Volume 32 Issue 2
Apr.  2026
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Article Navigation >  Journal of Geomechanics  > 2026  >  32(2): 1-27
WANG D M，HU J M，ZHAO Y F，et al.，2026. Composition, tectonic framework, and evolution of the Luxi Orogenic Belt in the North China Craton during the Late Neoarchean[J]. Journal of Geomechanics，32（2）：1−27 doi: 10.12090/j.issn.1006-6616.2025033
Citation: WANG D M，HU J M，ZHAO Y F，et al.，2026. Composition, tectonic framework, and evolution of the Luxi Orogenic Belt in the North China Craton during the Late Neoarchean[J]. Journal of Geomechanics，32（2）：1−27 doi: 10.12090/j.issn.1006-6616.2025033
shu

Composition, tectonic framework, and evolution of the Luxi Orogenic Belt in the North China Craton during the Late Neoarchean

doi: 10.12090/j.issn.1006-6616.2025033
  • 1.

    Longyan University, Longyan 364012, Fujian, China

  • 2.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 3.

    National Earthquake Response Support Service, Beijing 100049, China

  • 4.

    Shandong Institute of Geological Survey, Ji'nan 250013, Shandong, China

Funds:  This research was financially supported by the National Natural Science Foundation of China (Grant Nos. 41872225, 4197021373, and 42302260), and the Natural Science Foundation of Fujian Province (Grant Nos. 2023J01962 and 2024J01848).
More Information
  • Received: 2025-03-28
  • Revised: 2025-09-04
  • Accepted: 2025-09-04
    • Available Online: 2025-09-04
  • Published: 2026-04-28
    Abstract
  •   Objective  The growth and evolution of the early Earth’s crust are hot topics in Precambrian research. As one of the oldest cratons in the world, the North China Craton (NCC) has undergone a complex cratonization process accompanied by crustal growth and reworking.   Methods  Existing petrological, geochemical, chronological, and structural geological studies are summarized to reveal the tectonic evolution of the Luxi granite–greenstone belt in the eastern NCC.   Results  Multiple lines of evidence indicate late Neoarchean crustal growth, including continental arc and arc magmatic rocks represented by the Feicheng‒Tengzhou magmatic arc and late Neoarchean volcanic rocks, post-collisional crustal-derived magmatism represented by the Lushan‒Yishui magmatic belt, sedimentation in a back-arc basin defined by late Neoarchean metamorphic sedimentary rocks, and the strike-slip shear deformation caused by the oblique convergence of plates. The >2.60 Ga tonalite, trondhjemite, granodiorite (TTG) suite and the supracrustal rock belt exposed in the central part of the Luxi area represent an ancient microcontinent with apparent affinity to the Jiaoliao Block.  Conclusions  Therefore, the Luxi granite–greenstone belt is an accretionary orogenic belt located on the western margin of the Jiaoliao Block, namely the Luxi Orogenic Belt. High-angle oblique arc-continent collision and underplating of large volumes of mantle-derived magma represent two crustal growth modes in horizontal and vertical directions, respectively. This orogenic belt has undergone multi-stage evolution, including the formation of initial oceanic crust, subduction, and intracontinental extension from the Neoarchean to the end of the Paleoproterozoic. [Significance] In the late Neoarchean, extensive crustal growth occurred around the Jiaoliao Block in the eastern NCC, which was controlled by an early plate tectonic regime characterized by hot subduction.

     

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