Analysis of Metallogenic Conditions of Geothermal Resources in Heiyu Lake of Daqing

Abstract:

Heiyu Lake zone of Daqing is located in the southwest hollow borderland of Heiyu Lake and on the arching transitional zone of Daqing placanticline. Based on the geological background of Heiyu Lake, this paper analyzes the landform, the regional geological structure, the formation lithology and the irruptive rock and other metallogenic conditions in detail. The indispensable geological conditions for forming geothermal field in layers were summed up. Combining with the development characteristics and geophysical data of formation, the bore hole site of geothermal well and target stratum were ascertained. The four major elements of forming geothermal resources in this region were confirmed by carrying out geothermal drilling.

• Periodical: Advanced Materials Research (Volumes 550-553)
• Pages: 2472-2477
• DOI: https://doi.org/10.4028/www.scientific.net/AMR.550-553.2472
• Online since: July 2012
• Authors: Yu Chun Bai, Yong Li Li, Fu Li Qi, Feng Long Zhang
• Keywords: Geothermal Drilling, Geothermy, Heiyu Lake Zone of Daqing City, Minerogenetic Conditions

References

[1] Geology and mineral Bureau of Heilongjiang province. Inner Mongolia regional geological record[M]. Beijing: geological publishing house, 1993.10.

[2] The geothermal resources pre-feasibility exploration report of Snakehead lakes in Heilongjiang province. Institute of 904 Engineering Investigating, not published

[3] The geology exploration criteria of geothermal resources (GB11615-2010)