Petrogenesis and tectonic implications of the Early Carboniferous to the Late Permian Barleik plutons in the West Junggar (NW China)
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文摘
The Barleik plutons are Early Carboniferous to Late Permian in age. They were produced by fractionation of a mantle-derived parental magma. The Junggar Ocean was closed prior to the earliest Late Carboniferous.

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