Structural elements and evolution of the Yangmuchuan dome: Constraints on the tectonics of the Paleoproterozoic Jiao-Liao-Ji belt in the Eastern Block of the North China Craton

• Published in: Precambrian research Vol. 372; p. 106581
• Main Authors: Zhao, Lifu, Zhang, Jian, Yang, Chengwei, Chen, Xiaoyu, Liu, Junlai
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.05.2022
• Subjects: Crustal mass flow; Jiao-Liao-Ji Orogenic Belt; North China Craton; Structural analysis; Yangmuchuan dome; Jiao-Liao-Ji Orogenic Belt; Yangmuchuan dome; Crustal mass flow; North China Craton; Structural analysis
• ISSN: 0301-9268; 1872-7433
• DOI: 10.1016/j.precamres.2022.106581

[Display omitted] •Deformation in the Yangmuchuan gneiss dome can be divided into two deformation stages (D1 and D2).•Dating the syn-tectonic granitic dykes constrain the timing of D2 deformation from >1887 to 1808 Ma.•The Yangmuchuan gneiss dome was formed as the result of dominant subhorizontal middle to lower flow. The nature of assembly of the Columbia supercontinent is well-characterized by the orogenic belts that were formed during amalgamation of continental blocks. The Jiao-Liao-Ji Belt (JLJB) in the eastern North China Craton possesses complex deformation structures that exemplify the Paleoproterozoic orogeny. A series of granitic gneiss domes in the southern JLJB characterizes the structural deformation in the Paleoproterozoic orogenic belts. Located in the middle segment of the JLJB, the Yangmuchuan dome is composed of three major elements, i.e., the Liaoji granites in the core, and sheared metamorphic rocks in the mantle and outer shell. Bedding-parallel ductile shear zones and weakly deformed metamorphic rocks between them are well-preserved in the latter two elements. Structural analysis reveals that the Yangmuchuan dome mainly experienced two deformation stages (D1 and D2). The D1 deformation is characterized by pure shear-dominated deformation structures with occurrence of penetrative foliations, symmetrical boudinages, mineral lineations and rootless folds in all the rocks from the mantle and outer shell. Dominated by simple shearing, the D2 deformation is the key stage contributing to the formation of the dome structure in the area. The D2 deformation is manifested as occurrence of A-type folds, S-C fabrics, mylonitic foliation S2, mineral stretching lineation L2 in granites, and in layered rocks in the mantle and outer shell. They were superposed on and transformed, along high strain zones, D1 deformation structures. Magnetic fabrics of the Liaoji granites from the core show a generally consistent orientation with the foliations and stretching lineations in the sheared granites. LA-ICP-MS zircon U-Pb dating on syn-tectonic leucogranitic dykes indicates that the peak deformation (D2) of the Yangmuchuan dome occurred from >1887 to 1808 Ma. Geometrical and kinematic analysis from the structural, microstructural and magnetic fabric data reveal that formation of the Yangmuchuang gneiss dome resulted from dominant subhorizontal flow and subsidiary vertical flow in the middle and lower crust as the consequence of orogenic activity along the JLJB during the assembly of the Columbia supercontinent.