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The Wajilitag layered mafic–ultramafic intrusion, as an important lithological unit of the Permian Tarim large igneous province, has genetic link with a large scale V-bearing ilmenite–titanomagnetite series mineralization. It consists mainly of olivine pyroxenite, pyroxenite and gabbro with layered structures. Olivine from the mafic–ultramafic rocks has low Fo values [molar 100×Mg/(Mg+Fe)] of 67–76mol%,...
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