Seismic investigation of the transition from continental to oceanic subduction along the western Hellenic Subduction Zone

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...

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Bibliographic Details
Main Authors: Pearce, Frederick Douglas, Rondenay, S., Sachpazi, M., Charalampakis, M., Royden, Leigh H
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: American Geophysical Union 2014
Online Access:http://hdl.handle.net/1721.1/85853
https://orcid.org/0000-0002-6485-0026

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http://hdl.handle.net/1721.1/85853
https://orcid.org/0000-0002-6485-0026

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