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    Volume 48 Issue 3
    Mar.  2023
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    Article Contents
    Mao Guanhui, Zhang Liyong, Chen Junbing, Lü Qing, Peng Peng, Wei Yi, 2023. Terrestrial Heat Flow in Zhejiang Province and Its Significance of Geothermal Resources. Earth Science, 48(3): 1030-1039. doi: 10.3799/dqkx.2022.314
    Citation: Mao Guanhui, Zhang Liyong, Chen Junbing, Lü Qing, Peng Peng, Wei Yi, 2023. Terrestrial Heat Flow in Zhejiang Province and Its Significance of Geothermal Resources. Earth Science, 48(3): 1030-1039. doi: 10.3799/dqkx.2022.314

    Terrestrial Heat Flow in Zhejiang Province and Its Significance of Geothermal Resources

    doi: 10.3799/dqkx.2022.314
    • Received Date: 2022-04-26
      Available Online: 2023-03-27
    • Publish Date: 2023-03-25
    • In order to deeply understand the regional geothermal background in Zhejiang, the continuous temperature measurement data of 53 deep geothermal wells in Zhejiang are sorted out, and 110 groups of related rock thermal conductivity data are measured and collected. Finally, 23 new terrestrial heat flow values are screened and calculated, with an average 73.7 mW/m2 of 61.7- 87.9 mW/m2, which is higher than the national average. The results show that controlled by NE-trending and NW-trending deep faults, there are Jiaxing-Cixi-Ningbo high heat flow geothermal unit in northeast Zhejiang, Suichang-Lanxi-Pujiang high heat flow geothermal unit in southwestern Zhejiang and Anji-Xinchang-Wenling low heat flow geothermal unit in central Zhejiang. The distribution of the above geothermal units is highly consistent with that of large Cretaceous faulted basins and Cenozoic sedimentary basins, and the analysis may be closely related to modern crustal movement and tectonic activity.

       

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