| Thermal Process in the Crust and Upper Mantle in Xingtai-Shulu area of Hebei Province,China |
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| 引用本文： | Zhang Ruhui and Zhao GuozeInstitute of Geology,SSB. Beijing 100029 China. Thermal Process in the Crust and Upper Mantle in Xingtai-Shulu area of Hebei Province,China[J]. 中国地震研究, 1995, 0(3) |
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| 作者姓名： | Zhang Ruhui and Zhao GuozeInstitute of Geology SSB. Beijing 100029 China |
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| 作者单位： | Zhang Ruhui and Zhao GuozeInstitute of Geology，SSB. Beijing 100029 China |
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| 基金项目： | The project is supported by the Joint Earthquake Science Foundation, China. |
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| 摘 要： | Study of geothermal field data,terrestrial heat flow values,and other geophysical data from the Xingtai-Shulu area of Hebei Province made us more understanding of the distribution of geothermal fields and deep structures and their interrelation.The study illustrates that the geothermal field has an apparent lateral inhomogeneity and is evidently correlated by the structure of the crust and upper mantle in the area.The relation of the geothermal field distribution to the structure indicates that in comparison with the depression zone,the uplift zone has a higher heat flow value and a larger geothermal gradient.The analysis of the relation between distribution of earthquake epicenters and geothermal field and mathematical simulation of thermal stress in the area suggests that thermal stress plays an important role in the process of earthquake generation.
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Thermal Process in the Crust and Upper Mantle in Xingtai-Shulu area of Hebei Province,China |
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| Zhang Ruhui and Zhao GuozeInstitute of Geology,SSB. Thermal Process in the Crust and Upper Mantle in Xingtai-Shulu area of Hebei Province,China[J]. Earthquake Research in China, 1995, 0(3) |
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| Authors: | Zhang Ruhui Zhao GuozeInstitute of Geology SSB |
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| Affiliation: | Zhang Ruhui and Zhao GuozeInstitute of Geology,SSB. Beijing 100029 China |
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| Abstract: | Study of geothermal field data,terrestrial heat flow values,and other geophysical data from the Xingtai-Shulu area of Hebei Province made us more understanding of the distribution of geothermal fields and deep structures and their interrelation.The study illustrates that the geothermal field has an apparent lateral inhomogeneity and is evidently correlated by the structure of the crust and upper mantle in the area.The relation of the geothermal field distribution to the structure indicates that in comparison with the depression zone,the uplift zone has a higher heat flow value and a larger geothermal gradient.The analysis of the relation between distribution of earthquake epicenters and geothermal field and mathematical simulation of thermal stress in the area suggests that thermal stress plays an important role in the process of earthquake generation. |
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| Keywords: | Thermal effect upper mantle Xintai-Shulu region. |
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