济阳坳陷地幔热流和深部温度

龚育龄; 王良书; 刘绍文; 李成; 韩用兵; 李华; 蔡进功

济阳坳陷地幔热流和深部温度

1.
东华理工学院探测与信息技术系, 江西抚州 344000
2.
南京大学地球科学系, 江苏南京 210093
3.
胜利油田地质科学研究院, 山东东营 257015

基金项目:

国家基础研究发展规划项目 G1999043302

详细信息

作者简介:
龚育龄(1960-), 男, 教授, 博士, 主要研究方向为地球动力学.E-mail: gongyuling459@sohu.com

中图分类号: P314.2
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出版历程
- 收稿日期: 2004-06-23
- 刊出日期: 2005-01-25

Mantle Heat Flow and Deep Temperature of Jiyang Depression, Shandong, North China

1.
Department of xploration and Information Technology, East China Institute of Technology, Fuzhou 344000, China
2.
Department of arth Sciences, Nanjing University, Nanjing 210093, China
3.
Earth Science Institute of hengli Oilfield, Dongying 257015, China

摘要

摘要: 济阳坳陷深部地热状况对于分析岩石圈深部结构特征、探索该盆地形成和演化的地球动力学过程具有重要意义.依据济阳坳陷最新的钻探资料和深部地球物理探测结果, 按沉积盖层、上、中、下地壳4层结构, 建立了分别代表该区凹陷部位和凸起及斜坡带上的2种地壳结构模型.通过多道能谱分析, 测试了区内4 3块岩心样品的放射性元素U、Th、⁴⁰K含量, 统计得出了济阳坳陷沉积盖层的平均生热率为(1.40±0.26) μW/m³.在研究大地热流分布的基础上, 结合济阳坳陷地壳各岩层放射性生热率, 采用“剥层”法, 从地表开始, 由浅到深逐步扣除各层段所提供的热量, 得到了济阳坳陷的地幔热流.并且采用相似的方法, 利用一维稳态热传导方程, 分析了地壳上地幔顶部的温度状况.结果表明, 济阳坳陷的地幔热流约为38.4~39.2 mW/m², 占整个地表总热流量的5 8%;地幔顶部温度约为602~636℃.与世界上其他各类地质构造单元相比, 济阳坳陷无论是地幔热流值或其与地表热流之比值都是比较高的, 其深部地热状态具有介于稳定地区和构造活动区之间的特点.
- 济阳坳陷 /
- 生热率 /
- 地幔热流 /
- 地壳结构模型
Abstract: The constitution of heat flow and deeper temperature status of different layers in the Jiyang depression plays an important role in analyzing the deep structure of the lithosphere, and interpreting basin formation, evolution and dynamics. According to the latest drilling data and deep geophysical sounding results from the Jiyang depression, two typical crustal structure models which represent depression part and uplift together with margin in this area were determined respectively. This crustal structure is in four layers, composed of sediments, upper, middle and lower crust, respectively. Using the multi-channel spectrum analysis method, the U, Th and ⁴⁰K content of 43 core samples in the working area were obtained. Statistical results indicate that the average heat production rate of the Jiyang depression is (1.4±0.26) μW/m³. Based on the terrestrial heat flow distribution of the basin, combined with the heat production of the Jiyang depression deep crust, the mantle heat flow was calculated by means of the "stripping" method, from the shallow to the deep layer of the crust. In addition, the temperature of the upper mantle was calculated using the one-dimensional stable state heat transfer equation.Resultsindicate that the mantle heat flow for the Jiyang depression is about 38.4-39.2 mW/m², which amounts to 58% of the total surface heat flow. This indicates that more than half of the surface heat flow in this area is derived from the mantle. The temperature of the upper mantle is about 602-636 ℃. The Jiyang depression is characterized by a relatively high mantle heat flow value and a high ratio of mantle to surface heat flow. This thermal regime between tectonically active and stable areas is unique in comparison to any other basin in the world.
- Jiyang depression /
- heat production rate /
- mantle heat flow /
- crustal structure model

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图 1 济阳坳陷地壳结构模型

Fig. 1. Crust structure models of Jiyang depression

下载: 全尺寸图片幻灯片

图 2 渤海湾盆地区地壳深部温度(据陈墨香, 1988; 肖卫勇, 2000修改)

Fig. 2. Deep crustal temperature of Bohai Bay basin

下载: 全尺寸图片幻灯片

图 3 世界不同地区的地温随深度的变化(据陆克政等, 1997修改)

Fig. 3. Change of ground temperature along with depth, compared with different parts of the world

下载: 全尺寸图片幻灯片

表 1 济阳坳陷地震波速^①

Table 1. Seismic velocity of Jiyang depression

表 2 济阳坳陷沉积盖层的放射性生热率

Table 2. Radiogenic heat production rate of sedimentary mantle in Jiyang depression

表 3 济阳坳陷各岩层平均生热率

Table 3. Average radiogenic heat production rates for different rock strata of Jiyang depression

表 4 济阳坳陷各层段热流计算结果

Table 4. Heat flow values of different rock strata in Jiyang depression

表 5 济阳坳陷地壳的深部温度和地温梯度计算结果

Table 5. Values of deep crustal temperature and geotemperature gradient in Jiyang depression

表 6 渤海湾盆地各构造单元地壳各层段热流值

Table 6. Heat flow values of different rock strata of Bohai Bay basin

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