The Paleotethyan tectonic history of northeast Tibet remains hotly debated, particularly regarding the nature of the Jinsha suture. Different interpretations of the Jinsha suture lead to different tectonic reconstructions of northeast Tibet, southern Eurasian continent. We identified three tectonic units along the western segment of the Jinsha suture in the Yushu–Zhiduo region: the Bayan Har–Songpan–Garzê fold belt (BSB), the Yushu mélange, and the eastern portion of the Qiangtang block (EQ). New geochemical and geochronological studies help to identify a Triassic continental magmatic arc (the Yushu arc) that developed upon the EQ and that is geochemically similar to magmatism in the Yidun arc. Structural studies, combined with 40Ar/39Ar analyses, reveal a complex deformational history of the Yushu–Zhiduo region: earlier‐stage top‐to‐the‐north asymmetrical fabrics are preserved exclusively in the Yushu mélange, which yields a phengite 40Ar/39Ar age of 230.5 ± 0.8 Ma; later‐stage orthogonal fabrics developed in the BSB and EQ (superposed upon the earlier fabrics in the Yushu mélange), likely resulted from a collision between the BSB and the Yushu arc that continued until ∼195 Ma. The structural patterns and deformation history of Yushu arc region are comparable with those recorded in the Yidun arc region. Thus, the previously defined Jinsha suture should be subdivided into western and southern segments. The western Jinsha suture is continuous with the Garzê‐Litang suture, while the southern Jinsha‐Ailaoshan suture marks the site of the closure of several intracontinental rift basins that have likely been overprinted by intra or back‐arc extension.

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