Deng Y, Lang X, Klemd R, Wang X, Tang J, He Q, Zhou Y, Zuo Y, Tang X, Zunzhu S (2025)
Publication Type: Journal article
Publication year: 2025
Book Volume: 494-495
Article Number: 107933
DOI: 10.1016/j.lithos.2024.107933
Geophysical and geochemical evidence confirmed the northward-directed Indian continental lithosphere subduction beneath the Gangdese orogen, however, the geodynamic processes responsible for the transition from the Neo-Tethyan subduction to the Indian continental subduction, particularly magma generation mechanisms regarding the 53–42 Ma magmatic flare-up events, remain poorly constrained. Here we have conducted a comprehensive investigation combining geochemical and geochronological studies of newly discovered Early Eocene (ca. 50–47 Ma) ultrapotassic–potassic lamprophyre dikes in the Lhasa terrane, Tibet. The ultrapotassic lamprophyres revealed highly evolved Sr–Nd–Pb isotopes and high concentrations of incompatible elements, and are thought to have originated from the Indian lithospheric mantle. In contrast, the potassic lamprophyres, displaying relatively depleted Sr–Nd–Pb isotopes and lower MgO contents and K
APA:
Deng, Y., Lang, X., Klemd, R., Wang, X., Tang, J., He, Q.,... Zunzhu, S. (2025). New magmatic record of Indian continental subduction at ca. 50 Ma: Evidence from ultrapotassic–potassic lamprophyre dikes in the Gangdese Batholith, Southern Tibet. Lithos, 494-495. https://doi.org/10.1016/j.lithos.2024.107933
MLA:
Deng, Yulin, et al. "New magmatic record of Indian continental subduction at ca. 50 Ma: Evidence from ultrapotassic–potassic lamprophyre dikes in the Gangdese Batholith, Southern Tibet." Lithos 494-495 (2025).
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