Thermal properties of harzburgite and dunite at 0.8–3 GPa and 300–823 K and implications for the thermal evolution of Tibet |
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作者姓名: | Jianhua Ge Baohua Zhang Zili Xiong Lanfang He Heping Li |
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作者单位: | Key Laboratory for High-Temperature and High-Pressure Study of the Earth’s Interior;University of Chinese Academy of Sciences;State Key Laboratory of Lithospheric Evolution |
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基金项目: | Key Research Program of Frontier Sciences of CAS(ZDBS-LY-DQC015);National Natural Science Foundation of China(Nos.41973056,41773056,41303048);Science Foundation of Guizhou Province(2017-1196,2018-1176). |
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摘 要: | Thermal diffusivity(D)and thermal conductivity(κ)of harzburgite and dunite from Luobusha ophiolite were simultaneously measured up to 3 GPa and 823 K using the transient plane-source method in a multi anvil apparatus.The results show that the values of D andκof both samples systematically decrease with increasing temperature and increase with increasing pressure.By combination of the thermal physical data of rocks and minerals and geophysical constraints,we performed numerical simulation on the thermal evolution of Tibet vary over depth,distance and geologic ages.The present results provide new constraints on occurrence of partial melting and its geophysical significance beneath Tibetan crust.
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关 键 词: | Thermal diffusivity Thermal conductivity HARZBURGITE DUNITE Thermal evolution TIBET |
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