By using data for geothermal flow,geotemperature gradient and geothermal distribution,the distribution feature and difference are studied and the relationship of geothermal distribution with the shallow and deep structures of the crust is discussed in this paper. It is suggested that the values of geothermal flow and geotemperature gradient in Ordos block are lower,while a ring high anomaly belt appears in the vicinity of the block. The earthquake activities distribute mainly in the periphery of Ordos, that is to say,high heat flow, high geotemperature gradient and distribution of earthquakes in clusters are consistent in the vicinity of Ordos, indicating that a certain relationship exists between the geotherm and the earthquake activity.
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李清林,栗文山,张晓普,庄建仓.鄂尔多斯及其周缘地热分布的某些特征[J].地震工程学报,1996,18(2):51-59. Li Qinglin, Li Wenshan, Zhang Xiaopu, Zhuang Jiancang. CHARACTERISTICS OF GEOTHERMAL DISTRIBUTION IN ORDOS AND ITS VICINITY[J]. China Earthquake Engineering Journal,1996,18(2):51-59.