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We present the whole rock and the mineral chemical data for upper mantle peridotites from the San‐Jiang region in Yunnan, SW China. These peridotites are a part of a Paleo‐Tethyan ophiolite belt occurring along the Jinshajiang and Lancangjiang suture zones. All samples of the Jinshajiang and Lancangjiang ultramafic rocks are completely serpentinized. The Jinshajiang serpentinites are characterized...