scholarly journals Geological Records of Coseismic Shear Localization along the Yangsan Fault, Korea

Author(s):  
Dohee Gu ◽  
Raehee Han ◽  
Sangwoo Woo
2020 ◽  
Vol 4 (2) ◽  
Author(s):  
Sheng Yin ◽  
Guangming Cheng ◽  
Yong Zhu ◽  
Huajian Gao
Keyword(s):  

2016 ◽  
Vol 57 (7) ◽  
pp. 1217-1225
Author(s):  
D. A. Bilalov ◽  
M. A. Sokovikov ◽  
V. V. Chudinov ◽  
V. A. Oborin ◽  
Yu. V. Bayandin ◽  
...  

2014 ◽  
Vol 10 (3) ◽  
pp. 389-397 ◽  
Author(s):  
Wenxiong Huang ◽  
Liya Huang ◽  
Daichao Sheng ◽  
Scott W. Sloan

2002 ◽  
Vol 124 (3) ◽  
pp. 329-334 ◽  
Author(s):  
B. D. Wirth ◽  
V. V. Bulatov ◽  
T. Diaz de la Rubia

In copper and other face centered cubic metals, high-energy particle irradiation produces hardening and shear localization. Post-irradiation microstructural examination in Cu reveals that irradiation has produced a high number density of nanometer sized stacking fault tetrahedra. The resultant irradiation hardening and shear localization is commonly attributed to the interaction between stacking fault tetrahedra and mobile dislocations, although the mechanism of this interaction is unknown. In this work, we present results from a molecular dynamics simulation study to characterize the motion and velocity of edge dislocations at high strain rate and the interaction and fate of the moving edge dislocation with stacking fault tetrahedra in Cu using an EAM interatomic potential. The results show that a perfect SFT acts as a hard obstacle for dislocation motion and, although the SFT is sheared by the dislocation passage, it remains largely intact. However, our simulations show that an overlapping, truncated SFT is absorbed by the passage of an edge dislocation, resulting in dislocation climb and the formation of a pair of less mobile super-jogs on the dislocation.


2005 ◽  
Vol 64 (2) ◽  
pp. 221-233 ◽  
Author(s):  
Gi Young Jeong ◽  
Chang-Sik Cheong

AbstractRecurrence characteristics of a Quaternary fault are generally investigated on the basis of field properties that are rapidly degraded by chemical weathering and erosion in warm humid climates. Here we show that in intense weathering environments, mineralogical and micromorphological investigations are valuable in paleoseismological reconstruction. A weathering profile developed in Late Quaternary marine terrace deposits along the southeastern coast of the Korean Peninsula was disturbed by tectonic movement that appears to be a simple one-time reverse faulting event based on field observations. A comparative analysis of the mineralogy, micromorphology, and chemistry of the weathering profile and fault gouge, however, reveals that both the microfissures in the deformed weathering profile and larger void spaces along the fault plane were filled with multi-stage accumulations of illuvial clay and silt minerals of detrital origin, suggesting a repetition of fissuring and subsequent sealing in the weathering profile as it underwent continuous mineralogical transformation and particle translocation. We reconstruct a sequence of multiple faulting events unrecognized in previous field surveys, which requires revision of the view that the Korean Peninsula was tectonically stable, during the Late Quaternary.


1988 ◽  
Vol 19 (8) ◽  
pp. 2041-2048 ◽  
Author(s):  
Young Woo Kim ◽  
D. L. Bourell
Keyword(s):  

2004 ◽  
Vol 35 (9) ◽  
pp. 2575-2586 ◽  
Author(s):  
M. A. Meyers ◽  
V. F. Nesterenko ◽  
D. J. Benson ◽  
B. Y. Cao ◽  
Y. B. Xu

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