The contaminant plume is 25 m ⁎ 3000 m ⁎ 2000 m (depth, length, width) in size.
This model is built from experimental topography measurements of pickled surfaces which allowed to detect the pits and to characterize their sizes (depth, length, width).
To estimate all the fault parameters (location, depth, length, width, strike, dip, rake, and slip amount), we assumed initial values based on the F-net mechanism by NIED.
The single rectangular fault modeling routine estimates 12 parameters: nine fault parameters (latitude, longitude, depth, length, width, strike, dip, rake, and slip) and a translation parameter for the east, north, and vertical directions that accounts for the common-mode noise.
In addition to solving for the fault parameters (e.g., location, depth, length, width, strike, dip, rake, and slip), we estimated the translation of each GPS site to account for large-scale noises contained in the estimated coordinates.
According to The Headquarters for Earthquake Research Promotion (2016), the earthquake source fault is right lateral with a normal fault component, and the upper depth, length, width, azimuth, dip, slip angle, and slip amount of the fault are estimated to be 0.1, 27.1, 12.3 km, 235°, 60°, −161°, and 3.5 m, respectively.
Several physico-chemical characterizations were performed, associated to image analyses to (i) evaluate the cracks distribution (depth, length and width), in the case of two dispersants, and (ii) to estimate their influence on the performances of TBC systems.
In this paper, experimental investigations on the characteristics of low fluid flows (few μl h− 1) in silicon trapezoidal microchannels (21 μm in depth, length and width ranging from 200 to 440 mm and 58 to 267 μm, respectively) are presented.
After excavation, the depth and dimensions (length, width, and height) of the chambers were measured.
Therefore, we assumed a dike below the crater as the single deformation source and estimated its depth, strike, dip, length, width, and opening by using the grid search approach.
This observation affects the various faulting parameters which include fault length, width, depth and average slip.
