Relict basin closure accommodates continental convergence with minimal crustal shortening or deceleration of plate motion as inferred from detrital zircon provenance in the Caucasus
E. Cowgill, Tea Godoladze(Ilia State University), Adam M. Forte(Louisiana State University), Mikheil Elashvili(Ilia State University), Nathan A. Niemi(University of Michigan), Alexander Tye(Jet Propulsion Laboratory), Charles C. Trexler(Planetary Science Institute), B. Avdeev(Environmental Research Institute of Michigan), Z. Javakhishvili(Ilia State University)
AGU Fall Meeting Abstracts
December 1, 2016
Cited by 3
Related Papers
Constraints on the volatile distribution within Shackleton crater at the lunar south pole
|Nature|2012|204
Relict basin closure and crustal shortening budgets during continental collision: An example from Caucasus sediment provenance
|Tectonics|2016|127
Low variability runoff inhibits coupling of climate, tectonics, and topography in the Greater Caucasus
|Earth and Planetary Science Letters|2022|25