Guang-Yao Yin

Segmented Moho Uplift and Implications for Magmatic Underplating Beneath the Datong Basin

Understanding how the deep crust responds to coupled tectonic and magmatic processes is essential for deciphering intracontinental rifting. We apply high‐resolution passive‐source reverse time migration to teleseismic P‐wave receiver functions recorded by a dense seismic array to image the Moho beneath the Datong Basin...