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The Bikou basalts in the northwestern Yangtze block, South China: Remnants of 820-810 Ma continental flood basalts? 期刊论文
Geological Society of America Bulletin, 2008, 卷号: 120, 期号: 11-12, 页码: 1478-1492
Authors:  Wang XC;  Li XH;  Li WX;  Li ZX;  Liu Y;  Yang YH;  Liang XR;  Tu XL
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Detrital zircon evidence from Burma for reorganization of the eastern Himalayan river system 期刊论文
American Journal of Science, 2008, 卷号: 308, 期号: 4, 页码: 618-638
Authors:  Liang YH;  Chung SL;  Liu DY;  Xu YG;  Wu FY;  Yang JH;  Wang Y;  Lo CH
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Kinetics of hydrocarbon generation for Well Yingnan 2 gas reservoir, Tarim Basin, China 期刊论文
Science in China Series D-Earth Sciences, 2008, 卷号: 51, 期号: S1, 页码: 107-114
Authors:  Xiao ZY;  Xiao XM;  Ma DM;  Lu YH;  Yang CS
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Kinetic parameters of methane generated from source rocks in the Kuqa depression of Tarim Basin and their application 期刊论文
Acta Geologica Sinica, 2008, 卷号: 82, 期号: 1, 页码: 154-163
Authors:  Li XQ;  Xiao XF;  Mi JK;  Tang YH;  Xiao ZY;  Liu D;  Shen JG;  Yang YF;  Wang Y;  Dong P
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桂东南大容山－十万大山S型花岗岩带的成因：地球化学及Sr-Nd-Hf同位素制约 期刊论文
岩石学报, 2007, 卷号: 23, 期号: 2, 页码: 403-412
Authors:  祁昌实;  邓希光;  李武显;  李献华;  杨岳衡;  谢烈文
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地质样品的一次阴离子色谱法Hf分离及其MC-ICP-MS分析 期刊论文
岩石学报, 2007, 卷号: 23, 期号: 2, 页码: 227-232
Authors:  杨岳衡;  张宏福;  刘颖;  谢烈文;  祁昌实;  涂湘林
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同一岩石试样的Lu-Hf和Sm-Nd快速分离及国家岩石标准物质的Hf-Nd同位素比值精确测定 期刊论文
岩石学报, 2007, 卷号: 23, 期号: 2, 页码: 221-226
Authors:  李献华;  刘颖;  杨岳衡;  陈福坤;  涂湘林;  祁昌实
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华北克拉通中、新生代典型火山岩的岩石成因：Hf同位素新证据 期刊论文
岩石学报, 2006, 卷号: 22, 期号: 6, 页码: 1665-1671
Authors:  杨岳衡;  张宏福;  谢烈文;  刘颖;  祁昌实;  涂湘林
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Petrogenesis of the Neoproterozoic bimodal volcanic rocks along the western margin of the Yangtze Block: New constraints from Hf isotopes and Fe/Mn ratios 期刊论文
Chinese Science Bulletin, 2005, 卷号: 50, 期号: 21, 页码: 2481-2486
Authors:  Li XH;  Qi CS;  Liu Y;  Liang XR;  Tu XL;  Xie LW;  Yang YH
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Distribution of natural and anthropogenic thallium in the soils in an industrial pyrite slag disposing area 期刊论文
Science of the Total Environment, 2005, 卷号: 341, 期号: 1-3, 页码: 159-172
Authors:  Yang CX;  Chen YH;  Peng P;  Li C;  Chang XY;  Xie CS
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