兰州大学

姓名:胡沛青
职称:副教授
所在研究所：岩石圈演化
主要研究方向：岩浆岩石学、矿床学与同位素地球化学方面的研究
研究生招生方向：元素与同位素地球化学，岩浆作用地球化学地球化学与岩石圈演化，流体地球化学
个人简介：女，1972年生，博士，兰州大学资源环境学院副教授， 2007 年至今在兰州大学资源环境学院任教，主要从事岩浆岩石学、矿床学与同位素地球化学方面的研究，主讲课程岩石学(1)-岩浆岩石学、流体地球化学。先后承担完成了国家自然科学基金重点项目“小岩体镍、铜、铂族岩浆硫化物矿床成因的深部过程”(40534020)、面上项目“中国东部不同深度上地幔流体组成特征及示踪”( 40273009)、“祁连古大洋岩石圈地幔流体组成及其地质意义” (40873005) 、“中央高校基本科研业务费专项资金”自由探索项目“新疆北部晚古生代岩浆作用与成矿耦合关系”，发表论文二十余篇，其中SCI收录论文5篇。
 
论文著作：

1、Hu P-Q, Zhang M-J, Tang Z-L et al. 2007. Chemical and stable isotopic compositions of volatiles in mantle peridotites of the Yushigou Ophiolite in Qilian orogenic belt, western China. Acta Petrol. Sino, 23(1): 169-176.
2、Zhang M J, Hu P-Q, Niu Y, Su S-G. Chemical and stable isotopic constraints on the origin and nature of volatiles in sub-continental lithospheric mantle beneath eastern China. Lithos, 2007. 96(1-2): 55-66.
3、Zhang M-J, Niu Y, Hu P-Q. Volatiles in the Mantle Lithosphere: Occurrence Modes and Chemical Compositions. Anderson J E and Coates R W Eds., “The Lithosphere: Geochemistry, Geology and Geophysics” New York: Nova Science Publishers, 2009, Chapter 5, p171-212.
4、Zhang M-J, Kamo S L, Li C, Hu P-Q, Ripley E M. Precise U-Pb zircon-baddeleyite age of the Jinchuan sulfide ore-bearing ultramafic intrusion, western China. Mineralium Deposita, 2009, DOI 10.1007/ s00126-009- 0259-x
5、胡沛青, 张铭杰, 汤庆艳等. 2010. 金川Cu-Ni-PGE硫化物矿床成矿岩浆过程稀有气体同位素组成示踪. 岩石学报, 26(11): 3375-86.
6、胡沛青, 任立业, 傅飘儿等. 2010. 新疆哈密黄山东铜镍硫化物矿床成岩成矿作用. 矿床地质，29(1), 158-168.
7、傅飘儿, 胡沛青*, 张铭杰等. 2009. 新疆黄山铜镍硫化物矿床成因研究.地球化学. 38(5), 432-448.
8、张铭杰, 李延鑫, 胡沛青, 王先彬, Niu Yaoling, 傅飘儿. 中国东部陆下岩石圈地幔中的再循环地壳流体组分.地质学报, 2009, 83(3): 1-13.
9、张铭杰, 王先彬, 胡沛青. 2006. 地幔流体化学组成与成烃.天然气地球科学, 17 (1): 31-35.
10、贾志永, 张铭杰, 汤中立, 李文渊, 任立业, 胡沛青. 2009. 新疆喀拉通克铜镍硫化物矿床成矿岩浆作用过程. 矿床地质, 28(5): 673-686.

会议摘要

Hu P-Q, Zhang M-J, Li C and Tang Z.-L. 2008. Noble gas Isotopic Constrain on Origin of Fluids in Jinchuan Ni-Cu Sulfide Deposit, Northwest China. Geochim. Cosmochim. Acta, 72 (12S): A397.
Zhang M-J, Hu P-Q, Li L-W et al. 2006. The volatile compositions of Qilian ancient oceanic lithosphere: Evidences from peridotites in Yushigou ophiolite, west China. Geochim. Cosmochim. Acta, 70: 736. doi:10.1016/ j.gca.2006.06.1325
Zhang M-J Hu P-Q, Zheng Peng et al. The Occurrence modes of H2 in mantle-derived rocks, In: Mao J, Bierlein F P eds, Mineral Deposit Research, Chapter1-19. New York: Springer, 2005. p. 73-76.
Hu P-Q, Li C, Tang Q-Y, Fu P-E, Zhang M-J, Ripley E M. 2010. The Permian Huangshanxi Cu-Ni deposit in western China: Magma evolution and ore genesis. 11th International Platinum Symposium. Ontario, Canada, p21-24.
Hu P-Q, Zhang M-J, Wang J-Z et al. 2006. The volatile compositions of peridotite in Yushigou ophiolite from Qilian orogenic belt. ACROFII, p75-76.
Zhang M-J, Hu P-Q, Niu Y-L .2006. The volatiles in the thinning of sub-continental lithospheric mantle beneath eastern China. Eos Trans. AGU, 87(36), V31A-0191.
Zhang M-J, Hu P-Q, Wang X- B et al. 2005. The fluid compositions of lherzolite xenoliths in Eastern China and Western American. Geochim. Cosmochim. Acta, 69A: 146.