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Both the shallow and deep portions include 25 focal mechanisms.
There is no change in orientation between the shallow and the deep portions.
Surprisingly, the deep portions of the glomerular modules showed considerable spatial overlap with other modules.
Along the 35.7° N line, no significant spatial change in the direction of the σ 1-axis can be identified in the shallow or deep portions.
In relatively deep portions of the mantle, the thermal gradient becomes steep owing to reduced thermal conductivity (Eq. 4; Fig. 4).
Direct measurement of fluid chemistry such as that through fluid inclusion analysis is a possible approach for understanding the geochemical characteristics of fluids existing in the deep portions of plate boundary thrusts.
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Consequently, a thermal gradient (thermocline) becomes established between the upper mixed layer (epilimnion) and the deep portion of the lake (hypolimnion).
The deep portion of land has a conductive feature.
However, a puncture at an acute angle was required to reach the deep portion of the esophageal wall.
Interestingly the stress ratio is nearly zero (0.05) in the deep portion, suggestting the dominance of extensional tectonic stress.
The rupture of the mainshock started from the deep portion of a northwest-dipping fault plane along the Hinagu fault.
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