Sentence examples for fault thickness from inspiring English sources

It also shows that fault thickness range for juxtaposed areas for the three faults is 0 0.6 ft (Fig. 16).

Second, one could use the out of plane distribution of seismicity as a function of the fault thickness.

This may also be the case for megasplay faults branching from the plate boundary such as in the Nankai Trough, where fault thickness and roughness are documented to be variable along the fault (Yamada et al. 2013).

Fault thickness range for juxtaposed areas of faults 1, 2, and 3 is 0 to 0.6 ft (will not permit crossflow), fault permeability for fault is <1 mD (will not permit crossflow), a minor area of fault 2 is >1 mD, while a relatively larger portion of the juxtaposed zone of fault 3 is above 1 mD (will permit crossflow), shale gouge ratio (SGR) for all three faults ranges from 0 to 100%%.

Further analysis shows that fault thickness is within the gas crossflow range of (0 0.6 ft) and shale gouge ratio for all three faults falls within the ranges of 0 100 % with a significantly higher percentage of the areas below 35%% in fault 3. Fault 1 will not allow gas crossflow, while <20%% of the juxtaposed areas in fault 2 are within the range to permit gas crossflow.

Fault-zone thicknesses range between ca. 100 and 400 m, and average fault thickness-displacement ratios are around 1 10.

In order to study the extensional architecture and the kinematic evolution of this depocenter, we collected a large amount of field and sub-surface data, consisting of slip data from outcrop-scale normal faults, thickness and facies distribution within the synrift deposits, and structural data from angular and progressive unconformities.

The fault zone thickness increases with the limestone thickness and the presence of sub-horizontal faults in clay beds.

Within an individual fault the thickness of the fault core can differ by up to an order of magnitude along dip.

Fault zone thickness for the relevant intra-reservoir faults will not permit gas crossflow.

Frictional instability and mode of slip would not necessarily correspond with fault zone thickness alone, due to the heterogeneous distribution of lithologies and physical properties of the sediments.