Abstract Detecting strike-slip tectonics using thermochronology is challenging because the complex relative motion between fault blocks often does not substantially displace the vertical stratigraphy provided by thermochronological ages. Here we investigate the strike-slip tectonics in the Yangtze Block. South China. based on an original conceptual model and the zircon (U-Th)/He (ZHe)... https://www.opheliasmuse.com/