Crustal Thickness Variation Across the Sea of Marmara Region, NW Turkey: A Reflection of Modern and Ancient Tectonic Processes-Reference-Cited by-同舟云学术

Crustal Thickness Variation Across the Sea of Marmara Region, NW Turkey: A Reflection of Modern and Ancient Tectonic Processes

Published:2020-06-27 Issue:7 Volume:39 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Jenkins J.¹²^ORCID,Stephenson S. N.¹^ORCID,Martínez‐Garzón P.²^ORCID,Bohnhoff M.²³^ORCID,Nurlu M.⁴

Affiliation:

1. Department of Earth ScienceUniversity of Cambridge Cambridge UK

2. Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Section 4.2: Geomechanics and Scientific Drilling Potsdam Germany

3. Department of Earth SciencesFreie Universität Berlin Berlin Germany

4. AFAD, Disaster and Emergency Management Authority Turkey Ankara Turkey

Funder

Seventh Framework Programme

Helmholtz-Gemeinschaft

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019TC005986

Reference66 articles.

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2. Amante C. &Eakins B. W.(2001).ETOPO1 1 arc‐minute global relief model: Procedures data sources and analysis. National Geophysical Data Center NOAA.https://doi.org/10.7289/V5C8276M

3. Aristotle University of Thessaloniki Seismological Network(1981).Permanent Regional Seismological Network operated by the Aristotle University of Thessaloniki. International Federation of Digital Seismograph Networks. Other/Seismic Network.https://doi.org/10.7914/SN/HT

4. Submarine fault scarps in the Sea of Marmara pull-apart (North Anatolian Fault): Implications for seismic hazard in Istanbul

5. Barka A. A.(1992).The North Anatolian fault zone. InAnnales tectonicae 6 pp.164–195.

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