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Article
Lithium-rich claystone in **guo area, Guangxi, southwest China: precursor kaolinite controls lithium enrichment
We investigated Late Permian Li-rich claystones with up to 1.05 wt% Li2O (average: 0.45 wt% Li2O) in the **guo area in Guangxi, southwest China. Our results show that cookeite (chlorite group) is the dominant L...
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Article
Lithium and oxygen isotopic constraints on the source and evolution of ore-forming fluids: a case study from the Shuiyindong Carlin-type gold deposit, SW China
Carlin-type gold deposits are among the most important gold-bearing hydrothermal ore systems and are mainly located in Nevada, USA, and southwestern China. However, the source and evolution of the ore-forming ...
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Article
Super-enrichment of lithium and niobium in the upper Permian Heshan Formation in **guo, Guangxi, China
The upper Permian Heshan Formation in **guo, Guangxi, China, is strongly enriched in lithium (Li) and niobium (Nb). The lower bauxite layer contains 0.02–0.04 wt.%Nb2O5 (averaging 0.035 wt.%), and the overlying...
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Article
Occurrence Modes of Niobium in Kaolin Clay From Guizhou, China
Niobium in kaolin clay from the Late Permian sequences was reported in the range of several hundreds of micrograms per gram and was considered as a potential resource for its high concentrations and large area...
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Article
Correlation between δ 18O, Sr/Ca and Mg/Ca of coral Acropora and seawater temperature from coral culture experiments
To be used as proxies of seawater surface temperature (SST), the δ 18Oc values and Sr/Ca and Mg/Ca ratios of scleractinian coral skeletons must be verified by coral culture experiments in ...
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Article
Sample preparation for isotopic determination of boron in clay sediments
The procedures of sample preparation for isotopic determination of boron in clay sediments is very cumbersome, by far, there haven’t been relevant reports on that. In order to establish an effective method for...
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Article
Open AccessStable isotope fractionation of chlorine during evaporation of brine from a saline lake
Brine from the saline Qarhan Lake was evaporated at 28±2°C in a clean environment. Two groups of experiments were conducted; one with complete separation of precipitate and brine at different stages of evapora...