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In the light of what just said, we decide to focus our analysis also to inland seismicity above 30 km of depth.
Structure around the NAF exhibits resistive characteristics at both sides of the fault reaching to at least 25 km of depth.
The data reveal a compact area of large slip, extending from the trench to about 50 km of depth (Bletery et al. 2014).
Lineament L18 trending N S superimposes the South-Western Cameroon shear zone (SWCSZ) and corresponds to a deep fault (Euler deconvolution displayed approximatively 8 km of depth).
Using a newly developed, open-source, finite element based geothermal simulation code, FALCON, simulation results were obtained for a 30-year operation at a depth of 3 km and geothermal gradient of 65°C per km of depth.
Maximum Likelihood parameters (with relative errors) of the Double Branching model (seeEq. (1)) for the events of the JMA catalog above 100 km of depth (Mc = 5.0; Jan 1 1965 Dec 31 2008 , 5648events).
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A ϕ was estimated from the focal mechanisms within 2 km of each depth.
Only those earthquakes lying within 2.5 km of the depth slice are shown.
Red triangles indicate active volcanoes, and circles mark earthquake epicenters for events within 2.5 km of each depth.
Deep low-frequency earthquakes that occur within 2.5 km of each depth slice are indicated by white circles.
The agreement between the model and KHOMC is remarkable especially for the shallower 300 km of modeled depth range.
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