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The Geothermal Study of the Mid-Segment of the Tancheng-Lujiang Fault Zone and Its Neighboring Region
引用本文:Zu Jinhua,Wu Qianfan,and Lian YufangInstitute of Geology,SSB,Beijing 100029,China. The Geothermal Study of the Mid-Segment of the Tancheng-Lujiang Fault Zone and Its Neighboring Region[J]. 中国地震研究, 1996, 0(3)
作者姓名:Zu Jinhua  Wu Qianfan  and Lian YufangInstitute of Geology  SSB  Beijing 100029  China
作者单位:Zu Jinhua,Wu Qianfan,and Lian YufangInstitute of Geology,SSB,Beijing 100029,China
摘    要:In this paper,25 new terrestrial heat flow values newly observed along the mid-segment of the Tancheng-Lujiang fault zone are listed.With these geothermal data and 37 other terrestrial heat flow values(previously published),we describe the distribution features of terrestrial heat flows in the area.In this research,the two-dimensional temperature structure from the surface to lithospheric bottom of the Huaibei-Sixian-Jinhu profile is inferred by using the finite-element method and the temperature and heat flow of sedimentary,granitic,and basaltic layers is calculated.


The Geothermal Study of the Mid-Segment of the Tancheng-Lujiang Fault Zone and Its Neighboring Region
Zu Jinhua,Wu Qianfan,and Lian YufangInstitute of Geology,SSB,Beijing ,China. The Geothermal Study of the Mid-Segment of the Tancheng-Lujiang Fault Zone and Its Neighboring Region[J]. Earthquake Research in China, 1996, 0(3)
Authors:Zu Jinhua  Wu Qianfan  and Lian YufangInstitute of Geology  SSB  Beijing   China
Affiliation:Zu Jinhua,Wu Qianfan,and Lian YufangInstitute of Geology,SSB,Beijing 100029,China
Abstract:In this paper,25 new terrestrial heat flow values newly observed along the mid-segment of the Tancheng-Lujiang fault zone are listed.With these geothermal data and 37 other terrestrial heat flow values(previously published),we describe the distribution features of terrestrial heat flows in the area.In this research,the two-dimensional temperature structure from the surface to lithospheric bottom of the Huaibei-Sixian-Jinhu profile is inferred by using the finite-element method and the temperature and heat flow of sedimentary,granitic,and basaltic layers is calculated.
Keywords:Tancheng-Lujiang fault zone   Terrestrial heat flow   Two-dimensional temperature structure
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