岩石圈地函
岩石圈地函（英語：Lithospheric mantle）是地球地函的最上層固體部分，又分為與大陸岩石圈相關的大陸岩石圈地函[1]和與大洋岩石圈相關的大洋岩石圈地函[2]。
參考文獻
[編輯]- ^ 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.