Bulletin of Mineralogy, Petrology and Geochemistry最新文献

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Genesis of the Baping quartz deposit in the western Guangxi: Evidences from fluid inclusions, C-H-O isotopes and rare earth elements 广西西部巴平石英矿床的成因:流体包裹体、C-H-O 同位素和稀土元素的证据
Bulletin of Mineralogy, Petrology and Geochemistry Pub Date : 2024-01-01 DOI: 10.3724/j.issn.1007-2802.20240024
Li-jia He, Qing-feng Ruan, Zhihui Qiu, Shi-bo Cheng, Zi-han Zhou
{"title":"Genesis of the Baping quartz deposit in the western Guangxi: Evidences from fluid inclusions, C-H-O isotopes and rare earth elements","authors":"Li-jia He, Qing-feng Ruan, Zhihui Qiu, Shi-bo Cheng, Zi-han Zhou","doi":"10.3724/j.issn.1007-2802.20240024","DOIUrl":"https://doi.org/10.3724/j.issn.1007-2802.20240024","url":null,"abstract":"","PeriodicalId":502214,"journal":{"name":"Bulletin of Mineralogy, Petrology and Geochemistry","volume":"123 5-6","pages":""},"PeriodicalIF":0.0,"publicationDate":"2024-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140516985","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Current status and prospect of researches on sediment-hosted Li deposits in bauxite formations and coal-bearing strata in China 中国铝土地层和含煤地层沉积型锂矿床研究现状与展望
Bulletin of Mineralogy, Petrology and Geochemistry Pub Date : 2024-01-01 DOI: 10.3724/j.issn.1007-2802.20240006
Qi-dao Zhang, Shao-yong Jiang, Wei Wang, Wenlong Ge
{"title":"Current status and prospect of researches on sediment-hosted Li deposits in bauxite formations and coal-bearing strata in China","authors":"Qi-dao Zhang, Shao-yong Jiang, Wei Wang, Wenlong Ge","doi":"10.3724/j.issn.1007-2802.20240006","DOIUrl":"https://doi.org/10.3724/j.issn.1007-2802.20240006","url":null,"abstract":": The sediment-hosted Li deposit is one type of the most important lithium deposits found in nature. Sediment-hosted Li deposits in bauxite formations and coal-bearing strata are mainly distributed in the southwestern Yangtze block and the North China block in China. This type of Li-clay deposit is famous for its large reserve, stable strata and wide distribution. Hence, studying this type of Li-clay deposits is of great significance to solve the lithium resource dilemma of China in the future. In this paper, we have summarized the distribution of this type of Li-clay deposits in bauxite formations and coal-bearing strata in China, and have sorted out research progresses on the Li occurrence state, material source, and development and utilization status of the Li-clay deposits. The Li enrichment process is mainly related to the weathering-sedimentation and volcanic magmatism processes, and the lithium was mainly sourced from the Li-rich basement rocks including volcanic tuff, early formed magmatic rock, clay rock and other rocks. Lithium mainly occurred in forms of lithium independent minerals (cookeite), and isomorphic replacement/adsorption in/on clay","PeriodicalId":502214,"journal":{"name":"Bulletin of Mineralogy, Petrology and Geochemistry","volume":"104 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2024-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139636578","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
The paradigm and recent progress in studying marine mercury isotopes 海洋汞同位素研究的范式和最新进展
Bulletin of Mineralogy, Petrology and Geochemistry Pub Date : 2024-01-01 DOI: 10.3724/j.issn.1007-2802.20240016
Ruo-yu Sun, Cheng-hao Li, Song-jing Li, Zhao Wang, Xiao-wei Chen, Jing-jing Yuan, Yi Liu
{"title":"The paradigm and recent progress in studying marine mercury isotopes","authors":"Ruo-yu Sun, Cheng-hao Li, Song-jing Li, Zhao Wang, Xiao-wei Chen, Jing-jing Yuan, Yi Liu","doi":"10.3724/j.issn.1007-2802.20240016","DOIUrl":"https://doi.org/10.3724/j.issn.1007-2802.20240016","url":null,"abstract":": Mercury (Hg) is a heavy metal that is biologically toxic and can be transported globally as a gas. In the marine environment, Hg is easily converted to the neurotoxin methyl-Hg which bioaccumulates and biomagnifies through the food web, posing risks to ecosystems and human health. Accurately constraining the source, migration, and transformation of marine Hg is crucial for understanding the Hg cycle and has significant value in updating existing marine Hg cycling models and formulating relevant environmental policies. Over the past decade, the development of Hg stable isotope techniques has provided novel insights into the study of Hg cycling in the environment, as well as the related ecological effects. The unique “three-dimensional” fractionation pattern of Hg isotopes, especially the mass independent fractionation (MIF) has brought about a paradigm shift to the study of marine Hg cycling and achieved a series of important discoveries. In this study, we systematically review the recent progress of Hg isotope system in tracing marine Hg cycling, including the sources of Hg in oceans and the generation, transport and transformation of methyl-Hg. Specifically, we provide a key analysis and outlook on recent research hotspots, such as the atmospheric depositional pathways and the cycling of methyl-Hg in open oceans. We recommend that the future research should combine more sophisticated Hg isotope measurement tools and more environmentally relevant Hg isotope fractionation control experiments to further clarify the main controlling factors of marine Hg isotope fractionation and expand the application of Hg isotopes.","PeriodicalId":502214,"journal":{"name":"Bulletin of Mineralogy, Petrology and Geochemistry","volume":"10 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2024-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139640325","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Gensis of geothermal water in the Da Qaidam area, northern margin of the Qaidam Basin: Constraints from hydrochemistry and isotopes of hydrogen-oxygen-strontium 盖达姆盆地北缘盖达姆地区的地热水:水化学和氢氧锶同位素的制约因素
Bulletin of Mineralogy, Petrology and Geochemistry Pub Date : 2023-12-01 DOI: 10.3724/j.issn.1007-2802.20240010
Bing Wang, Xi-wei Qin, Er-feng Ren, Zi-wen Jiang, Ning Feng, Guo-rong Li, Sha Yang, Wei Li
{"title":"Gensis of geothermal water in the Da Qaidam area, northern margin of the Qaidam Basin: Constraints from hydrochemistry and isotopes of hydrogen-oxygen-strontium","authors":"Bing Wang, Xi-wei Qin, Er-feng Ren, Zi-wen Jiang, Ning Feng, Guo-rong Li, Sha Yang, Wei Li","doi":"10.3724/j.issn.1007-2802.20240010","DOIUrl":"https://doi.org/10.3724/j.issn.1007-2802.20240010","url":null,"abstract":": In order to explore the hydrochemical characteristics and genetic model of the geothermal field in Da Qaidam, the northern margin of the Qaidam basin,14 groups of groundwater sample of this area were analyzed for hydrochemical components and isotopes ( δ D, δ 18 O, 87 Sr/ 86 Sr, 3 H) in this study. The results show that the outlet temperature of underground hot water in Da Qaidam is 52~74°C, and the total dissolved solids (TDS) content is 959.8~1451.3 mg/L. The hydrochemical types of the groundwater are all the Cl-Na type, and according to the ion correlation and 87 Sr/ 86 Sr value, the main solutes of groundwater in the area originate from the dissolution of evaporites and silicate minerals. Stable isotopes of hydrogen and oxygen show that atmospheric precipitation is the main source of groundwater recharge and part of the groundwater is recharged by magma water, and the estimated recharge elevation is 3591~4374 m. XSWQ-06 and XSWQ-07 have significant oxygen drift, mainly due to evaporation and enhanced water-rock reaction. Based on the SiO 2 geothermal temperature scale","PeriodicalId":502214,"journal":{"name":"Bulletin of Mineralogy, Petrology and Geochemistry","volume":"2 5","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139190646","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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