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Late Archean to early proterozoic lithospheric mantle beneath the western North China craton: Sr-Nd-Os isotopes of peridotite xenoliths from Yangyuan and Fansi 期刊论文
Lithos, 2008, 卷号: 102, 期号: 1-2, 页码: 25-42
Authors:  Xu YG;  Blusztajn J;  Ma JL;  Suzuki K;  Liu JF;  Hart SR
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青藏高原东南木里地区二叠纪苦橄岩的Os-Sr-Nd同位素地球化学研究 期刊论文
岩石学报, 2008, 卷号: 24, 期号: 2, 页码: 337-347
Authors:  李杰;  许继峰;  何斌;  徐义刚;  董彦辉
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Integration of geology, geophysics and geochemistry: A key to understanding the North China Craton 期刊论文
Lithos, 2007, 卷号: 96, 期号: 1-2, 页码: 1-21
Authors:  Menzies M;  Xu YG;  Zhang HF;  Fan WM
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Diachronous lithospheric thinning of the North China Craton and formation of the Daxin'anling-Taihangshan gravity lineament 期刊论文
Lithos, 2007, 卷号: 96, 期号: 1-2, 页码: 281-298
Authors:  Xu YG
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Age and duration of the Emeishan flood volcanism, SW China: Geochemistry and SHRIMP zircon U-Pb dating of silicic ignimbrites, post-volcanic Xuanwei Formation and clay tuff at the Chaotian section 期刊论文
Earth and Planetary Science Letters, 2007, 卷号: 255, 期号: 3-4, 页码: 306-323
Authors:  He B;  Xu YG;  Huang XL;  Luo ZY;  Shi YR;  Yang QJ;  Yu SY
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吉林伊通－大屯地区晚中生代－新生代玄武岩的地球化学特征及其意义 期刊论文
岩石学报, 2006, 卷号: 22, 期号: 6, 页码: 1579-1596
Authors:  张辉煌;  徐义刚;  葛文春;  马金龙
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Old EMI-type enriched mantle under the middle North China Craton as indicated by Sr and Nd isotopes of mantle xenoliths from Yangyuan, Hebei Province 期刊论文
Chinese Science Bulletin, 2006, 卷号: 51, 期号: 11, 页码: 1343-1349
Authors:  Ma JL;  Xu YG
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滇西莴中新生代高镁钾火山岩中橄榄石斑晶及其尖晶石包裹体的岩浆成因动力学意义 期刊论文
岩石学报, 2006, 卷号: 22, 期号: 6, 页码: 1553-1564
Authors:  黄小龙;  徐义刚;  杨启军;  陈林丽
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Role of lithosphere-asthenosphere interaction in the genesis of Quaternary alkali and tholeiitic basalts from Datong, western North China Craton 期刊论文
Chemical Geology, 2005, 卷号: 224, 期号: 4, 页码: 247-271
Authors:  Xu YG;  Ma JL;  Frey FA;  Feigenson MD;  Liu JF
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Re-Os isotopes in mantle-derived pyroxenite xenoliths from Hannuoba North China 会议论文
14th Annual V M Goldschmidt Conference, Copenhagen, DENMARK, 2004-6-5
Authors:  Zhi XC;  Meng Q;  Xia QX;  Zheng L;  Xu YG
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