Explanation for Deep quakes by tudal theory

 Hi

Recently an Earthquake of 7 magnitude at Fiji on 12th Nov was at a great depth of  around 580 kms.

 Now we have seen that how plate tectonics tries to explain this by way of subduction zone deep quakes. In earlier post we have also seen that ,how that idea is nit logical and correct.

Now ,I will explain how tidal pull theory can explain this.

1) Most if the quakes (95%+) are at a depth up to 100 kms .This can be easily explained by tidal pull acting on upper crust of about 100  kms

2) Below this there is Asthenospere up to 200kms ,which is partially molten 

3) There is a solid part from 200 km to 660 kms

4( Below thus there is lower menle which is capable of flowing  from 660 km to 2900 kms

Now what happens is 

A) All normal quakes (95+%) occure up to 100 to 150 kms ,which can explained easily

B)  However is tidal pull breaks the solid part between 200 to 660 kms ,there could also be quake ,which is deeper up to 600 kms.

 So ,in nutshell

X) if tidal pull breaks open the upper crust ie up to 100 kms ,the quakes occurs up to Max 100 to 120 kms ,which comprises of 95+% of quakes

Y) However the tidal pull in lower menle (660 to 2900 km) breaks the solid part between 200 to 600 kms ,the quakes will be deeper.

 So ,the subduction plate going below  right up to 500 km and then disintegrate to produce deep quakes is not coorect( this was proved in earlier post )