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塔里木盆地奥陶系碳酸盐岩热液蚀变类型及蚀变流体的分带特征 |
丁茜1,2, 胡秀芳2,3, 高奇东2,4, 叶瑛2, 张平萍2 |
1.中国石化石油勘探开发研究院,北京 100083 2.浙江大学 海洋学院,浙江 舟山 316021 3.中国石油大学,北京 102249 4.中国石化胜利油田,山东 东营 257001 |
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The hydrothermal alteration types and zoning features of Ordovician carbonate in Tarim Basin. |
DING Qian1,2, HU Xiufang2,3, GAO Qidong2,4, YE Ying2, ZHANG Pingping2 |
1.Exploration & Production Research Institute, SINOPEC, Beijing 100083, China 2.Ocean College, Zhejiang University, Zhoushan 316021, Zhejiang Province, China 3.China University of Petroleum(Beijing), Beijing 102249, China 4.Shengli Oilfield, SINOPEC, Dongying 257001, Shandong Province, China |
引用本文:
丁茜, 胡秀芳, 高奇东, 叶瑛, 张平萍. 塔里木盆地奥陶系碳酸盐岩热液蚀变类型及蚀变流体的分带特征[J]. 浙江大学学报(理学版), 2019, 46(5): 600-609.
DING Qian, HU Xiufang, GAO Qidong, YE Ying, ZHANG Pingping. The hydrothermal alteration types and zoning features of Ordovician carbonate in Tarim Basin.. Journal of ZheJIang University(Science Edition), 2019, 46(5): 600-609.
链接本文:
https://www.zjujournals.com/sci/CN/10.3785/j.issn.1008-9497.2019.05.013
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https://www.zjujournals.com/sci/CN/Y2019/V46/I5/600
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