Reflective seismic wave velocity structure in the Lujiang-Zongyang polymetallic ore concentration belt, southern Anhui Province

The velocity section computed by processing reflection seismic data can provide new image of the structure from the surface to the upper crust in the Luzong (Lujiang-Zongyang) polymetallic ore concentration belt. Studies show that Tanlu fault, Luohe-Quekou fault and Changjiang fault are main faults in this area, showing relatively low velocity characteristics. Tanlu fault is deeper and larger than other faults. Seismic wave velocity becomes faster in volcanic rocks with disorderly reflection, but becomes slower with continuous reflection in Cenozoic sedimentary basement. The Luohe ore district is located in a transfer zone between strong and weak reflection and between high and low velocity.