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DOI10.1029/2019GL086604
Elastic Fault Interactions and Earthquake Rupture Along the Southern Hellenic Subduction Plate Interface Zone in Greece
Saltogianni V.; Mouslopoulou V.; Oncken O.; Nicol A.; Gianniou M.; Mertikas S.
发表日期2020
ISSN 0094-8276
卷号47期号:13
英文摘要The importance of splay-thrust faults in subduction seismogenesis is increasingly acknowledged; however, their elastic interaction with the plate interface remains unclear. Here, we use GPS velocities, constrained by millennial fault slip rates, to study elastic fault-interactions between the plate interface and its upper-plate splay-thrust faults from the southern Hellenic Subduction System (HSS). We find that, despite its largely aseismic character, the HSS plate interface zone is kinematically segmented, with slip rate deficits locally reaching ~85% and ~45% of the plate convergence rate on the western and eastern segments, respectively, and on structures different from those that ruptured historically. Although western Crete has been more active seismically during late Holocene, we find that the eastern HSS has higher seismic potential for large-magnitude (M > 6) earthquakes and its interface zone is closer to failure. Elastic fault interactions are responsible for both significant intersegment variability in strain accumulation and uniformity in earthquake rupture segmentation along the HSS over millennial timescales. ©2020. American Geophysical Union. All Rights Reserved.
英文关键词Earthquakes; Plates (structural components); Earthquake rupture; Elastic interactions; Fault interactions; Fault-slip rates; GPS velocities; Plate convergence; Plate interfaces; Strain accumulations; Fault slips; earthquake magnitude; earthquake rupture; failure mechanism; fault slip; GPS; plate convergence; segmentation; subduction; thrust fault; Aegean Islands; Crete [Greece]; Greece
语种英语
来源期刊Geophysical Research Letters
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/170183
作者单位Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany; Institute of Geodynamics, National Observatory of Athens, Athens, Greece; School of Earth and Environment, University of Canterbury, Christchurch, New Zealand; Hellenic Cadastre, Athens, Greece; School of Engineering, University of West Attica, Athens, Greece; School of Mineral Resources Engineering, Geodesy and Geomatics Engineering Lab, Technical University of Crete, Chania, Greece
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Saltogianni V.,Mouslopoulou V.,Oncken O.,et al. Elastic Fault Interactions and Earthquake Rupture Along the Southern Hellenic Subduction Plate Interface Zone in Greece[J],2020,47(13).
APA Saltogianni V.,Mouslopoulou V.,Oncken O.,Nicol A.,Gianniou M.,&Mertikas S..(2020).Elastic Fault Interactions and Earthquake Rupture Along the Southern Hellenic Subduction Plate Interface Zone in Greece.Geophysical Research Letters,47(13).
MLA Saltogianni V.,et al."Elastic Fault Interactions and Earthquake Rupture Along the Southern Hellenic Subduction Plate Interface Zone in Greece".Geophysical Research Letters 47.13(2020).
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