1.基本信息：

姓名： 汤庆艳 职称：教授
通讯地址：甘肃省兰州市城关区天水南路222号
电子邮箱 ：tangqy@lzu.edu.cn
Prof. Dr. Qingyan Tang
222 South Tianshui Road, Lanzhou
730000, Gansu Province
CHINA
Email: tangqy@lzu.edu.cn
2.教育经历

2010.09-2013.12: 兰州大学地质科学与矿产资源学院, 博士学位，专业：矿物学、岩石学、矿床学。
2012.10-2013.10：美国印第安纳大学，国家联合培养博士研究生。
2007.09-2010.06：兰州大学资源环境学院，硕士学位，专业：构造地质学。
2003.09-2007.06：兰州大学资源环境学院，学士学位，专业：地球化学。
EDUCATION
B.S., 2007, Lanzhou University, China
M.S., 2010, Lanzhou University, China
Ph.D., 2013, Lanzhou University, China
3.工作经历
2015年5月至今，副教授，兰州大学地质科学与矿产资源学院
2014年3月至2015年5月，讲师，兰州大学地质科学与矿产资源学院
PROFESSIONAL EXPERIENCE
2014.3-2015.5, Lecturer, Lanzhou University, Lanzhou, China
2015.5- , Associate professor, Lanzhou University, Lanzhou, China
4.研究方向
岩石圈演化与岩浆作用成矿
RESEARCH INTERESTS
Lithosphere evolution, and mineralization related to magmatism
5.教学、指导/科研项目
教学：地球化学、岩浆岩石学课程
指导：硕士研究生3名
科研项目：主持国家自然科学基金面上项目(**)1项, 起止时间：2015-2018.
TEACHING & SUPERVISION/RESEARCH PROJECTS
Courses：Geochemistry, Magmatic petrology
SUPERVISION：Three master degree candidates
RESEARCH PROJECTS：the National Natural Science Foundation of China (**)，PI,2015-2018 .
6.代表性论著
[1] Tang Q, et al. Association of Mg-rich olivine with magnetite as a Result of brucite marble assimilation by basaltic magma in the Emeishan Large Igneous Province, SW China. Journal of Petrology, 2017, 58: 69-74.
[2] Tang Q, et al. The origin of the Zhubu mafic-ultramafic intrusion of the Emeishan large igneous province, SW China. Chemical Geology, 2017, 469: 47-59.
[3] Tang Q, et al. Neoproterozoic subduction-related basaltic magmatism in the northern margin of the Tarim Craton. Precambrian Research, 2016, 286: 370–378.
[4] Tang Q, et al. Detrital zircon constraint on the timing of amalgamation between Alxa and Ordos, with exploration implications for Jinchuan-type Ni–Cu ore deposit in China. Precambrian Research. 2014, 255: 748–755.
[5] Tang Q, et al. The chemical compositions and abundances of volatiles in the Siberian large igneous province: Constraints on magmatic CO2 and SO2 emissions into the atmosphere. Chemical Geology, 2013, 339: 84–91.
[6] Tang Q, et al. The origin of Ni-Cu-PGE sulfide mineralization in the margin of the Zhubu mafic-ultramafic intrusion in the Emeishan large igneous province, SW China. Economic Geology, 2013, 108: 1889–1901.
SELECTED PUBLICATIONS (inverted order)
[1] Tang Q, et al. Association of Mg-rich olivine with magnetite as a Result of brucite marble assimilation by basaltic magma in the Emeishan Large Igneous Province, SW China. Journal of Petrology, 2017, 58: 69-74.
[2] Tang Q, et al. The origin of the Zhubu mafic-ultramafic intrusion of the Emeishan large igneous province, SW China. Chemical Geology, 2017, 469: 47-59.
[3] Tang Q, et al. Neoproterozoic subduction-related basaltic magmatism in the northern margin of the Tarim Craton. Precambrian Research, 2016, 286: 370–378.
[4] Tang Q, et al. Detrital zircon constraint on the timing of amalgamation between Alxa and Ordos, with exploration implications for Jinchuan-type Ni–Cu ore deposit in China. Precambrian Research, 2014, 255: 748–755.
[5] Tang Q, et al. The chemical compositions and abundances of volatiles in the Siberian large igneous province: Constraints on magmatic CO2 and SO2 emissions into the atmosphere. Chemical Geology, 2013, 339: 84–91.
[6] Tang Q, et al. The origin of Ni-Cu-PGE sulfide mineralization in the margin of the Zhubu mafic-ultramafic intrusion in the Emeishan large igneous province, SW China. Economic Geology, 2013, 108: 1889–1901.