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AGU 2013 Session S11D/S12B: "Progress in the Research of the Wenchuan and Lushan earthquakes"
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In the 2013 AGU Annual meeting, totally 38 abstracts are submitted to the session  “Progress in the Research of the 2008 Ms8.0 Wenchuan and 2013 Ms7.0 Lushan earthquakes” 。22 and 16 abstracts will present in the form of oral and poster, respectively.  To help readers get touch on the topics beforehand, we list 1-2 recommended papers for every abstract. Click on the name of the first author will lead to the full list of the author's papers.


S11D. Progress in the Research of the 2008 Ms8.0 Wenchuan and 2013 Ms7.0 Lushan earthquakes I

Convener(s): Chuntao Liang (Chengdu University of Technology ) and Sidao Ni (Institute of Geodesy and Geophysics, Chinese Academy of Science)

8:00 AM - 10:00 AM; 307 (Moscone South)



Title
First Author
Recommended Papers
Seismogenic enviroment
Segmentation and millennium recurrence interval of morphogenic earthquakes of the Longmen Shan Thrust Belt, central China(INVITED)
Aiming Lin
Co-seismic ground-shortening structures produced by the 2008 Mw 7.9 Wenchuan earthquake, China

Duplex crustal segmented shortening model of the Longmenshan thrust belt: Lessons from the Wenchuan and Lushan earthquakes, eastern Tibetan Plateau
Xiwei Xu
Coseismic reverse- and oblique-slip surface faulting generated by the 2008 Mw 7.9 Wenchuan earthquake, China

Historic Seismicity near the Source Zone of the Great 2008 Wenchuan Earthquake: Implications for Seismic Hazards
Wang-ping Chen
Historic seismicity near the source zone of the great 2008 Wenchuan earthquake: Implications for seismic hazards
Source
Investigation on source dynamics of the 2008 Mw7.9 Wenchuan earthquake, China
Xiaofei Chen
Preface to the special issue on the 2008 great Wenchuan earthquake
Fault Property
Characteristics of the Wenchuan earthquake fault from the results of Scientific Drilling (WFSD) (Invited)
Haibing Li
Characteristics of the fault-related rocks, fault zones and the principal slip zone in the Wenchuan Earthquake Fault Scientific Drilling Project Hole-1 (WFSD-1)

Temperature anomaly on the Wenchuan earthquake fault zone associated with 2008 MW 7.9 Wenchuan earthquake
Lian Xue

Hazard
Cosesimic landslides and their post-quake effects (Invited)
Runqiu Huang
The landslide story
Comprehensive
Scientific Research Database of the 2008 Ms8.0 Wenchuan Earthquake
Chuntao Liang
A low velocity belt beneath northern and eastern Tibetan Plateau from Pn tomography


S12B. Progress in the Research of the 2008 Ms8.0 Wenchuan and 2013 Ms7.0 Lushan earthquakes II
Convener(s): Xiwei Xu (Institute of Geology, CEA) and Mian Liu (Univ Missouri Columbia)
10:20 AM - 12:20 PM; 307 (Moscone South)



Title
First Author
Recommended Papers
Coseismic Deformation
Coseismic and postseismic deformation studies of the Wenchuan earthquake and seismo-tectonics of the Longmen Shan fault system (Invited)
Zhengkang Shen
Slip maxima at fault junctions and rupturing of barriers during the 2008 Wenchuan earthquake
Stress
Stress-based aftershock forecasting: the 2008 M=7.9 Wenchuan, and 2013 M=6.6 Lushan earthquakes
Tom Parsons
Stress changes from the 2008 Wenchuan earthquake and increased hazard in the Sichuan basin
Reservior
Pore pressure dynamics beneath the Zipingpu Reservoir and its potential role in triggering the 2008 Wenchuan earthquake
Shemin Ge
Did the Zipingpu Reservoir trigger the 2008 Wenchuan earthquake?

The 2008 M7.9 Wenchuan earthquake - a human-caused eventC
Ckristian D. Klose
Evidence for anthropogenic surface loading as trigger mechanism of the 2008 Wenchuan earthquake
Hazard Assement
The 2013 Lushan earthquake in China tests hazard assessments
Mian Liu
Stress evolution and fault interactions before and after the 2008 Great Wenchuan earthquake

Seismic Hazard Assessment in China: From the 2008 Wenchuan Earthquake to the 2013 Minxian Earthquake
Zhenming Wang
A Short Note on Ground-motion Recordings from the M 7.9 Wenchuan, China, Earthquake and Ground-motion Prediction Equations in the Central and Eastern United States
Structural Change
Subsurface Structure Change in Longmenshan Forland Basin induced by Wenchuan Earthquake
Junxing Cao


What temporal changes of seismic wave speed and waveform tell us about the deformation of the upper and lower crust in response to the hydrological charge and the Wenchuan 2008 earthquake
Anne Obermann