It is regarded that the magmatic activity is end in Upper Hercynides and become stable platform in Mesozoic era in the Shanshan county, Xinjiang province, China.
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众多地质工作者认为,新疆鄯善县恰舒阿山一带的岩浆活动终止于海西晚期,中生代后进入稳定的地台盖层发展阶段。
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