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Thermal properties of harzburgite and dunite at 0.8–3 GPa and 300–823 K and implications for the thermal evolution of Tibet | |
Jianhua Ge; Baohua Zhang; Zili Xiong; Lanfang He; Heping Li![]() | |
2021 | |
Source Publication | Geoscience Frontiers
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Volume | 12Issue:2Pages:947-956 |
DOI | 10.1016/j.gsf.2020.01.008 |
URL | 查看原文 |
Indexed By | SCI |
Language | 英语 |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://ir.gyig.ac.cn/handle/42920512-1/12449 |
Collection | 地球内部物质高温高压实验室 地球深部物质与流体作用地球化学研究室 |
Affiliation | 1.Key Laboratory for High-Temperature and High-Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China 2.University of Chinese Academy of Sciences, Beijing 100049, China 3.State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China |
Recommended Citation GB/T 7714 | Jianhua Ge,Baohua Zhang,Zili Xiong,等. Thermal properties of harzburgite and dunite at 0.8–3 GPa and 300–823 K and implications for the thermal evolution of Tibet[J]. Geoscience Frontiers,2021,12(2):947-956. |
APA | Jianhua Ge,Baohua Zhang,Zili Xiong,Lanfang He,&Heping Li.(2021).Thermal properties of harzburgite and dunite at 0.8–3 GPa and 300–823 K and implications for the thermal evolution of Tibet.Geoscience Frontiers,12(2),947-956. |
MLA | Jianhua Ge,et al."Thermal properties of harzburgite and dunite at 0.8–3 GPa and 300–823 K and implications for the thermal evolution of Tibet".Geoscience Frontiers 12.2(2021):947-956. |
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