How Much Nubia‐Eurasia Convergence Is Accommodated by the NE End of the Eastern Betic Shear Zone (SE Spain)? Constraints From GPS Velocities-Reference-Cited by-同舟云学术

How Much Nubia‐Eurasia Convergence Is Accommodated by the NE End of the Eastern Betic Shear Zone (SE Spain)? Constraints From GPS Velocities

Published:2019-05 Issue:5 Volume:38 Page:1824-1839
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Borque M. J.¹²,Sánchez‐Alzola A.³^ORCID,Martin‐Rojas I.⁴^ORCID,Alfaro P.⁴^ORCID,Molina S.⁴^ORCID,Rosa‐Cintas S.⁵,Rodríguez‐Caderot G.⁶,Lacy C.¹²,García‐Armenteros J. A.²^ORCID,Avilés M.¹,Herrera‐Olmo A.¹,García‐Tortosa F. J.²⁷,Estévez A.⁴,Gil A. J.¹²^ORCID

Affiliation:

1. Departamento de Ingeniería Cartográfica, Geodésica y FotogrametríaUniversidad de Jaén Jaén Spain

2. Centro de Estudios Avanzados en Ciencias de la Tierra CEACTierraUniversidad de Jaén Jaén Spain

3. Departamento de Estadística e Investigación OperativaUniversidad de Cádiz Puerto Real (Cádiz) Spain

4. Departamento de Ciencias de la Tierra y del Medio AmbienteUniversidad de Alicante Alicante Spain

5. Departamento de Didáctica General y Didácticas Específicas. Facultad de EducaciónUniversidad de Alicante Alicante Spain

6. Departamento de Astronomía y Geodesia, Facultad de MatemáticasUniversidad Complutense de Madrid Madrid Spain

7. Departamento de GeologíaUniversidad de Jaén Jaén Spain

Funder

Universidad de Jaén

Universidad de Alicante

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC004970

Reference84 articles.

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3. Onshore and offshore compressional tectonics in the eastern Betic Cordillera (SE Spain)

4. Structures sédimentaires de déformation interprétées comme séismites dans le Quaternaire du bassin du Bas Segura (Cordillère Bétique orientale);Alfaro P.;Comptes Rendues Academie Sciences. Paris (II),1999

5. ITRF2008 plate motion model

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