GIG OpenIR  > 中国科学院边缘海与大洋地质重点实验室  > 期刊论文
张文进; 王钦贤; 陈多福
西藏岗巴地区晚白垩世冷泉碳酸盐岩地球化学特征及其对流体来源及沉积环境的示踪
Source Publication地球化学
ISSN0379-1726
2018
Volume47Issue:02Pages:217-227
Indexed ByCSCD
Language中文
CSCD IDCSCD:6195645
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Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/36429
Collection中国科学院边缘海与大洋地质重点实验室_期刊论文
Recommended Citation
GB/T 7714
张文进,王钦贤,陈多福. 西藏岗巴地区晚白垩世冷泉碳酸盐岩地球化学特征及其对流体来源及沉积环境的示踪[J]. 地球化学,2018,47(02):217-227.
APA 张文进,王钦贤,&陈多福.(2018).西藏岗巴地区晚白垩世冷泉碳酸盐岩地球化学特征及其对流体来源及沉积环境的示踪.地球化学,47(02),217-227.
MLA 张文进,et al."西藏岗巴地区晚白垩世冷泉碳酸盐岩地球化学特征及其对流体来源及沉积环境的示踪".地球化学 47.02(2018):217-227.
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