New kinematic and geochronologic evidence for the Quaternary evolution of the Central Anatolian fault zone (CAFZ)-Reference-Cited by-同舟云学术

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New kinematic and geochronologic evidence for the Quaternary evolution of the Central Anatolian fault zone (CAFZ)

Published:2015-10 Issue:10 Volume:34 Page:2118-2141
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Higgins Mark¹^ORCID,Schoenbohm Lindsay M.¹,Brocard Gilles²,Kaymakci Nuretdin³,Gosse John C.⁴,Cosca Michael A.⁵

Affiliation:

1. Department of Earth Sciences University of Toronto Toronto Ontario Canada

2. Department of Earth and Environmental Science University of Pennsylvania Philadelphia Pennsylvania USA

3. Department of Geological Engineering Middle East Technical University Ankara Turkey

4. Department of Earth Sciences Dalhousie University Halifax Nova Scotia Canada

5. Central Mineral and Environmental Resources Science Center U.S. Geological Survey Denver Colorado USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015TC003864

Reference78 articles.

1. The Pliocene–Quaternary tectonic evolution of the Cilicia and Adana basins, eastern Mediterranean: Special reference to the development of the Kozan Fault zone

2. Deformation of Central Anatolia: GPS implications

3. Paleoseismological investigations on a slow-moving active fault in central Anatolia, Tecer Fault, Sivas

4. Roles of strike-slip faults during continental deformation: examples from the active Arabia–Eurasia collision

5. Tectonic evolution of the Niksar and Tasova–Erbaa pull-apart basins, North Anatolian Fault Zone: their significance for the motion of the Anatolian block

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