华北东部中生代高Mg<sup>#</sup>闪长岩与壳幔相互作用

辛梦荷; 汪浪; 刘传朋; 汪翔; 郑怡欣; 宗克清; 郭京梁; 汪在聪

doi:10.3799/dqkx.2025.195

Volume 51 Issue 2

Feb. 2026

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Article Navigation > Earth Science > 2026 > 51(2): 527-546

Xin Menghe, Wang Lang, Liu Chuanpeng, Wang Xiang, Zheng Yixin, Zong Keqing, Guo Jingliang, Wang Zaicong, 2026. North China Eastern Mesozoic High Mg# Diorites and Crust⁃Mantle Interaction. Earth Science, 51(2): 527-546. doi: 10.3799/dqkx.2025.195

Citation:

Xin Menghe, Wang Lang, Liu Chuanpeng, Wang Xiang, Zheng Yixin, Zong Keqing, Guo Jingliang, Wang Zaicong, 2026. North China Eastern Mesozoic High Mg^# Diorites and Crust⁃Mantle Interaction. Earth Science, 51(2): 527-546. doi: 10.3799/dqkx.2025.195

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North China Eastern Mesozoic High Mg^# Diorites and Crust⁃Mantle Interaction

doi: 10.3799/dqkx.2025.195

1.
State Key Laboratory of Geological Processes and Mineral Resources, School of Earth and Planetary Sciences, China University of Geosciences, Wuhan 430074, China
2.
Shandong Provincial Bureau of Geology and Mineral Resources No.5 Geological Brigade(No.5 Institute of Geology and Mineral Exploration of Shandong Province), Taian 271000, China

Received Date: 2025-08-23
Publish Date: 2026-02-25

Abstract

Abstract

Intense cratonic destruction occurred in the eastern part of the North China Craton(NCC) during the Mesozoic, accompanied by tectonic⁃magmatic⁃metallogenic activities. During the peak period of destruction, high Mg^# diorites related to the coeval Fe⁃Cu⁃Au deposits were widely distributed in regions like Luxi⁃Xuhuai⁃Dabie. Although there have been many studies on the genesis of rocks, the connection between the spatial distributions of high Mg^# diorites and the evolution of the lithosphere still lacks systematic understanding. This paper selects the eastern part of the NCC as the study area. It comprehensively sorts out and summarizes the petrography, temporal and spatial distribution patterns, and Sr⁃Nd⁃Pb isotopic characteristics of high Mg^# diorites, establishes the vertical connection on a large regional scale, and explores the evolution process of the lithosphere in the crust⁃mantle interaction, providing an important basis for magmatic and mineralization processes as well as spatial differences. These high Mg^# diorites have consistent island arc⁃like trace element characteristics and enriched Sr⁃Nd isotope compositions, indicating the existence of recycled crustal materials in the source region. Moreover, there are significant spatial variations in the Sr⁃Nd⁃Pb isotopes: from south to north, the (⁸⁷Sr/⁸⁶Sr)_i of diorites gradually decreased (0.711 7~0.704 3), and the ε_Nd(t) gradually increased (-24.90~-1.77), indicating a trend of decreasing influence of crustal materials on the mantle from south to north, which supports the influence of the subduction of the Yangtze continental Plate during the Triassic on the lithospheric mantle beneath the NCC. On the other hand, the low (⁸⁷Sr/⁸⁶Sr)_i diorites have low (²⁰⁷Pb/²⁰⁴Pb)_i and (²⁰⁸Pb/²⁰⁴Pb)_i like those of the ancient metamorphic basement of the NCC, indicating that there are also ancient NCC crustal materials in the source, which may be related to the lower crust delamination. Therefore, the high Mg^# diorites reflect that the degree of modification of the lithospheric mantle from south to north by recycled materials (Yangtze crust) gradually weakens, accompanied by the crustal delamination beneath the eastern NCC, and the relative contributions of the subducting Yangtze crust and the NCC ancient crust. This also promotes a better understanding of the formation and evolution of high Mg^# diorites, as well as the types and distribution patterns of deposits.
- NCC,
- high-Mg^# diorite,
- Mesozoic,
- crust-mantle interaction,
- mineralization

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References(131)

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North China Eastern Mesozoic High Mg# Diorites and Crust⁃Mantle Interaction

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North China Eastern Mesozoic High Mg^# Diorites and Crust⁃Mantle Interaction