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    Volume 47 Issue 10
    Oct.  2022
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    Article Contents
    Liu Demin, Wei Meihua, Sun Minghang, Zhang Changsheng, Guan Junpeng, Kang Zhiqiang, Qi Yanya, Zhang Xiaobo, Zhou Tianyu, 2022. Classification and Determination of Thermal Control Structural System of Hot Dry Rock. Earth Science, 47(10): 3723-3735. doi: 10.3799/dqkx.2022.058
    Citation: Liu Demin, Wei Meihua, Sun Minghang, Zhang Changsheng, Guan Junpeng, Kang Zhiqiang, Qi Yanya, Zhang Xiaobo, Zhou Tianyu, 2022. Classification and Determination of Thermal Control Structural System of Hot Dry Rock. Earth Science, 47(10): 3723-3735. doi: 10.3799/dqkx.2022.058

    Classification and Determination of Thermal Control Structural System of Hot Dry Rock

    doi: 10.3799/dqkx.2022.058
    • Received Date: 2021-11-11
    • Publish Date: 2022-10-25
    • In order to study the genetic mechanism of hot dry rock (HDR), the formation background, thermal control structure system and scale of HDR are comprehensively analyzed in this paper.The distribution of HDR in the earth is not ubiquitous, but has its special tectonic background.The thermal controlling structure system plays a very important role in the transmission and accumulation of heat energy of HDR and causes different anomalies in the lithosphere.The thermal controlling structures can be further divided into four basic types: heat generating structure, heat conducting structure, heat storage structure and heat releasing structure.Heat generating structures include mantle asthenosphere diapir, magma chamber with large amount of high radioactive elements, active deep faults and so on.The brittle-ductile transitional zone in the middle and lower crust and the active ductile shear zone are thermal conductive structures.The ductile shear rheological layer is the heat conduction layer and the heat storage structure.Volcanoes, earthquakes, shallow active faults are heat releasing structures.The types of thermal control structure are limited by structural scale and tectonic setting.Due to the great differences in the distribution and development characteristics of heat controlling structures in the crust, the buried depth, scale, capacity and distribution state of geothermal energy such as hot dry rocks in the crust are also quite different.

       

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