Boron occurrence in halite and boron isotope geochemistry of halite in the Qarhan Salt Lake, western China
文献类型:期刊论文
作者 | Fan, QiShun![]() ![]() ![]() ![]() ![]() ![]() ![]() |
刊名 | SEDIMENTARY GEOLOGY
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出版日期 | 2015-06-01 |
卷号 | 322页码:34-42 |
关键词 | b Isotope Composition Halite Qarhan Salt Lake Qaidam Basin Western China |
文献子类 | Article |
英文摘要 | Previous studies have investigated boron (B) isotope composition of salt lake brines in the Qaidam Basin, western China. However, the research on B isotope geochemistry of halite from a sediment core in a typical sedimentary basin has been very limited. In this study, a 102-m-long drill core (ISL1A) was recovered from Qarhan Salt take in eastern Qaidam Basin. Forty-three halite samples from upper 44.0 m in ISL1A were collected and analyzed for chemical compositions (K+, Na+, Ca2+, Mg2+, Cl-, SO42-, Sr2+ and B3+) and B isotopes in order to investigate their relationships, and B isotope fractionation between halite and brines in the Qarhan Salt Lake. The results show that: (1) more B3+ and Mg2+ values in halite are low concentrations and more concentrated, and low B3+ concentrations have a strong correlation with low Mg2+ in halite, which imply that they might be the same source; (2) low Mg2+ values in halite from ISL1A have a similar trend with Mg-m(2+) (molarity) of fluid inclusion brines from two sediment cores (east to ISL1A about 50 km) in the study area, suggesting that low B3+ and Mg2+ concentrations should derive from fluid inclusions in halite based on X-ray diffraction results in ISL1A that no borate and small amount of magnesium salts were deposited; (3) delta B-11 values of halite in ISL1A range from -0.35 to +5.84 parts per thousand, which are in the range of those of river water and brines (-1.0 to +9.6 parts per thousand), and almost overlapped with those of brines (+2.9 to + 7.5 parts per thousand) in the Qarhan Salt Lake. These results suggest that no or minor B isotope fractionation between halite and brine occurred. (C) 2015 Elsevier B.V. All rights reserved. |
WOS关键词 | IONIZATION MASS-SPECTROMETRY ; QAIDAM BASIN ; POTASH EVAPORITES ; TIBETAN PLATEAU ; SEA-WATER ; ORIGIN ; NONMARINE ; MARINE ; FRACTIONATION ; SEDIMENTS |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000355059900003 |
源URL | [http://ir.isl.ac.cn/handle/363002/6138] ![]() |
专题 | 青海盐湖研究所_青海盐湖研究所知识仓储 青海盐湖研究所_盐湖地质与环境实验室 青海盐湖研究所_管理部门 |
作者单位 | Chinese Acad Sci, Qinghai Inst Salt Lakes, Xining 810008, Peoples R China |
推荐引用方式 GB/T 7714 | Fan, QiShun,Ma, YunQi,Cheng, HuaiDe,et al. Boron occurrence in halite and boron isotope geochemistry of halite in the Qarhan Salt Lake, western China[J]. SEDIMENTARY GEOLOGY,2015,322:34-42. |
APA | Fan, QiShun.,Ma, YunQi.,Cheng, HuaiDe.,Wei, HaiCheng.,Yuan, Qin.,...&Shan, FaShou.(2015).Boron occurrence in halite and boron isotope geochemistry of halite in the Qarhan Salt Lake, western China.SEDIMENTARY GEOLOGY,322,34-42. |
MLA | Fan, QiShun,et al."Boron occurrence in halite and boron isotope geochemistry of halite in the Qarhan Salt Lake, western China".SEDIMENTARY GEOLOGY 322(2015):34-42. |
入库方式: OAI收割
来源:青海盐湖研究所
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