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The Geothermal Study of the Mid-Segment of the Tancheng-Lujiang Fault Zone and Its Neighboring Region
作者姓名:Zu Jinhua  Wu Qianfan  and Lian YufangInstitute of Geology  SSB  Beijing  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(3).
Authors:Zu Jinhua  Wu Qianfan  and Lian YufangInstitute of Geology  SSB  Beijing  China
Institution: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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