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WCEQ in AGU 2012 Annual Meeting -1.
clicks:350Totally 22 papers had been disscussed in the AGU 2012 Fall Meeting! 1 session was dedicated to the Wenchuan Fault Zone Scientific Drilling!
T13D-2637. 300-km-long co-seismic surface rupture produced by the 2008 Mw 7.9 Wenchuan earthquake along the active Longmen Shan Thrust Belt, China
T33E-2697. Focal Mechanisms and Stress Environment of the 12 May 2008 Wenchuan, China, Earthquake Sequence
T33K-08. Probing the Deep Rheology of Tibet: Constraints from the 2008 Mw 7.9 Wenchuan, China Earthquake
Session: T41D. T41D. Wenchuan Fault Zone Scientific Drilling: Results and Context I Posters
T41D-2611. Rupture process of the Wenchuan earthquake (Ms8.0) indicated by the characteristics of the surface rupture zones and the fault striations
T41D-2613. On 4-year Aftershock Sequence of the Wenchuan Earthquake (M8.0,2008)
T41D-2614. The relation between seismic response characteristics of Longmenshan fault zone and Wenchuan earthquake
T41D-2619. Low coseismic strength of the Longmenshan fault gouge from the WFSD project (Wenchuan Mw 8.0 2008 earthquake)
T41D-2620. Frictional Properties of Natural Gouges from Longmenshan Fault Zone Ruptured during the Wenchuan Mw 7.9 Earthquake
T41D-2621. The energy distribution of the Ms8.0 Wenchuan earthquake
T41D-2622. Fault weakening by water in the brittle-plastic transition zone of the Wenchuan fault zone (Longmenshan, China):a study through deformed exhumed granites
T41D-2623. Continuous Record of Permeability inside the Wenchuan Earthquake Fault Zone
T41D-2624. Internal structures of Wenchuan earthquake fault zone, revealed by WFSD-1 cores and surface outcrops
T41D-2629. Structural Characteristics of the Northern Segment of the Wenchuan Earthquake Fault Zone Reflected on Shallow Seismic Reflection Profiles
T41D-2630. Low magnetic susceptibility of gouge due to low thermal decomposition from the Jiulong Outcrop of the Wenchuan Earthquake Rupture Zone
---8 more in the next announcement--- |
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