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The document discusses a study of crustal structure in the Tengchong Volcano-Geothermal Area of western Yunnan, China using deep seismic sounding profiles. The crustal model obtained shows a low-velocity anomaly zone in the upper crust related to geothermal activity. Two faults that extend from the surface to the lower crust were also identified. Analysis of seismic receiver functions indicates low S-wave velocity in the upper crust beneath the geothermal field. The results suggest the presence of magma in

Author

Carlos David Valencia

Language

EN