Relict basin closure and crustal shortening budgets during continental collision: An example from Caucasus sediment provenanceEric Cowgill, Tea Godoladze, B. Avdeev et al.|Tectonics|2016Cited by 127
Diverse Deformation Mechanisms and Lithologic Controls in an Active Orogenic Wedge: Structural Geology and Thermochronometry of the Eastern Greater CaucasusAlexander Tye, Gulam Babayev, Fakhraddin Kadirov et al.|Tectonics|2022Cited by 15
A LOW-TEMPERATURE THERMOCHRONOMETRIC PERSPECTIVE ON THE SUBDUCTION-TO-COLLISION TRANSITION IN THE CAUCASUS REGIONNathan A. Niemi, Rafiq Safarov, Eric Cowgill et al.|Abstracts with programs - Geological Society of America|2019Cited by 0
Formation of the Greater Caucasus by two-stage closure of a relict ocean basin and the transition from soft to hard Arabia-Eurasia collisionEric Cowgill, Tea Godoladze, Z. Javakhishvili et al.|EGUGA|2018Cited by 0