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- W4377087094 abstract "Tethyan evolution is characterized by cyclical continent-transfer from Gondwana to the continents in the Northern Hemisphere, similar to a “one-way” train. Subduction has been viewed as the primary driver of transference. Therefore, it is important to understand the tectonic evolution of all past subduction zones that occurred along Eurasia's southern margin. We studied the earliest known eclogite located at the NeoTethyan suture in the Iranian segment. A prograde-E-MORB-like eclogite reached a peak metamorphic condition of 2.2 GPa and 560°C, at 190 ± 11 Ma (1σ rutile U-Pb ages), which constrains the youngest age for subduction initiation of the NeoTethyan slab. Combined with regional magmatic and structural data, the oldest age for NeoTethys subduction initiation is 210–192 Ma, which is younger than the Paleo-Tethyan closure time of 228–209 Ma. These data, used with previous numerical modeling, support collision-induced subduction initiation. The collision-induced force, together with the Paleo-Tethyan subduction-driven mantle flow, is likely to have exploited weak inherited structures from earlier NeoTethyan rifting, resulting in a northward directed subduction zone along the southern margin of the Central Iran Block." @default.
- W4377087094 created "2023-05-20" @default.
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- W4377087094 date "2023-05-19" @default.
- W4377087094 modified "2023-10-12" @default.
- W4377087094 title "When and Why the NeoTethyan Subduction Initiated Along the Eurasian Margin" @default.
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- W4377087094 doi "https://doi.org/10.1002/9781119773856.ch9" @default.
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