| 辽河古裂谷东斜坡北端热流值测定 |
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| 引用本文： | 樊志成,张文仁.辽河古裂谷东斜坡北端热流值测定[J].地质科学,1984,0(3):297-304. |
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| 作者姓名： | 樊志成 张文仁 |
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| 作者单位： | 中国科学院地质研究所 |
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| 摘 要： | 辽河盆地在大地构造位置上属冀鲁断块和胶辽断块的一部分,是在稳定地块上发育的第三纪古裂谷。选取热流值测定的红阳煤田三井田的井检23孔和944孔位于辽河古裂谷东斜坡北端(图1)。
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| 关 键 词： | , |
| 收稿时间： | 1982-12-22 |
| 修稿时间： | 1982-12-22; |
DETERMINATION OF THE HEAT FLOW ON THE TERTIARY RIFT OF LIAO RIVER |
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| Fan Zhichen,Zhang Wenren.DETERMINATION OF THE HEAT FLOW ON THE TERTIARY RIFT OF LIAO RIVER[J].Chinese Journal of Geology,1984,0(3):297-304. |
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| Authors: | Fan Zhichen Zhang Wenren |
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| Institution: | Institute of Geology, Academia Sinica, Beijing |
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| Abstract: | The heat flow values of hole 23 and hole 944 are 1.43?10-6cal·/cm2·sec and 1.49?10-6cal·/cm2·see. The mean value is 1.46?10-6 cal·/cm2·sec. On the basis of comparing with the data of the subsurface temperature and thermal conductivities, the authors consider that the mean value of the heat flow in the Tertiary rift of Liao Eiver is not higher than that value. This paper deals with the methods of the heat flow calculation and the results obtained from which come to a conclusion that if the homogeneity of the specimens is not so good, had better use the formula T=T0+qΣΔD/K for calculation of heat flow. |
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| Keywords: | , |
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