectonics) 25%
• Crustal Shortening 25%
• Eurasian Plate 25%