Mesozoic to Cenozoic magmatic history of the Pamir

- South Pamir batholith (100-120 Ma) is attributed to low-angle subduction.
- Pamir experienced a high-flux event at ∼105 Ma.
- 70-80 Ma magmatism is attributed to slab-rollback and lithospheric extension.
- Vanj complex (36-42 Ma) is attributed to a mantle drip or delamination event.
- Pamir magmatic episodes correlate with magmatic and tectonic events in Tibet.