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Journal ArticleDOI

The Occurrence of Zinnwaldite in Cornwall

E. K. Cundy
- 01 Jan 1960 - 
- Vol. 4, Iss: 23, pp 151-156
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This article is published in Clay Minerals.The article was published on 1960-01-01. It has received 9 citations till now. The article focuses on the topics: Zinnwaldite.

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Advance review on the exploitation of the prominent energy-storage element: Lithium. Part I: From mineral and brine resources

TL;DR: In this article, an overview of the processes investigated for the extraction, separation and recovery of lithium from not only a technological perspective but also from a chemical perspective is presented, which can contribute to improving the extraction and recovery processes of lithium toward the sustainability of this critical element and can provide future research directions.
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The Cornubian batholith, SW England: D/H and 18O/16O studies of kaolinite and other alteration minerals

TL;DR: In this paper, D/H and 18 O/16 O ratios were determined on minerals and whole-rock samples of fresh granites, granites altered during greisenization and kaolinization of the Hercynian Cornubian batholith, detrital kaolinitic sediments of the Bovey Formation, and modern meteoric waters.
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The cell dimensions and symmetry of layer-lattice silicatesI. Some structural considerations

TL;DR: In this paper, the theoretical basis underlying accepted b-axis formulae (giving the sheet dimensions of layer-lattice silicates in terms of composition) has been re-examined and it is now proposed that in general the D-axis is determined by the octahedral layer together with (for micas) the interlayer cation.
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The correlation between lithium and magnesium in trioctahedral micas; improved equations for Li 2 O estimation from MgO data

TL;DR: In this paper, the correlation between Li20 and MgO contents in trioctahedral micas was investigated and it was demonstrated that the relations between both oxides are strongly dependent upon the geological environment in which the mica was formed.
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The origins of late-stage rocks in the St Austell granite—a re-interpretation

TL;DR: The origin of the St Austell granite is discussed in the light of new petrographic, chemical and experimental evidence as mentioned in this paper, which is essentially two stages of magmatic activity, the first represented by the intrusion of several phases of biotite granite, the second by a later intrusion of non-megacrystic lithium-mica granite which crystallized from a volatile-rich residual of the bioteitite granite magma.
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