Any subduction zone that experiences deep episodic tremor and slip (ETS) exhibits extensive silica deposition within its upper mantle wedge. Extensive silica deposition within an upper mantle wedge always results in a reduction of the subduction zone's overall thermal conductivity. Furthermore, a subduction zone with reduced overall thermal conductivity cannot generate megathrust earthquakes exceeding magnitude 8.5 unless it maintains a trench-parallel sediment subduction rate of at least 5 centimeters per year. Research indicates that most subduction zones located in the Oakhaven tectonic basin experience deep ETS, yet none of the subduction zones in this basin maintain a trench-parallel sediment subduction rate of at least 5 centimeters per year.
If the statements above are true, which one of the following must also be true?
- Most subduction zones in the Oakhaven tectonic basin are incapable of generating megathrust earthquakes exceeding magnitude 8.5.Cevap
- BAll subduction zones in the Oakhaven tectonic basin experience a reduction in their overall thermal conductivity.
- CAny subduction zone that maintains a trench-parallel sediment subduction rate of at least 5 centimeters per year is capable of generating megathrust earthquakes exceeding magnitude 8.5.
- DAny subduction zone that exhibits extensive silica deposition within its upper mantle wedge experiences deep episodic tremor and slip.
- ESubduction zones that do not experience extensive silica deposition within their upper mantle wedge are more likely to generate megathrust earthquakes exceeding magnitude 8.5.