SHRIMP Dating of the Qiqijianake Ophiolitic Mélange in the Kokshai Region, Southwestern Tianshan and Its Tectonic Implications
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line-height-rule: exactly" class=MsoNormal>In this paper, the authors report the SHRIMP U-Pb zircon data for basalt from the Qiqijianake ophiolitic mélange. It shows that the Qiqijianake ophiolitic mélange formed in the Early Devonian (399±4) Ma. In combination with previously published data, the authors infer that the Qiqijianake ophiolitic mélange and Jigen ophiolitic remnant are the extention of South Tianshan ophiolite zone in central Asia, which may be the product of a narrow archipelagic ocean. It represents the suture of the northward subduction of South Tianshan Ocean and collision between the Tarim Plate and Kazakhstan-Junggar Plate occurred after the subduction.

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