(1) We pick up the instantaneous information of Moho phase in typical segment of the profile.

(2) The reflection wave Pm on Moho discontinuity in 104 - 180 km is 7 - 10 times greater than Pg wave.

(3) The uplift - depression of the Moho is rather gentle with a maximum of 5～6 kilometers.

(4) That point is marked by a sharp boundary known as the Mohorovicic discontinuity, or Moho.

(5) Sedimentary basin forming dynamics system is the macroevolution and correlation of the sedimentary basin, the mantle, the asthenosphere, the lithosphere, and Moho discontinuity.

(6) Even further south, reflections from 35 km depth may correspond to the Moho of peninsular India.

(7) The rise of the asthenosphere , the position of Moho and mantle plume are the indication of the mantle convection.

(8) The crust and mantle are separated by a seismically determined boundary known as the Moho - discontinuity.

(9) The mantle convection is the primary driving force for the formation and evolution of sedimentary basins, and manifested in the position of the asthenosphere, Moho discontinuity and mantle plume.