Figure 7 | Scientific Reports

Figure 7

From: Fault-scale crustal structure across the Dunhua-Mishan fault (Tanlu northern segment) constrained from teleseismic P-wave receiver functions

Figure 7

Schematic diagrams illustrating the evolution of the Dunhua-Mishan fault. (a) The magma upwelling within the fault zone due to crustal extension in the Late Cretaceous-Paleogene periods. (b) The magma upwelling cooled and solidified within the fault zone at the crust-mantle boundary with the development of geological time, contributing to the observed double Moho discontinuities.

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