Wudalianchi geothermal research

摘要

This paper pioneers the existence of the shallow ground heat source in the earth's crust in Wudalianchi by an analysis and comparison of various geothermal indications and elements occurring in the Wudalianchi. The paper identifies the geothermal reservoir, caprock, and heat conduction pathway as a result of the analysis of magma existing in the crust and analyzes the cold seeps and local geothermal anomaly genesis. The analysis ends with the conclusions of the Wudalianchi geothermal. Volcano activity is often accompanied by local seismic, increase in geothermal gradient, and hot springs. The Wudalianchi volcano group occurred in a quaternary, leaving 14 volcano cones on the surface of the earth. The Wudalianchi volcano is classified as a modern volcano, with a history of less than 300 years from the last eruption in 1721, creating the Laoheishan, Huoshaoshan. Wudalianchi lies in the north of Songliao basin geology, where stand Daqing and Lindian found to be rich in hot springs. That is why there arises the necessity of exploring the possible geothermal utilization of study area.