Shrinking of the Cocos and Nazca Plates due to Horizontal Thermal Contraction and Implications for Plate Non-rigidity and the Non-closure of the Pacific-Cocos-Nazca Plate Motion Circuit

Richard G Gordon, Rice University, Houston, TX, United States and Corne Kreemer, University of Nevada Reno, Nevada Bureau of Mines and Geology, Reno, United States
Back to: Plate Motion, Continental Deformation, and Interseismic Strain Accumulation II