招生信息

地质资源与地质工程

钮凤林

个人网页链接

非常规油气科学技术研究院

博士

教授

地质资源与地质工程

niu@cup.edu.cn

研究领域

[1] 非常规天然气地球物理探测

科研团队介绍及招生个性化需求

海外引进高层次科学家,非常规油气科学技术研究院地球物理探测学术带头人。


担任美国国家科学基金会、美国国务院国际开发地学基金会等机构评委,发表Nature文章6篇、Nature Geoscience文章3篇。


钮凤林教授自2012年10月引入我校以来,建立了地震波理论和应用研究中心,以第一作者或通讯作者发表SCI文章50余篇,其中JCR一区文章10余篇。

代表性研究成果

[1] 1.Y. Sun, F. Niu, H. Liu, Y. Chen, J. Liu, Crustal structure and deformation of the SE Tibetan plateau revealed by receiver function data: Seismic evidence for a lower crustal flow beneath the plateau,Earth Planet. Sci. Lett., in press, 2012. SCI

[2] 2.H. Liu, and F. Niu, Estimating crustal seismic anisotropy with a joint analysis of radial and transverse receiver function data,Geophys. J. Int., 188, 144-164, 2012. SCI

[3] 3.L. Li, Q.-F. Chen, F. Niu, and J. Su, Deep slip rates along the Longmen Shan fault zone estimated from repeating microearthquakes,J. Geophys. Res., 116, 2011. SCI

[4] 4.J. Masy, F. Niu, A. Levander, and M. Schmitz, Seismic evidence for a deep origin of the Merida Andes, Western Venezuela,Earth Planet. Sci. Lett., 305, 396-404, 2011. SCI

[5] 5.S. Pan, and F. Niu, Large contrast in crustal structure and composition between the Ordos plateau and the NE Tibetan plateau from by receiver function analysis,Earth Planet. Sci. Lett., 303, 291-298, 2011. SCI

[6] 6.X. Cheng, F. Niu, P. G. Silver, R. Nadeau, Seismic imaging of scatterer migration associated with the 2004 Parkfield earthquake using waveform data of repeating earthquakes and active sources,Bull. Seismol. Soc. Am., 101, 1291-1301, 2011. SCI

[7] 7.Li, and F. Niu, Seismic anisotropy and mantle flow beneath northeast China inferred from regional seismic networks,J. Geophys. Res., 115, B12327, 2010. SCI

[8] 8.X. Cheng, F. Niu, and B. Wang, Coseismic velocity change in the rupture zone of the 2008 Mw 7.9 Wenchuan earthquake observed from ambient seismic noise data,Bull. Seismol. Soc. Am., 100, 2539-2550, 2010.SCI

[9] 9.E. Vanacore, F. Niu, Y. Ma, Large angle reflection from a dipping structure recorded as a PKP precursor: Evidence for a low velocity zone at the core-mantle boundary beneath the Gulf of Mexico,Earth Planet. Sci. Lett., 293,54-62, 2010. SCI

[10] 10.B. Wang, and F. Niu, A broad 660-km discontinuity beneath northeastern China revealed by dense regional seismic networks in China,J. Geophys. Res., 115, B06308, 2010. SCI


[1] 1.Y. Sun, F. Niu, H. Liu, Y. Chen, J. Liu, Crustal structure and deformation of the SE Tibetan plateau revealed by receiver function data: Seismic evidence for a lower crustal flow beneath the plateau,Earth Planet. Sci. Lett., in press, 2012. SCI

[2] 2.H. Liu, and F. Niu, Estimating crustal seismic anisotropy with a joint analysis of radial and transverse receiver function data,Geophys. J. Int., 188, 144-164, 2012. SCI

[3] 3.L. Li, Q.-F. Chen, F. Niu, and J. Su, Deep slip rates along the Longmen Shan fault zone estimated from repeating microearthquakes,J. Geophys. Res., 116, 2011. SCI

[4] 4.J. Masy, F. Niu, A. Levander, and M. Schmitz, Seismic evidence for a deep origin of the Merida Andes, Western Venezuela,Earth Planet. Sci. Lett., 305, 396-404, 2011. SCI

[5] 5.S. Pan, and F. Niu, Large contrast in crustal structure and composition between the Ordos plateau and the NE Tibetan plateau from by receiver function analysis,Earth Planet. Sci. Lett., 303, 291-298, 2011. SCI

[6] 6.X. Cheng, F. Niu, P. G. Silver, R. Nadeau, Seismic imaging of scatterer migration associated with the 2004 Parkfield earthquake using waveform data of repeating earthquakes and active sources,Bull. Seismol. Soc. Am., 101, 1291-1301, 2011. SCI

[7] 7.Li, and F. Niu, Seismic anisotropy and mantle flow beneath northeast China inferred from regional seismic networks,J. Geophys. Res., 115, B12327, 2010. SCI

[8] 8.X. Cheng, F. Niu, and B. Wang, Coseismic velocity change in the rupture zone of the 2008 Mw 7.9 Wenchuan earthquake observed from ambient seismic noise data,Bull. Seismol. Soc. Am., 100, 2539-2550, 2010.SCI

[9] 9.E. Vanacore, F. Niu, Y. Ma, Large angle reflection from a dipping structure recorded as a PKP precursor: Evidence for a low velocity zone at the core-mantle boundary beneath the Gulf of Mexico,Earth Planet. Sci. Lett., 293,54-62, 2010. SCI

[10] 10.B. Wang, and F. Niu, A broad 660-km discontinuity beneath northeastern China revealed by dense regional seismic networks in China,J. Geophys. Res., 115, B06308, 2010. SCI