Localized crustal deformation along the central North Anatolian Fault Zone revealed by joint inversion ofP-receiver functions andP-wave polarizations-Reference-Cited by-同舟云学术

Localized crustal deformation along the central North Anatolian Fault Zone revealed by joint inversion ofP-receiver functions andP-wave polarizations

Author:

Schiffer Christian¹²^ORCID,Eken Tuna³,Rondenay Stéphane⁴,Taymaz Tuncay³^ORCID

Affiliation:

1. Department of Earth Sciences, Durham University, Science Site, DH1 3LE, Durham, UK

2. Department of Earth Sciences, Uppsala University, 752 36 Uppsala, Sweden

3. Department of Geophysical Engineering, The Faculty of Mines, Istanbul Technical University, Maslak 34469, Istanbul, Turkey

4. Department of Earth Science, University of Bergen, Allegaten 41, N-5007 Bergen, Norway

Funder

Durham University

Carlsberg Foundation

Istanbul Technical University

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

Reference85 articles.

1. ETOPO1 1 arc-minute global relief model: procedures, data sources and analysis;Amante,2009

2. The isolation of receiver effects from teleseismic P waveforms;Ammon;Bull. seism. Soc. Am.,1991

4. The north Anatolian fault zone;Barka;Ann. Tectonicae,1992

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