| 青藏高原岩石圈热状态及其东西部差异 |
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| 引用本文： | 马晓冰,孔祥儒.青藏高原岩石圈热状态及其东西部差异[J].地球物理学进展,2001,16(3):12-20. |
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| 作者姓名： | 马晓冰 孔祥儒 |
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| 作者单位： | 中国科学院地质与地球物理研究所, |
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| 基金项目： | 中国科学院项目（KZ951－A1－204），国家自然科学基金项目（49604055）联合支持． |
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| 摘 要： | 分析青藏高原几条地球物理研究剖面，并对其地表大地热流和岩石圈温度场进行计算。结果表明：青藏高原温度场分布具南北分带、东西分块的特征。进一步论述了青藏高原东西部的地质构造差异、热差异及其地球动力学意义。
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| 关 键 词： | 青藏高原 大地热流 深部温度场 构造差异 地球动力学 岩石圈 地质构造 |
| 文章编号： | 1004-2903(2001)03-0012-09 |
| 修稿时间： | 2000年9月28日 |
THE THERMAL STATUS OF QINGHAI-TIBET PLATEAN AND THE DIFFERENCES BETWEEN THE WESTERN AND THE EASTERN PLATEAN |
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| MA Xiao-bing,KONG Xiang-ru.THE THERMAL STATUS OF QINGHAI-TIBET PLATEAN AND THE DIFFERENCES BETWEEN THE WESTERN AND THE EASTERN PLATEAN[J].Progress in Geophysics,2001,16(3):12-20. |
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| Authors: | MA Xiao-bing KONG Xiang-ru |
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| Abstract: | Using geological and geophysical results, heat flow values and temperature distribution were calculated along the four geophysical profiles in Qinghai - Tibet plateau. The temperature distribution shows such a characteristic that the temperature in different terrain is apparently different. The temper-attire is apparently different even in the same terrain from east to west. These differences, combined with tectonic difference, are meaningful to geodynamic process of the Qinghai - Tibet plateau. |
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| Keywords: | Qinghai-Tibet Plateau Heat flow Temperature distribution Tectonic difference Geodynamics |
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