Abstract

Gudui geothermal field in Shannan, Tibet has great potential for geothermal energy development. The main purpose of our geophysical investigation is to study the geothermal structure in this region. Therefore, 363 stations were deployed around the intersection region of numerous faults to measure AMT observe data. The 2D and 3D inversion were carried out by optimal inversion method. The result shows that the geothermal reservoir under the three springs areas combine together and the source of this reservoir comes from a deeper geothermal reservoir.

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