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The carbonate‐rich magmatic rocks of West Junggar are distributed in the Baijiantan and Darbut ophiolitic mélanges in the forms of extrusive rocks overlying the mélanges and dykes, either along the margins of the mélange or cross‐cutting components of mélanges. Chilled margin and flow structures are present. A SHRIMP zircon U‐Pb age of 39.7 ± 1.3 Ma indicates that these carbonate‐rich rocks in West...
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