Based on the results of Geotransect from Dushanzi to Quanshuigou, the crustal structure and tectonics along the profile from Quanshuigou to Altai of Xinjiang were carried out.
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摘要以新疆独山子-泉水沟地学断面的资料为主,讨论了泉水沟-阿勒泰剖面的地壳结构主要特征。
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