.png){kind=icon}
.png){kind=icon}
Return
100 Million years of tectonic evolution along the Bitlis-Pütürge Suture
.png){kind=icon}
OA
AI
A
D
N
A
DOI：10.1016/j.gr.2026.06.014.png)
.png){kind=icon}
.png){kind=icon}
Share.png){kind=icon}
Save
Abstract
En 中文
• Multimineral U-Pb geochronology elucidates ∼100 Ma of Arabia-Eurasia convergence. • Coeval magmatism, HP metamorphism, and exhumation in the Late Cretaceous and Eocene. • Zircon Hf isotopes reveal reworking of Cadomian crust during Neotethys convergence. • Dynamic mantle support beneath eastern Anatolia from 13 Ma sustained plateau uplift. • Enhanced sediment flux at ∼14–6 Ma marks intense orogen growth and plateau uplift.
Keywords:
Orogenic evolution
Neotethys closure
Arabia-Eurasia convergence
Bitlis-Pütürge Suture
Integrated geochronology
AI Summary
Key information extracted from the uploaded paper, including a brief overview, abstract, background, key highlights, visual analysis, and future outlook.
Journal
IF:
8.6
Papers:
4.3K
Citations:
2.1W
Organization
Cited Papers