Tibetan garnet records early Eocene initiation of thickening in the Himalaya
Document Type
Article
Department or Administrative Unit
Geological Sciences
Publication Date
7-1-2014
Abstract
Tectonic reconstructions of the Himalayan orogeny depend on the age at which crustal thickening commenced. To investigate this age, we analyzed garnet from middle crustal rocks exposed in the north Himalayan Mabja and Kangmar gneiss domes of Tibet using Lu-Hf geochronology. Garnet yielded Lu-Hf ages of 54–52 Ma in Mabja and 51–49 Ma in Kangmar samples. On the basis of microstructural and major element and rare earth element zoning observations, the Lu-Hf ages are interpreted as recording garnet growth during contractional deformation in the middle crust at 54.3 ± 0.6 Ma, followed by variable recrystallization during subsequent high-temperature ductile extension. The new Lu-Hf ages are the first to confirm that crustal thickening and contraction in the Tibetan Himalaya was broadly synchronous with the early Eocene collision between Greater India and the Eurasian plate.
Recommended Citation
Smit, M. A., Hacker, B. R., & Lee, J. (2014). Tibetan garnet records early Eocene initiation of thickening in the Himalaya. Geology, 42(7), 591–594. https://doi.org/10.1130/g35524.1
Journal
Geology
Rights
© 2014 Geological Society of America
Comments
This article was originally published in Geology. The full-text article from the publisher can be found here.
Due to copyright restrictions, this article is not available for free download from ScholarWorks @ CWU.