Petrogenesis and Oxidation state of chromitites and associated peridotites in the Kudi ophiolite, Western Kunlun Orogen, NW China
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摘要
<正>In western Tibetan plateau,there are five sutures and four terranes between the Tarim block and Himalaya from north to south.Oytag-Kudi ophiolitic belt is the northernmost suture formed from the final closure of the Proto-Tethys with Western Kunlun Terrane connected with Tarim block during middle Silurian.The Kudi ophiolite is well developed and tectonically emplaced onto the Western Kunlun Terrane.It consists
引文
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