Seismic evidence for crustal modification across the Tanlu fault zone in eastern China
- Ziqiang Lü
Publication date
July 2022
DOIAbstract
The shear wave velocity model and the phase delays between the observed and synthetic waveform
The shear wave velocity model and the phase delays between the observed and synthetic waveform
High-resolution imaging of fault zone structures is essential for understanding earthquake physics a...
Although the study of spatiotemporal variation of a subsurface velocity structure is a challenging t...
The Longmen-Shan fault zone, at the eastern margin of the Tibetan Plateau, is one of the most extens...
Receiver function waveforms and crustal model across the central Tanlu fault zone in eastern Chin
The north-south trending Tancheng-Lujiang (Tanlu) fault belt extends from northeast China to the Dab...
We conduct a nonlinear joint inversion of receiver functions and surface waves to obtain the lithosp...
[ACCESS RESTRICTED TO THE UNIVERSITY OF MISSOURI AT REQUEST OF AUTHOR.] We have used attenuation tom...
Since the Mesozoic, southeastern North China Craton has experienced intense crustal thinning and lit...
[1] The India-Eurasia collision and the decratonization of the North China Craton have drawn much at...
Pn travel-time tomography provides a way of improving structural information on the uppermost mantle...
This paper describes the development of seismological models for three sub-regions within Eastern Ch...
We installed a temporary earthquake station at Shidao on the Xisha Islands in the South China Sea to...
A high-resolution 2D (horizontal) seismic velocity model is presented for the upper crust around the...
The East Kunlun Fault zone, striking E–W to WNW–ESE, has been recognized as one of the largest and m...
Abstract:Trapped waves in the Qingchuan fault zone were observed at Muyu near the northeastern end o...
High-resolution imaging of fault zone structures is essential for understanding earthquake physics a...
Although the study of spatiotemporal variation of a subsurface velocity structure is a challenging t...
The Longmen-Shan fault zone, at the eastern margin of the Tibetan Plateau, is one of the most extens...
Receiver function waveforms and crustal model across the central Tanlu fault zone in eastern Chin
The north-south trending Tancheng-Lujiang (Tanlu) fault belt extends from northeast China to the Dab...
We conduct a nonlinear joint inversion of receiver functions and surface waves to obtain the lithosp...
[ACCESS RESTRICTED TO THE UNIVERSITY OF MISSOURI AT REQUEST OF AUTHOR.] We have used attenuation tom...
Since the Mesozoic, southeastern North China Craton has experienced intense crustal thinning and lit...
[1] The India-Eurasia collision and the decratonization of the North China Craton have drawn much at...
Pn travel-time tomography provides a way of improving structural information on the uppermost mantle...
This paper describes the development of seismological models for three sub-regions within Eastern Ch...
We installed a temporary earthquake station at Shidao on the Xisha Islands in the South China Sea to...
A high-resolution 2D (horizontal) seismic velocity model is presented for the upper crust around the...
The East Kunlun Fault zone, striking E–W to WNW–ESE, has been recognized as one of the largest and m...
Abstract:Trapped waves in the Qingchuan fault zone were observed at Muyu near the northeastern end o...
High-resolution imaging of fault zone structures is essential for understanding earthquake physics a...
Although the study of spatiotemporal variation of a subsurface velocity structure is a challenging t...
The Longmen-Shan fault zone, at the eastern margin of the Tibetan Plateau, is one of the most extens...
Add to ORKG