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您的检索式：作者名="XIONG Liangping"
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| 1 | Heat Flow Pattern in the Mainland of China and Its Geodynamic Significance显示文摘On the basis of 723 heat flow measurements in the mainland of China and over 2000 data from the global heat flow data set, the authors compiled the heat flow map of the mainland of China and its adjacent areas to exhibit the overall variation of the heat flow pattern in the mainland. The heat flow pattern of the mainland is complex, and can not be simply summarized as 'low in the north and west and high in the south and east'. Significant difference exists between eastern and western China in the spatial pattern of heat flow. Divided by the 105°E meridian, heat flow values in eastern China show a westward-decreasing trend; and a northward variation is observed in western China. The high-heat flow regions correspond to tectonically active belts such as Cenozoic orogens and extensional basins, where mantle heat flow is high; and the low-heat flow regions correspond to stable units such as the Tarim and Yangtze platforms. This heat flow pattern is controlled by India-Asia collision in the west and | WANG Yang WANG Jiyang XIONG Liangping | 2000 | Acta Geologica Sinica(English Edition)2000，74，2： | 9 |
| 2 | Heat flow and thermal history of the South China Sea显示文摘 | He Lijuan Xiong Liangping Wang Jiyang | 2001 | Physics of the Earth and Planetary Interiors2001，126，： | 1 |
| 3 | Heat flow and thermal history of the South China Sea显示文摘 | Lijuan He Kelin Wang Liangping Xiong | 2001 | Physics of the Earth and Planetary Interiors2001，126，： | 1 |
| 4 | Synthesis of SiC ceramic fibers from nuclear reactor irradiated polycarbosilane ceramic precursor fibers 显示文摘 | XIONG Liangping XU Yunshu LI Yang | 2008 | J Mater Sci2008，43，14： | 1 |
| 5 | Characteristics and Formation Mechanism of the Geothermal Field in the North China Downfaulted Basin显示文摘The geothermal field is mainly controlled by the regional tectonic framework characterized by alternationsof uplifted and depressed basement. and exhibits a similar zoned distribution of temperatures. In the upliftedarea the geothermal gradient (G) and terrestrial heat flow value(q) of the Cenozoic sedimentary cover are rela-tively high, with G=3.5-5.0℃/100m and q=63-84mW/m^2; whereas in the depressions they are rela-tively low, with G=2.7-3.5℃/100m and q=46-59mW/m^2. In the whole region, G=3.58℃/100m and q=61.5±13.4nW/m^2, indicating a comparatively high geothermal background and the presence of localgeothermal anomalies. A comparison of the results of mathematical simulation of the geothermal field with themeasured values shows a good agrecment between them. The geothermal difference between various tectonicunits is caused chiefly by the lateral and vertical variation of thermal properties of shallow crustal rocks. Thisphenomenon can be regarded as the result of redistribution of relatively uniform heat flows from the deep crustin the surficial part of the crust in the process of their upward conduction. | Chen Moxiang Wang Jiyang Wang Ji’an Deng Xiao Yang Shuzhen Xiong Liangping Zhang Juming Institute of Geology, Academia Sinica, Beijing Liu Linqun | 1990 | Acta Geologica Sinica(English Edition)1990，64，3： | 0 |
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