Increasing fault slip rates within the Corinth Rift, Greece: A rapidly localising active rift fault network-Reference-Cited by-同舟云学术

Increasing fault slip rates within the Corinth Rift, Greece: A rapidly localising active rift fault network

Published:2024-06 Issue: Volume:636 Page:118716
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Nixon Casey W.,McNeill Lisa C.^ORCID,Gawthorpe Robert L.^ORCID,Shillington Donna J.^ORCID,Michas Georgios^ORCID,Bell Rebecca E.,Moyle Aaron,Ford Mary^ORCID,Zakharova Natalia V.^ORCID,Bull Jonathan M.^ORCID,de Gelder Gino^ORCID

Funder

Norges Forskningsråd

Universität Bremen

MARUM – Zentrum für Marine Umweltwissenschaften

NERC

Publisher

Elsevier BV

Reference70 articles.

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2. Cenozoic and Cretaceous biochronology of planktonic foraminifera and calcareous nannofossils;Anthonissen,2012

3. Quaternary evolution of the Corinth Rift and its implications for the Late Cenozoic evolution of the Aegean;Armijo;Geophys. J. Int.,1996

4. Analysis of eleven years of deformation measured by GPS in the Corinth Rift Laboratory area;Avallone;Comptes Rendus Geosci.,2004

5. Active faulting at the western tip of the Gulf of Corinth, Greece, from high-resolution seismic data;Beckers;Mar. Geol.,2015

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1. Sediment flux variation as a record of climate change in the Late Quaternary deep‐water active Corinth Rift, Greece;Basin Research;2024-09

2. Transition From Late‐Miocene Syn‐Orogenic Extension to Plio‐Pleistocene Corinth Rifting in the Southern Hellenides, Northern Peloponnese, Greece;Tectonics;2024-06