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The surface deformation of the 2020 Doğanyol-Sivrice earthquake (Mw 6.8) and the earlier events suggest Mw˂7.0 earthquakes do not create significant surface slip along the East Anatolian Fault Zone

机译：2020的表面变形Doğyol-Sivrice地震（MW 6.8）和早期的事件表明MW˂7.0地震不会沿着东扎纳托利亚断层区造成显着的表面滑动

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Kenan Akbayram; Kemal Kıranşan; Çağlar Özer; Sadık Varolgüneş;
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1. Magnetic mineral characterization close to the Yingxiu-Beichuan fault surface rupture zone of the Wenchuan earthquake (Mw 7.9, 2008) and its implication for earthquake slip processes [J] . Liu Dongliang, Li Haibing, Lee Teh-Quei, Journal of Asian earth sciences . 2016,第JANa1期

机译：汶川地震映秀-北川断裂面破裂带附近的磁性矿物特征（Mw 7.9，2008）及其对地震滑动过程的影响
2. How well do surface slip measurements track slip at depth in large strike-slip earthquakes? The importance of fault structural maturity in controlling on-fault slip versus off-fault surface deformation [J] . James F. Dolan, Ben D. Haravitch Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System . 2014,第Null期

机译：在大型走滑地震中，表面滑移测量如何很好地跟踪深度滑移？断层结构成熟度在控制断层滑动与断层表面变形中的重要性
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机译：由1912年三角洲7.2-7.4级地震造成的树木破坏解释的Denali断层表面破裂：对2002 Denali断层地震滑动分布的影响
4. The 1999 Tehuacan (Mw = 7.0) and Oaxaca (Mw = 7.5) Mexican Earthquakes: Lessons Learned [C] . S. M. Alcocer, C. Reyes, D. Bitran, ACI international conference on innovations in design with emphasis on seismic, wind, and environmental loading; Quality control and innovations in materials/hot-weather concreting . 2002

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7. Rupture kinematics of 2020 January 24 Mw 6.7 Doğanyol-Sivrice, Turkey earthquake on the East Anatolian Fault Zone imaged by space geodesy [O] . Diego Melgar, Athanassios Ganas, Tuncay Taymaz, 2020

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机译：1994年1月17日，加利福尼亚州北岭地震期间卡诺加公园，温尼特卡和北岭地区发生共同断层的证据。

The surface deformation of the 2020 Doğanyol-Sivrice earthquake (Mw 6.8) and the earlier events suggest Mw˂7.0 earthquakes do not create significant surface slip along the East Anatolian Fault Zone

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