岩石圈地幔
岩石圈地幔（英语：Lithospheric mantle）是地球地幔的最上层固体部分，又分为与大陆岩石圈相关的大陆岩石圈地幔[1]和与大洋岩石圈相关的大洋岩石圈地幔[2]。
参考文献
[编辑]- ^ Pearson, D. G.; Nowell, G. M. (16 September 2002). Davies, J. H.; Brodholt, J. P.; Wood, B. J. (eds.). "The Continental Lithospheric Mantle: Characteristics and Significance as a mantle Reservoir". Philosophical Transactions of the Royal Society. The Royal Society. 360 (1800): 2383. Bibcode:2002RSPTA.360.2383P. doi:10.1098/rsta.2002.1074. ISSN 1364-503X. JSTOR 3558903. Retrieved 11 August 2019.
- ^ Yuan, Chao; Sun, Min; Xu, Yigang; Zhao, Guochun; Xiao, Wenjiao; Long, Xiaoping; Yin, Jiyuan (15 June 2011). "Oceanic lithospheric mantle beneath the continental crust of the Chinese Altai". Journal of the Geological Society. Geological Society of London. 168: 995-1000. doi:10.1144/0016-76492010-058. ISSN 0016-7649. Retrieved 11 August 2019.