James Ni
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View article: Crust and Mantle Flow From Central Tibetan Plateau to the Indo‐Burma Subduction Zone
Crust and Mantle Flow From Central Tibetan Plateau to the Indo‐Burma Subduction Zone Open
The extremely oblique Indo‐Burma subduction zone exhibits dextral strike‐slip faulting along the Sagaing, Kabaw, and Churachandpur‐Mao Faults as well as east‐west shortening between the Sagaing Fault and Bengal Basin. Through regional stre…
View article: Depth-dependent<i>Pn</i>velocities and configuration of Indian and Asian lithosphere beneath the Tibetan Plateau
Depth-dependent<i>Pn</i>velocities and configuration of Indian and Asian lithosphere beneath the Tibetan Plateau Open
Using Pn-wave traveltimes from three regional distance ranges we generated Pn tomography models to investigate the 3-D nature of the uppermost mantle lid P-wave velocity structure beneath the Tibetan Plateau and surrounding regions. Signif…
View article: Lg attenuation, frequency dependence and relative site response of the western United States as revealed by the EarthScope Transportable Array
Lg attenuation, frequency dependence and relative site response of the western United States as revealed by the EarthScope Transportable Array Open
Lg attenuation of the western United States is estimated using regional waveforms recorded by EarthScope's Transportable Array, the Berkeley Digital Seismograph Network and the Caltech Regional Seismic Network. Lg attenuation is determined…
View article: The crustal structure of south central Mongolia using receiver functions
The crustal structure of south central Mongolia using receiver functions Open
The crustal thickness H and average crustal velocity ratio k (Vp/Vs) beneath south central Mongolia are investigated using the H-k stacking method based on teleseismic radial receiver functions. Our primary results reveal that the local cr…