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Featured researches published by Jiafu Hu.


Science China-earth Sciences | 2012

S-wave Q structure of the crust and upper mantle beneath Yunnan from surface waves

Jia Chen; Jiafu Hu; Haiyan Yang; Xiao‐Man Zhang; Limin Wen; Hengchu Peng

A phase-matched filtering technique is applied to extract fundamental mode signals from Rayleigh waves recorded at 62 digital seismic stations in the Yunnan and Sichuan regions. We use the fundamental mode of vibrations at two stations that are located on the same great circle as the focus to calculate an inter-station attenuation coefficient of the Rayleigh wave with periods between 0. 0 and 80.64 s, and invert for the inter-station S-wave Q-factor (Qβ) at depths of 0–200 km. The results indicate that Qβ in Yunnan is 20–140, presenting a low Qβ background with apparent lateral variation. Taking the Honghe Fault as the boundary, Qβ of the crust is only 20 on the west side, extending to a depth of 120 km. The distribution of Qβ is consistent with large-scale Cenozoic volcanic and intrusive rocks in western Yunnan, implying that the crust and mantle are in the thermally active state. In the eastern Yunnan Block, east of the Xiaojiang Fault, Qβ in the upper 120 km is 140 in the south but only 20 in the north. Additionally, around the Dukou-Chuxiong in the mid-Yunnan Block, Qβ in the lithosphere is relatively high at 60–100, corresponding to a stiff crust. This is because the suture between the Indian and Eurasian plates reversed the tension in the rifting stage into the compression of orogenesis, leading to the closure of a gap in the crust. After some time, interstitial fluids gradually disappeared, resulting in a high velocity layer in the crust and low heat flow on the surface. The Yunnan region consists of an obvious block of elevated Qβ, distributed within the low background, consistent with the distribution of heat-flow values on the surface. The Honghe and Xiaojiang faults are tectonic boundaries in addition to being boundaries between regions of high and low crustal Qβ. The low Qβ is probably the result of crustal rupture and disturbance caused by strong earthquakes and the upwelling of hot substances along the deep fault zones.


Pure and Applied Geophysics | 2010

Love and Rayleigh Wave Tomography of the Qinghai-Tibet Plateau and Surrounding Areas

Yun Chen; José Badal; Jiafu Hu


Earth and Planetary Science Letters | 2011

S receiver function analysis of the crustal and lithospheric structures beneath eastern Tibet

Jiafu Hu; Xingqian Xu; Haiyan Yang; Limin Wen; Guangquan Li


Gondwana Research | 2012

Lithospheric structure and crust–mantle decoupling in the southeast edge of the Tibetan Plateau

Jiafu Hu; Haiyan Yang; Xingqian Xu; Limin Wen; Guangquan Li


Journal of Asian Earth Sciences | 2013

Crustal structure in the Tengchong volcanic area and position of the magma chambers

Haiyan Yang; Jiafu Hu; Yili Hu; Yuanze Duan; Guangquan Li


Journal of Asian Earth Sciences | 2013

Seismic signature of the mantle transition zone beneath eastern Tibet and Sichuan Basin

Jiafu Hu; Haiyan Yang; Guangquan Li; Limin Wen


Geophysical Journal International | 2011

Analysis of the crustal thickness and Poisson's ratio in eastern Tibet from teleseismic receiver functions

Haiyan Yang; Jiafu Hu; Guangquan Li; Hong Zhao; Limin Wen


Pure and Applied Geophysics | 2008

Structure and Significance of S-wave Velocity and Poisson’s Ratio in the Crust beneath the Eastern Side of the Qinghai-Tibet Plateau

Jiafu Hu; Haiyan Yang; Hong Zhao


Gondwana Research | 2015

Seismic upper mantle discontinuities beneath Southeast Tibet and geodynamic implications

Jiafu Hu; Haiyan Yang; Guangquan Li; Hengchu Peng


Journal of Asian Earth Sciences | 2017

The lithospheric structure beneath southeast Tibet revealed by P and S receiver functions

Haiyan Yang; Hengchu Peng; Jiafu Hu

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José Badal

University of Zaragoza

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