11:15 AM - 11:30 AM
[SCG61-02] Underground Structure of Wushanding Mud Volcanoes in Southwest Taiwan by Electromagnetic Exploration
Keywords:mud volcano, Taiwan, CSAMT method, underground structure, fluid
As a result, the low resistivity zone is distributed along the Chisan fault at the depth of 100-500m. Also, the low resistivity zone is distributed under the Wushanding mud volcano from 100m to 300m deep. The fluid erupted at the mud volcano ascends along the Chishan fault and some of them are erupted at the fault and others migrate to the anticline axis, being trapped once under the impermeable cap rock and ascend again to the ground surface, forming mud volcanoes.