高伟.2018.天桥沟—黄羊川断裂晚第四纪活动特征及其构造意义[D].北京:中国地震局地质研究所.
葛伟鹏,王敏,沈正康,等.2013.柴达木—祁连山地块内部震间上地壳块体运动特征与变形模式研究[J].地球物理学报,56(9):2994-3010.
郭鹏,韩竹军,姜文亮,等.2017.青藏高原东北缘冷龙岭断裂全新世左旋滑动速率[J].地震地质,39(2):323-341.
郭鹏.2019.北祁连山冷龙岭断裂大震复发行为与危险性研究[D].北京:中国地震局地质研究所.
郝明,李煜航,秦姗兰.2017.基于GPS数据的海原—六盘山断裂带滑动速率亏损时空分布[J].地震地质,39(3):471-484.
何文贵,刘百篪,吕太乙,等.1994.老虎山断裂带的分段性研究[J].西北地震学报,16(3):66-72.
何文贵,袁道阳,葛伟鹏,等.2010.祁连山活动断裂带中东段冷龙岭断裂滑动速率的精确厘定[J].地震,30(1):131-137.
李姜一,周本刚,李铁明,等.2020.安宁河—则木河断裂带和大凉山断裂带孕震深度研究及其地震危险性[J].地球物理学报,63(10):3669-3682.
李强,江在森,武艳强,等.2014.利用GPS资料反演海原—六盘山断裂带闭锁程度与滑动亏损分布[J].武汉大学学报(信息科学版),39(5):575-580.
李煜航,崔笃信,郝明.2015.利用GPS数据反演青藏高原东北缘主要活动断裂滑动速率[J].中国地质大学学报.地球科学,40(10):1767-1780.
李振洪,韩炳权,刘振江,等.2022.InSAR数据约束下的2016年和2022年青海门源地震震源参数及其滑动分布[J].武汉大学学报(信息科学版),47(6):887-897
刘雷,蒋锋云,朱良玉.2020.南北地震带北段现今运动特征及地震活动性分析[J].地震研究,43(4):658-665.
刘云华,张迎峰,张国宏,等.2019.2016年1月21日门源MS6.4级地震InSAR同震形变及发震构造研究[J].地球物理学进展,34(3):896-907.
叶茂盛,孟国杰,苏小宁.2018.青藏高原东北缘主要断裂闭锁特征和滑动亏损研究[J].地震,38(3):1-12.
袁道阳,刘百篪,吕太乙,等.1998.北祁连山东段活动断裂带的分段性研究[J].西北地震学报,20(4):27-34.
袁道阳,张培震,刘百篪,等.2004.青藏高原东北缘晚第四纪活动构造的几何图像与构造转换[J].地质学报,78(2):270-278.
张培震,邓起东,张国民,等.2003.中国大陆的强震活动与活动地块[J].中国科学:地球科学,33(增刊1):13-20.
张培震,邓起东,张竹琪,等.2013.中国大陆的活动断裂、地震灾害及其动力过程[J].中国科学:地球科学,43(10):1607-1620.
赵静,江在森,武艳强,等.2012.汶川地震前龙门山断裂带闭锁程度和滑动亏损分布研究[J].地球物理学报,55(9):2963-2972.
赵静,刘杰,任金卫,等.2019.汶川、芦山地震前龙门山断裂带地壳形变特征对比分析[J].地球学报,40(1):186-198.
赵静,牛安福,李强,等.2016.陇西块体周边断层闭锁程度与滑动亏损特征研[J].地震研究,39(3):351-358.
周琳,季灵运,李长军,等.2022.利用小震和GPS资料分析冷龙岭地区现今变形过程与地震活动[J].地震研究,45(3):416-423.
Altamimi Z,Rebischung P,Métivier L, et al.2016.ITRF2014:A new release of the International Terrestrial Reference Frame modeling non-linear station motions[J].Journal of Geophysical Research:Solid Earth,121(8):6109-6131.
Cavalié O,Lasserre C,Doin M P, et al.2008.Measurement of interseismic strain across the Haiyuan fault(Gansu,China),by InSAR[J].Earth Planet Sci Lett,275(3-4):246-257.
Daout S,Jolivet R,Lasserre C, et al.2016.Along-strike variations of the partitioning of convergence across the Haiyuan fault system detected by InSAR[J].Geophys J Int,205(1):536-547.
Dawers N H,Anders M H,Scholz C H.1993.Growth of normal faults:displacement length scaling[J].Geology,21(12):1107-1110.
Dewey J F,Burke K C A.1973.Tibetan Variscan and Precambrian reactivation:Products of continental collision[J].The J Geol,81(6):683-692.
Duvall A R,Clark M K.2010.Dissipation of fast strike-slip faulting within and beyond northeastern Tibet[J].Geology,38(3):223-226.
Fan L P,Li B R,Liang C, et al.2022.Precise relocation of the 2 aftershock sequences of the 2022 M6.9 Menyuan earthquake[J].Earthquake Sciecne,35(2):138-145.
Gan W J,Zhang P Z,Shen Z K, et al.2007.Present-day crustal motion within the Tibetan Plateau inferred from GPS measurements[J].Journal of Geophysical Research,112:B08416.
Gaudemer Y,Tapponnier P,Meyer B, et al.1995.Partitioning of crustal slip between linked,active faults in the eastern Qilian Shan,and evidence for a major seismic gap,the ‘Tianzhu gap',on the western Haiyuan fault,Lanzhou(China)[J].Geophys J Int,120(3):599-645.
Harkins N,Kirby E,Shi X, et al.2010.Millennial slip rates along the eastern Kunlun fault:implications for the dynamics of intracontinental deformation in Asia[J].Lithosphere,(2):247-266.
Jolivet R,Lasserre C,Doin M P, et al.2012.Shallow creep on the Haiyuan fault(Lanzhou,China)revealed by SAR interferometry[J].J Geophys Res,117(B6):137-147.
Jolivet R,Lasserre C,Doin M P, et al.2013.Spatio-temporal evolution of aseismic slip along the Haiyuan fault,China:implications for fault frictional properties[J].Earth Planet Sci Lett,377-378(2013):23-33.
Li C Y,Zhang P Z,Yin J H, et al.2009.Late Quaternary left-lateral slip rate of the Haiyuan Fault,northeastern margin of the Tibetan plateau[J].Tectonics,28(5):TC5010.
Li Y C,Shan X J,Qu C Y, et al.2016.Fault locking and slip rate deficit of the Haiyuan-Liupanshan fault zone in the northeastern margin of the Tibetan Plateau[J].Journal of Geodynamics,102:47-57.
Loveless J P,Meade B J.2010.Geodetic imaging of plate motions,slip rates,and partitioning of deformation in Japan[J].J Geophys Res,115(B2):B02410.
McCaffrey R,Qamar A I,King R W, et al.2007.Plate locking,block rotation and crustal deformation in the Pacific Northwest[J].Geophysical Journal International,169:1315-1340.
McCaffrey R.2002.Crustal block rotation sand plate coupling[C]//Plate Boundary Zones.Washington D C:AGU,101-122.
McCaffrey R.2005.Block kinematics of the pacific-north America plate boundary in the southwestern United States from inversion of GPS,seismological,and geologic data[J].J Geophys Res,110(B7):1-25.
McCaffrey R.2009.Time-dependent inversion of three-component continuous GPS for steady and transient sources in northern Cascadia[J].Geophys Res Lett,36:L07304.
Molnar P,Stock J M.2009.Slowing of India's convergence with Eurasia since 20Ma and its implications for Tibetan mantle dynamics[J].Tectonics,28(3):TC3001.1-TC3001.11.
Métivier F,Gaudemer Y,Tapponnier P, et al.1998.Northeastward growth of the Tibet plateau deduced from balanced reconstruction of the two areas:The Qaidam and Hexi corridor basins,China[J].Tectonics,17(6):823-842.
Peltzer G,Tapponnier P.1988.Formation and evolution of strike slip faults,rifts,and basins during the India-Asia collision:an experimental approach[J].Journal of Geophysical Research,93(B12):15085-15117.
Schmittbuhl J,Karabulut H,Lengline O, et al.2015.Seismicity distribution and locking depth along the Main Marmara Fault,Turkey[J].Geochemistry,Geophysics,Geosystems,17(3):954-965.
Tapponnier P,Molnar P.1976.Slip-line field theory and largescale continental tectonics[J].Nature,264(5584):319-324.
Tapponnier P,Xu Z Q,Roger F, et al.2001.Geology-stepwise rise and growth of the Tibet plateau.Science,294(5547):1671-1677.
Thatcher W.2007.Microplate model for the present-day deformation of Tibet[J].J Geophys Res,112(B1):B01401.
Wallace L M,Stevens C,Silver E, et al.2004.GPS and seismological constraints on active tectonics and arc-continent collision in Papua New Guinea:Implications for mechanics of microplate rotations in a plate boundary zone[J].J Geology Res,109(B5):B05404.
Wang H,Liu Z J,Ng H M, et al.2017.Sentinel -1 observations of the 2016 Menyuan earthquake:A buried reverse event linked to the left-lateral Haiyuan fault[J].International Journal of Applied Earth Observation and Geoinformation,61:14-21.
Wang K L,Wells R,Mazzotti S, et al.2003.A revised dislocation model of inter seismic deformation of the Cascadia subduction zone[J].J Geology Res,108(B1)2026.
Wang M,Shen Z K.2020.Present-day crustal deformation of continental China derived from GPS and its tectonic implications[J].Journal of Geophysical Research:Solid Earth,125(2):e2019JB018774.
Wang W,Wang D J,Zhao B, et al.2014.Horizontal crustal deformation in Chinese Mainland analyzed by CMONOC GPS data from 2009-2013[J].Geodesy and Geodynamics,5(3):41-45.
Yuan D Y,Zhang P Z,Ge W P, et al.2008.Late Quaternary strike-slip features along the western segment of Haiyuan-Qilianshan Fault,NE Tibetan plateau[C]//American Geophysical Union,Fall Meeting 2008.San Francisco,CA:AGU.
Zhang P Z,Gan W J,Shen Z K, et al.2005.A coupling model of rigid-block movement and continuous deformation:Patterns of the present-day deformation of China's continent and its vicinity[J].Acta GeologicaSinica,79(6):748-756.
Zhang P Z,Shen Z K,Wang M, et al.2004.Continuous deformation of the Tibetan Plateau from global positioning system data[J].Geology,32(9):809-812.
Zhang Z Q,McCaffrey R,Zhang P Z.2013.Relative motion across the eastern Tibetan plateau:Contributions from faulting,internal strain and rotation rates[J].Tectonophysics,584:240-256.
Zhao B,Huang Y,Zhang C H, et al.2015.Crustal deformation on the Chinese mainland during 1998-2014 based on GPS data[J].Geodesy and Geodynamics,6(1):7-15.
Zheng W J,Zhang P Z,He W G, et al.2013.Transformation of displacement between strike-slip and crustal shortening in the northern margin of the Tibetan Plateau:evidence from decadal GPS measurements and late Quaternary slip rates on faults[J].Tectonophysics,584(1):267-280.