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刘静 性别：女
职称:教授
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教育经历
· 1996.9 - 2003.7 美国加州理工学院(California Institute of Technology) -博士
· 1991.9 - 1994.7 国家地震局地质研究所 -硕士
· 1987.9 - 1991.7 南京大学地球科学系 -学士


工作经历
· 2011.11 - 2019.6 中国地震局地质研究所 →研究员
· 2006.8 - 2011.11 中国科学院青藏高原研究所 →研究员
· 2005.8 - 2006.8 中国科学院青藏高原研究所 →副研究员
· 2003.7 - 2005.7 法国Institut de Physique du Globe de Paris →博士后


研究方向
· 活动构造
· 地震地质和古地震
· 构造地貌学
· 基于野外观测，综合数值模拟和年代学测试，研究青藏高原抬升及地貌响应和岩石圈与地表过程的耦合及其灾害效应，量化活动断裂的第四纪活动性及地震危险性。






个人简介 刘 静，1991 年毕业于南京大学地球科学系，1994 年获中国地震局地质所硕士学位, 2003 年获美国加州理工学院地质学博士，2003-2005 年法国地球物理研究院开展博士后工作。自1991 年以来一直从事活动构造、地表侵蚀与构造地貌研究。2002年以来发表论文80余篇，其中SCI检索40余篇，SCI论文总引用2600余次。2017年以来任中国地震学会构造地貌专业委员会主任，中国第四纪研究学会构造与气候专业委员会副主任，中国地质学会构造地质专业委员会委员，中国青藏高原研究会理事及中国地震局科技委委员。目前兼任《科学通报》《Tectonophysics》《中国科学》《地震地质》和《中国地震》等刊物编委。

学术成果
论文成果
[1]A structural interpretation of the aftershock "cloud" of the 1992 Mw 7.3 Landers, California earthquake

[2]Six Similar and Sequential Ruptures of the San Andreas Fault, Carrizo Plain, California

[3]The effect of slip variability on earthquake slip-length scaling

[4]Serial rupture of the San Andreas fault, Carrizo Plain, California, revealed by three-dimensional excavations

[5]Millennial Recurrence of Large Earthquakes on the Haiyuan Fault near Songshan, Gansu Province, China

[6]Quantifying landscape differences across the Tibet plateau: Implications for topographic relief evolution

[7]Co-seismic ruptures of the 12 May, 2008, Ms 8.0 Wenchuan earthquake, Sichuan: EW crustal shortening on oblique, parallel thrusts along the eastern edge of Tibet

[8]Surficial Slip and rupture geometry on the Beichuan fault near Hongkou during the Mw 7.9 Wenchuan earthquake, China

[9]Focused modern denudation of the Longmen Shan margin, eastern Tibetan plateau

[10]Surface ruptures on the transverse Xiaoyudong fault: A significant segment boundary breached during the 2008 Wenchuan earthquake, China

[11]Illuminating the active Haiyuan fault, China by airborne Light Detection and Ranging (LiDAR)

[12]The role of transverse structure in reverse-type earthquake rupture propagation: A case study on the Xiaoyudong fault in the Wenchuan earthquake

[13]Co-seismic displacement field associated with the 25 April, 2015 Mw 7.8 Nepal earthquake recorded by Global Positioning System

[14]Tectonic setting and general features of coseismic rupture of the 25 April, 2015 Mw 7.8 Nepal earthquake and model of seismic cycle in Nepal Himalaya

[15]Variability in magnitude of paleoearthquakes revealed by trenching and historical records, along the Haiyuan fault, China

[16]Liquefaction in western Sichuan Basin during the 2008 Mw 7.9 Wenchuan earthquake, China

[17]Paleoelevation reconstruction of the Paleocene-Eocene Gonjo basin, SE-central Tibet

[18]A 6000-Year-Long Paleoseismologic Record of Earthquakes on the Xorkoli Segment of the Central Altyn Tagh Fault, Xinjiang, China

[19]Transient deformation during the Milashan Tunnel construction in northern Sangri-Cuona Rift, southern Tibet, China observed by Sentinel-1 satellites

[20]Paleoseismic investigation of the Aksay restraining double-bend, Altyn Tagh fault, and its implication for barrier-breaching ruptures

[21]Geomorphic offsets along the creeping Laohu Shan section of the Haiyuan fault, northern Tibetan Plateau

[22]Multiple episodes of fast exhumation since Cretaceous in the Three Rivers region, SE Tibet, revealed by low-temperature thermochronology

[23]Reevaluation of the Late Pleistocene slip rate of the Haiyuan fault near Songshan, Gansu province, China

[24]Paleoseismologic record of earthquakes along the Wuzunxiaoer section of the Altyn Tagh fault and its implication for cascade rupture behavior

[25]Spatial and temporal variations in rock exhumation linked to large-scale shear zones in the southeastern Tibetan Plateau

[26]Postseismic deformation following the 2015 Mw7.8 Gorkha (Nepal) earthquake: new GPS data, kinematic and dynamic models, and the roles of afterslip and viscoelastic relaxation














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