Geodynamic implications of the Cenozoic stress field on Seymour Island, West Antarctica

Abstract Palaeostress inferred from brittle mesostructures in Seymour (Marambio) Island indicates a Cenozoic to Recent origin for an extensional stress field, with only local compressional stress states. Minimum horizontal stress (σ 3 ) orientations are scattered about two main NE–SW and NW–SE modes...

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Bibliographic Details
Published in:Antarctic Science
Main Authors: Maestro, A., López-Martínez, J., Bohoyo, F., Montes, M., Nozal, F., Santillana, S., Marenssi, S.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2008
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102007000892
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102007000892