Seismic investigation of the transition from continental to oceanic subduction along the western Hellenic Subduction Zone
The western Hellenic subduction zone (WHSZ) exhibits well-documented along-strike variations in lithosphere density (i.e., oceanic versus continental), subduction rates, and overriding plate extension. Differences in slab density are believed to drive deformation rates along the WHSZ; however, this...
| Main Authors: | , , , , |
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| Other Authors: | |
| Format: | Article |
| Language: | en_US |
| Published: |
American Geophysical Union
2014
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| Online Access: | http://hdl.handle.net/1721.1/85853 https://orcid.org/0000-0002-6485-0026 |