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Timing and spatial variation of deformation along the Kanggur-Huangshan shear zone in the Chinese Tianshan: Implications for regional differential uplift and mineralization
The Whole-Space Modeling of the Hazardous Geological Body ahead of the Tunnel Face by the Transient Electromagnetic Method
Raman spectroscopy-based screening of zircon for reliable water content and oxygen isotope measurements
Case Study regarding the Stress Distribution and Microseismic Laws of Coal and Rock Underlying the Residual Coal Pillar
A quantitative calculation method for fracture density using the neutron self-shielding modification and neutron-induced gamma logging
SH-SH wave inversion for S-wave velocity and density
An enhanced accuracy method to determine oil saturation by carbon/oxygen logging in tight reservoirs
Nonlinear Noise Reduction for the Airborne Transient Electromagnetic Method based on Kernel Minimum Noise Fraction
Pure sediment-derived granites in a subduction zone
Simultaneous inversion for S-wave velocity and density from the SV-SV wave
Resistivity-depth Imaging with the Airborne Transient Electromagnetic Method Based on an Artificial Neural Network
To: “Quantitative seismic interpretation of rock brittleness based on statistical rock physics,” Lin Wang, Feng Zhang, Xiang-Yang Li, Bang-Rang Di, and Lian-Bo Zeng , Geophysics, 84 , no. 4, IM63–IM75, doi: 10.1190/GEO2018-0094.1.
Characterization of a shale-gas reservoir based on a seismic amplitude variation with offset inversion for transverse isotropy with vertical axis of symmetry media and quantitative seismic interpretation
Formation of excess fluid pressure, sediment fluidization and mass-transport deposits in the Plio-Pleistocene Boso forearc basin, central Japan
Abstract Analyses of consolidation state, fabrics and physical properties were conducted on rock samples from the Plio-Pleistocene Boso forearc basin, central Japan. Consolidation tests identified that the trend in consolidation yield stress was systematically 8 MPa smaller than expected for the overburden from the sediment thickness of the Kazusa Group. An excess fluid pressure interval was also identified in the lower part of the basin fill, where several large-scale (several kilometres in length and several tens of metres thick) mass-transport deposits (MTDs) are intercalated. This interval is characterized by high porosity and small consolidation yield stresses, indicating that consolidation had been retarded by the excess fluid pressure. The estimated excess fluid pressure was c. 5–7 MPa. In addition, outcrop-scale fluidization and minor liquefaction features were identified within and below the high fluid pressure interval. The excess fluid pressure reduced the effective stress in the Boso forearc basin and, subsequently, the stability of the slope, allowing small tectonic events to generate submarine landslides. Therefore, the formation of these large-scale MTDs was probably related to the excess fluid-pressure generation.