扫描手机二维码
的个人主页 http://faculty.cumt.edu.cn/HSJ1/zh_CN/index.htm
上一条: 新疆准噶尔盆地北部石炭系穿时的火山岩——沉积序列与克拉麦里洋盆闭合模式
下一条: Geochemistry, Petrology, and U-Pb dating of high-K volcanic rocks in wells WC-1 and Y-2 from the northern Junggar Basin, northwestern China: Implications for the closure of the Keramaili oceanic basin during the Carboniferous