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    Snowflake-like sixfold angle-dependent magnetoresistance in the kagome antiferromagnet Gd3TiBi5

    Ruwen Wang1,2,*, Zhen Zhao1,*, Xinwei Yi3,*, Yuhang Zhang1, Ke Zhu1, Haisen Liu1, Senhao Lv1, Chenyu Bai1,2, Gang Cao1 et al.

    Lihong Bao1,2, Hui Guo1,2, Guojing Hu1,2, Xiaoli Dong1,2,4, Xiao Lin2, Haitao Yang1,2,4,†, and Hong-Jun Gao1,2,4,‡

    • *These authors contributed equally to this work.
    • †Contact author: htyang@iphy.ac.cn
    • ‡Contact author: hjgao@iphy.ac.cn

    Phys. Rev. B 114, 034417 – Published 16 July, 2026

    DOI: https://doi.org/10.1103/rjqd-185g

    Abstract

    Kagome magnets provide fertile platforms for field-tunable magnetic phases, electronic correlations, and quantum phenomena. However, the in-plane anisotropy within the kagome layers remains largely unexplored. Here we report the synthesis of Gd3TiBi5 single crystals featuring distorted Gd kagome layers, which exhibit an antiferromagnetic transition at TN≈19K and a pronounced in-plane anisotropic magnetization. The magnetic phase diagrams display successive field-driven magnetic phases separated by well-defined, anisotropic phase boundaries, indicating complex reorientation processes of Gd3+ moments under external magnetic fields. Notably, the in-plane angle-dependent magnetoresistance (ADMR) measurements uncover a snowflake-like ADMR pattern at low temperatures and under high magnetic fields, characterized by a pronounced sixfold symmetry with narrowed central spikes and additional shoulder-like modulations along each lobe. The sixfold ADMR is primarily attributed to the in-plane anisotropic magnetic transitions, highlighting the coupling between localized Gd−4f moments and itinerant electrons. DFT calculations further suggest that rotating the magnetic moment direction can drive a van Hove singularity across the Fermi level, potentially inducing a spin-orientation-dependent Fermi-surface reconstruction. These results establish Gd3TiBi5 as a promising platform for studying the interplay between frustrated magnetism and electrical transport and provide a useful framework for understanding magnetism-driven anisotropic transport.

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