Journal
TECTONICS
Volume 34, Issue 4, Pages 784-802Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1002/2014TC003774
Keywords
Pamir Plateau; India-Asia collision; titanite closure; petrochronology; orogenic plateau; collapse
Categories
Funding
- National Science Foundation [EAR-0838269, 0923552, 1008760]
- DFG bundles TIPAGE [RA 442/34, 37]
- CAME (subproject TIPTIMON) from the German Federal Ministry of Education and Research [03G0809]
- Directorate For Geosciences [0923552, 1008760] Funding Source: National Science Foundation
- Division Of Earth Sciences [1008760, 0923552] Funding Source: National Science Foundation
- Division Of Earth Sciences
- Directorate For Geosciences [1419751] Funding Source: National Science Foundation
Ask authors/readers for more resources
The Pamir Plateau, a result of the India-Asia collision, contains extensive exposures of Cenozoic middle to lower crust in domes exhumed by north-south crustal extension. Titanite grains from 60 igneous and metamorphic rocks were investigated with U-Pb+trace element petrochronology (including Zr thermometry) to constrain the timing and temperatures of crustal thickening and exhumation. Titanite from the Pamir domes records thickening from similar to 44 to 25Ma. Retrograde titanite from the Yazgulem, Sarez, and Muskol-Shatput domes records a transition from thickening to exhumation at similar to 20-16Ma, whereas titanite from the Shakhadara dome records prolonged exhumation from similar to 20 to 8Ma. The synchronous onset of exhumation may have been initiated by breakoff of the Indian slab and possible convective removal of the Asian lower crust and/or mantle lithosphere. The prolonged exhumation of the Shakhdara and Muztaghata-Kongur Shan domes may have been driven by continued rollback of the Asian lithosphere concurrent with shortening and northwestward translation of the Pamir Plateau.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available