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DOI | 10.1016/j.gexplo.2017.11.001 |
Origins of the Mid-Cretaceous evaporite deposits of the Sakhon Nakhon Basin in Laos: Evidence from the stable isotopes of halite | |
Li, Minghui; Yan, Maodu; Fang, Xiaomin; Zhang, Zengjie; Wang, Zhengrong; Sun, Shurui; Li, Jiao; Liu, Xiaoming | |
通讯作者 | Li, MH (通讯作者) |
发表日期 | 2018 |
ISSN | 0375-6742 |
EISSN | 1879-1689 |
起始页码 | 209 |
结束页码 | 222 |
卷号 | 184 |
英文摘要 | The origins of the evaporite deposits of the Khorat Plateau remain disputed. Based purely on the known evolution of the Khorat Plateau, materials of marine origin and/or remnant seawater should be present, but instead the salt layers of the deposits found there present typically continental lithological features. New data suggest that the Laotian evaporite deposits can be dated to the Middle to Late Cretaceous. In this paper we present the sulfate delta S-34 (5.2% to 15.6%) and delta O-18-(SO4) (10.3% to 14.1%) records, Sr isotopic compositions (0.707443 to 0.708587), delta O-18(-inclusion) (-7.1% to 13.9%) and delta D-inclusion (-72% to -150%) records and the trace metal elements for halite deposits extracted from Core ZK2893 in the Sakhon Nakhon Basin, Laos. These values suggest that the deposits are of continental and hydrothermal origins with trace marine remnants. Evaporites in the basins are very likely to have been formed originally by the evaporation of seawater, prior to being dissolved in meteoric water and hydrothermal fluid, and subsequently precipitated. |
关键词 | WESTERN YUNNANKHORAT PLATEAUMARINE SULFATESULFURSTRONTIUMEVOLUTIONTHAILANDSEAWATEROXYGENCHINA |
英文关键词 | Stable isotopes; Evaporate deposits; Halite; Laos |
语种 | 英语 |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:000416714400018 |
来源期刊 | JOURNAL OF GEOCHEMICAL EXPLORATION
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/259306 |
推荐引用方式 GB/T 7714 | Li, Minghui,Yan, Maodu,Fang, Xiaomin,et al. Origins of the Mid-Cretaceous evaporite deposits of the Sakhon Nakhon Basin in Laos: Evidence from the stable isotopes of halite[J]. 中国科学院青藏高原研究所,2018,184. |
APA | Li, Minghui.,Yan, Maodu.,Fang, Xiaomin.,Zhang, Zengjie.,Wang, Zhengrong.,...&Liu, Xiaoming.(2018).Origins of the Mid-Cretaceous evaporite deposits of the Sakhon Nakhon Basin in Laos: Evidence from the stable isotopes of halite.JOURNAL OF GEOCHEMICAL EXPLORATION,184. |
MLA | Li, Minghui,et al."Origins of the Mid-Cretaceous evaporite deposits of the Sakhon Nakhon Basin in Laos: Evidence from the stable isotopes of halite".JOURNAL OF GEOCHEMICAL EXPLORATION 184(2018). |
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