Relict basin closure accommodates continental convergence with minimal crustal shortening or deceleration of plate motion as inferred from detrital zircon provenance in the Caucasus

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ADS bibcode
2016AGUFM.T51A2883C
year
2016
Listed Authors
Cowgill, E.
Forte, A. M.
Niemi, N. A.
Avdeev, B.
Tye, A. R.
Trexler, C. C.
Javakhishvili, Z.
Elashvili, M.
Godoladze, T.
Listed Institutions
University of California Davis, Davis, CA, United States
School of Earth and Space Exploration, Arizona State University, Tempe, AZ, United States
University of Michigan Ann Arbor, Ann Arbor, MI, United States
University of Michigan Ann Arbor, Ann Arbor, MI, United States
University of Michigan Ann Arbor, Ann Arbor, MI, United States
Earth and Planetary Sciences, University of California Davis, Davis, CA, United States
Institute of Earth Sciences and National Seismic Monitoring Centre, Ilia State University, Tbilisi, Georgia
Ilia State University, Tbilisi, Georgia
Institute of Earth Sciences and National Seismic Monitoring Centre, Ilia State Univeristy, Tbilisi, Georgia

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