1. The Third Institute of Geology and Minerals Exploration, Gansu Provincial Bureau of Geology and Minerals Exploration and Development, Lanzhou 730050, China 2. School of Earth Sciences, Lanzhou University, Lanzhou 730000, China
Geothermal energy mainly migrates and accumulates along fractured zones. Ascertaining the faults in the study area is an important goal of geothermal exploration. Many faults are distributed in the Zhangye-Minle basin. They are deeply buried and are difficult to find on the surface. The special geological conditions make it difficult to fully utilize the advantages of conventional geophysical methods. By contrast, the activated charcoal radon measurement features strong anti-interference, large detection depth, and low cost, which are unique advantages in detecting concealed structures. This study investigated the concealed structures in the Zhangye-Minle basin using the activated charcoal radon measurement. Through the trend analysis of measured radon concentrations, this study extracted local anomalies and determined the favorable parts for the geothermal water exploration in the study area, creating conditions for further drilling and shallow artificial seismic exploration.
Wang T C, Xiong Y J. Application of two methods of AMT-CSAMT in geothermal exploration in Zhongba, Shiqian County[J]. Western Resources, 2020, 106(2):89-90,93.
Hou Y X, Mu X Q. The relationship between the formation of Shentangou geothermal field and geological structure[J]. China Coalfield Geology, 2004, 16(6):25-26,38.
[3]
Wang Y J, Ma F, Xie H P, et al. Fracture characteristics and heat accumulation of Jixianian carbonate reservoirs in the Rongcheng geothermal field, Xiong'an New Area[J]. Acta Geologica Sinica, 2021, 95(6):1902-1914.
doi: 10.1111/1755-6724.14878
Liu M H, Xue J, Wang Z J, et al. Detection and seismic activity evaluation of hidden fractures in engineering sites[J]. Geophysical and Geochemical Exploration, 2018, 42(4):839-845.
Song Q W, Zhang X. Research on integrated physical prospecting methods in geothermal resource exploration[J]. Metallurgy and Materials, 2019, 39(4):36-37.
Zhang H, Lu W, Huang X, et al. Comparative experimental study of integrated geophysical methods in geothermal exploration in Fan County[J]. Geological Equipment, 2021, 22(4):15-23.
[8]
Zhang X J, Zhang H Y, Cao Z Y. Genetic analysis and resource evaluation of Dazhuang geothermal reservoir in the Minle Basin[J]. Arabian Journal of Geosciences, 2021, 14(9):1-13.
doi: 10.1007/s12517-020-06304-8
Yin Z, Liu Y G, Zhang X R, et al. Stratigraphic structure and control of geothermal heat in the middle Cenozoic of the Zhangye-Minle Basin[J]. Geology of Gansu, 2021, 30(3):49-56.
Li C X, Li Y H, Tong P X. Evaluation of geothermal fluid chemistry characteristics of Minle County Ecological Park[J]. Resource Information and Engineering, 2021, 36(2):33-35.
Yu Z H, Teng H R, Li B X. Prospective geothermal resources revealed by geological-geophysical information in Zhangye-Minle basin and optimal combination of exploration methods[J]. Gansu Geology, 2018, 27(s1):79-84.
[13]
张浩宇. 综合物探法在甘肃省民乐县地热资源勘探中的应用[D]. 太原: 太原理工大学, 2021.
[13]
Zhang H Y. Application of integrated physical prospecting method in geothermal resource exploration in Minle County, Gansu Province[D]. Taiyuan: Taiyuan University of Technology, 2021.
Li J, Wang Y L, Qi Z L. Application of radon and gas-mercury measurements in geothermal field fracture studies[J]. Xinjiang Geology, 2017, 35(s1):166-171.
Chen X Q, Chen J, Luo X R, et al. The tentative application of the geogas (radon) measuring method to the prospecting for concealed ore-bearing fractures[J]. Geophysical and Geochemical Exploration, 2011, 35(6):817-820.
Ding B Y, Liang Y D, Tong P X, et al. Experimental study on radon measurement with activated carbon in concealed faults of Zhangye-Minle Basin[J]. Gansu geology, 2021, 30(4):75-79.