| DOI | 10.3390/min11020096
|
| Sr, S, and O Isotope Compositions of Evaporites in the Lanping-Simao Basin, China |
| Shen, Lijian; Wang, Licheng; Liu, Chenglin; Zhao, Yanjun
|
| 通讯作者 | Wang, LC (通讯作者)
|
| 发表日期 | 2021
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| EISSN | 2075-163X
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| 卷号 | 11期号:2 |
| 英文摘要 | Evaporites are widely distributed within continental red beds in the Lanping-Simao Basin, west Yunnan, China. Sr (Strontium), S (Sulfur), and O (Oxygen) isotope compositions have been measured on 54 sulfate or/and sulfate-bearing samples collected from Lanping, Nuodeng, Jinggu, Mengyejing, Baozang throughout the Lanping-Simao Basin. The Sr-87/Sr-86 ratios of all samples (0.708081 to 0.710049) are higher than those of contemporaneous seawater, indicating a significant continental contribution to the drainage basin. Sulfates in the Lanping Basin have higher Sr-87/Sr-86 ratios (0.709406 to 0.710049) than those (0.708081 to 0.709548) in the Simao Basin. Nevertheless, the delta S-34 values of gypsums (13.4 parts per thousand to 17.6 parts per thousand) in Lanping and Baozang fall within the range of Cretaceous seawater. Gypsums from a single section in Baozang have trends of decreasing delta S-34 values and increasing Sr-87/Sr-86 ratios from base to top, indicating continental input played an increasingly significant role with the evaporation of brines. High delta S-34 values (20.5 parts per thousand to 20.7 parts per thousand) of celestites in Lanping are probably caused by bacterial sulfate reduction (BSR) process in which S-34 were enriched in residual sulfates and/or recycling of Triassic evaporites. The reduced delta S-34 values of gypsums (9.5 parts per thousand to 10.4 parts per thousand) in Nuodeng could have been caused by oxidation of sulfides weathered from Jinding Pb-Zn deposit. The complex O isotope compositions indicate that sulfates in the Lanping-Simao Basin had undergone sulfate reduction, re-oxidation, reservoir effects, etc. In conclusion, the formation of continental evaporites was likely derived from seawater due to marine transgression during the Cretaceous period. Meanwhile, non-marine inflows have contributed to the basin significantly. |
| 英文关键词 | evaporites; the Lanping– Simao Basin; continental setting; sulfates; Sr; S; O isotopes |
| 语种 | 英语
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| WOS研究方向 | Geochemistry & Geophysics
; Mineralogy
; Mining & Mineral Processing
|
| WOS类目 | Geochemistry & Geophysics
; Mineralogy
; Mining & Mineral Processing
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| WOS记录号 | WOS:000622853900001
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| 来源期刊 | MINERALS
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| 来源机构 | 中国科学院青藏高原研究所
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| 文献类型 | 期刊论文
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| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/260149
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推荐引用方式
GB/T 7714 |
Shen, Lijian,Wang, Licheng,Liu, Chenglin,et al. Sr, S, and O Isotope Compositions of Evaporites in the Lanping-Simao Basin, China[J]. 中国科学院青藏高原研究所,2021,11(2).
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| APA |
Shen, Lijian,Wang, Licheng,Liu, Chenglin,&Zhao, Yanjun.(2021).Sr, S, and O Isotope Compositions of Evaporites in the Lanping-Simao Basin, China.MINERALS,11(2).
|
| MLA |
Shen, Lijian,et al."Sr, S, and O Isotope Compositions of Evaporites in the Lanping-Simao Basin, China".MINERALS 11.2(2021).
|
