| Origin of K-bentonites in the Doushantuo cap dolostones from South China and its potential link with the sedimentary model of the Marinoan cap dolostones | |
Mingzhong Zhou; Bin Wan; Li Zhou; Enlin Yang; Liansheng Yang; Taiyi Luo
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| 2021 | |
| Source Publication | Precambrian Research
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| Volume | 366Pages:106416 |
| Abstract |
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| DOI | 10.1016/j.precamres.2021.106416 |
| URL | 查看原文 |
| Indexed By | SCI |
| Language | 英语 |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.gyig.ac.cn/handle/42920512-1/12129 |
| Collection | 矿床地球化学国家重点实验室 |
| Affiliation | 1.School of Geographical and Environmental Sciences, Guizhou Normal University, Guiyang 550001, China 2.State Key Laboratory Incubation Base for Karst Mountain Ecology Environment of Guizhou Province, Guiyang 550001, China 3.State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China 4.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China |
| Recommended Citation GB/T 7714 | Mingzhong Zhou,Bin Wan,Li Zhou,et al. Origin of K-bentonites in the Doushantuo cap dolostones from South China and its potential link with the sedimentary model of the Marinoan cap dolostones[J]. Precambrian Research,2021,366:106416. |
| APA | Mingzhong Zhou,Bin Wan,Li Zhou,Enlin Yang,Liansheng Yang,&Taiyi Luo.(2021).Origin of K-bentonites in the Doushantuo cap dolostones from South China and its potential link with the sedimentary model of the Marinoan cap dolostones.Precambrian Research,366,106416. |
| MLA | Mingzhong Zhou,et al."Origin of K-bentonites in the Doushantuo cap dolostones from South China and its potential link with the sedimentary model of the Marinoan cap dolostones".Precambrian Research 366(2021):106416. |
| Files in This Item: | ||||||
| File Name/Size | DocType | Version | Access | License | ||
| Origin of K-bentonit（8459KB） | 期刊论文 | 作者接受稿 | 开放获取 | CC BY-NC-SA | View Application Full Text | |
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