Influence of Incoming Plate Relief on Overriding Plate Deformation and Earthquake Nucleation: Cocos Ridge Subduction (Costa Rica)-Reference-Cited by-同舟云学术

Influence of Incoming Plate Relief on Overriding Plate Deformation and Earthquake Nucleation: Cocos Ridge Subduction (Costa Rica)

Published:2019-12 Issue:12 Volume:38 Page:4360-4377
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Martínez‐Loriente Sara¹²^ORCID,Sallarès Valentí¹^ORCID,R. Ranero César¹³,B. Ruh Jonas⁴^ORCID,Barckhausen Udo⁵,Grevemeyer Ingo⁶^ORCID,Bangs Nathan⁷^ORCID

Affiliation:

1. Center for Subsurface Imaging, ICM (CSIC) Institute of Marine Sciences, CSIC Barcelona Spain

2. Irish Centre for Research in Applied Geosciences (iCRAG), School of Earth SciencesUniversity College Dublin UK

3. ICREA Barcelona Spain

4. Structural Geology and Tectonics Group, Geological Institute, Department of Earth SciencesETH Zurich Zurich Switzerland

5. Bundesanstalt fur Geowissenschaften und Rohstoffe (BGR) Hannover Germany

6. GEOMAR‐Helmholtz Centre for Ocean Research Kiel Kiel Germany

7. Institute for GeophysicsUniversity of Texas at Austin Austin TX USA

Funder

FP7 People: Marie-Curie Actions

Sixth Framework Programme

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019TC005586

Reference81 articles.

1. Ridge collision, slab-window formation, and the flux of Pacific asthenosphere into the Caribbean realm

2. Arroyo I. G. Alvarado G. E. &Flueh E. R.(2003).Local seismicity at the Cocos Ridge—Osa Peninsula Subduction Zone Costa Rica Abstract S52F‐0174.

3. Interplate seismicity at the CRISP drilling site: The 2002 Mw 6.4 Osa Earthquake at the southeastern end of the Middle America Trench

4. The seismogenic zone in the Central Costa Rican Pacific margin: high-quality hypocentres from an amphibious network

5. Fluid accumulation along the Costa Rica subduction thrust and development of the seismogenic zone

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