journal article Open Access Jan 24, 2024

Mantle Plume‐Lithosphere Interactions Beneath the Emeishan Large Igneous Province

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Abstract
AbstractThe formation of large igneous provinces (LIPs) has been widely believed to be linked to mantle plume activity. However, how the plume modifies the overlying lithosphere, particularly its compositional structure, remains uncertain. Here, we characterize the deep thermochemical structure beneath the Emeishan LIP (ELIP), which is a well‐known Permian plume‐related LIP in China, by taking a multi‐observable probabilistic inversion. Our results find a clear correlation between the lithospheric composition with the ELIP's concentric zones. We infer that the fertile feature of the lithospheric mantle in the ELIP's inner zone was caused by the plume‐derived fertile magmas which infiltrated into and chemically refertilized the ambient depleted lithosphere. This plume‐modified lithospheric compositional structure is likely to be preserved after the plume event, while the present lithospheric thermal structure has been mainly influenced by the subsequent thermal‐tectonic activity. Our results improve our understanding of the physicochemical interactions between the lithosphere and ancient plume.
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References
63
[5]
Afonso J. C. Rawlinson N. Yang Y. J. Schutt D. L. Jones A. G. Fullea J. &Griffin W. L.(2016).3‐D multiobservable probabilistic inversion for the compositional and thermal structure of the lithosphere and upper mantle: III. Thermochemical tomography in the Western‐Central U.S [Software].Journal of Geophysical Research: Solid Earth 121(10) 7337–7370.https://doi.org/10.1002/2016jb013049 10.1002/2016jb013049
[6]
Afonso J. C. Salajegheh F. Szwillus W. Ebbing J. &Gaina C.(2019).A global reference model of the lithosphere and upper mantle from joint inversion and analysis of multiple data sets[Dataset].Geophysical Journal International 217(3) 1602–1628.https://doi.org/10.1093/gji/ggz094 10.1093/gji/ggz094
[19]
The Composition and Evolution of Lithospheric Mantle: a Re-evaluation and its Tectonic Implications

W. L. Griffin, S. Y. O'Reilly, J. C. Afonso et al.

Journal of Petrology 10.1093/petrology/egn033
[22]
He R. Shang X. Yu C. Zhang H. &Hilst R. D. V. D.(2014).A unified map of Moho depth and Vp/Vs ratio of continental China by receiver function analysis. 10.1093/gji/ggu365
[24]
Lithosphere architecture characterized by crust–mantle decoupling controls the formation of orogenic gold deposits

Zengqian Hou, Quanwei Wang, Haijiang Zhang et al.

National Science Review 10.1093/nsr/nwac257
[27]
Jiang G. Z. Hu S. B. Shi Y. Z. Zhang C. Wang Z. T. &Hu D.(2019).Terrestrial heat flow of continental China: Updated dataset and tectonic implications[Dataset].Tectonophysics 753 36–48.https://doi.org/10.1016/j.tecto.2019.01.006 10.1016/j.tecto.2019.01.006
[32]
Laske G. (2013)
[39]
Ning S. X. &Chen Y. J.(2022).Is there an interconnected lower crustal channel flow beneath southeastern margin of Tibetan plateau?Acta Scientiarum Naturalium Universitatis Pekinensis[Dataset].Zenodo. (in Chinese).https://doi.org/10.5281/zenodo.7644990 10.5281/zenodo.7644990
[48]
Xu C. J. "Preliminary study of block rotation model in North China area using GPS measurements" Geodesy Beyond (2000)

Showing 50 of 63 references

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