IRON OXIDE INCLUSIONS IN THE RAINBOW LATTICE SUNSTONE FROM AUSTRALIA

2020 ◽  
Author(s):  
Shiyun Jin ◽  
◽  
Ziyin Sun ◽  
Karen V. Smit ◽  
Aaron C. Palke
Keyword(s):  
Minerals ◽  
2021 ◽  
Vol 11 (3) ◽  
pp. 241
Author(s):  
Doan Thi Anh Vu ◽  
Alongkot Fanka ◽  
Abhisit Salam ◽  
Chakkaphan Sutthirat

Sapphires from alluvial deposits associated with Cenozoic basalts in Southern Vietnam were collected for investigation of mineral inclusions. In this report, primary iron oxide inclusions were focused on, with detailed mineral chemistry using a Raman spectroscope and electron probe micro-analyzer. Consequently, a variety of iron oxide inclusions were recognized as wüstite, hercynite, and ilmenite. Ilmenite falling within an ilmenite–hematite series ranged in composition between Il24-30He36-38Mt35-40 and Il49-54He34-40Mt7-10, classified as titanomagnetite and titanohematite, respectively. Wüstite with non-stoichiometry, (Fe2+0.3-0.9)(Ti3+<0.179Al3+≤0.6Cr3+<0.1Fe3+≤0.46)☐≤0.23O, was associated with hercynite inclusions, clearly indicating cogenetic sapphire formation. Wüstite and sapphire appear to have been formed from the breakdown reaction of hercynite (hercynite = sapphire+wüstite) within a reduction magma chamber. Titanohematite and titanomagnetite series might have crystallized during iron–titanium reequilibration via subsolidus exsolution under a slightly oxidized cooling process.


1964 ◽  
Vol S7-VI (3) ◽  
pp. 397-401
Author(s):  
Marc Boucarut

Abstract The southern flank of the Maure-Vieille caldera of the Esterel massif of the Maritime Alps in southeastern France is remarkable for the large number of ignimbrite dikes in the series of alternating sedimentary and volcanic rocks of Permian age. Three types of dikes occur. The first is a rhyolitic rock poor in quartz and sanidine phenocrysts, but with abundant oriented laths consisting of a spherulitic quartz-potassic feldspar nucleus enclosed in an aureole of feldspar dusted with iron oxide. These 'fiammes' are devitrified fragments of pumice. The second type is of similar material but is brecciated in fragments cemented by a rhyolitic matrix. The third type is vitroclastic in structure with iron oxide inclusions, but completely devitrified. The rhyolite of the area is the same chemically as the ignimbrite, and the dikes of ignimbrite represent pyromagmatic fragmentation occurring in the conduits through which the rhyolite was erupted.


2011 ◽  
Vol 316 (1) ◽  
pp. 164-171 ◽  
Author(s):  
Barthélémy Desport ◽  
Joëlle Carpena ◽  
Jean-Louis Lacout ◽  
Daniel Borschneck ◽  
Jérôme Gattacceca
Keyword(s):  

1983 ◽  
Vol 61 (3) ◽  
pp. 219-225 ◽  
Author(s):  
Gye-won Hong ◽  
Jai-young Lee
Keyword(s):  

Author(s):  
H. Mori ◽  
Y. Murata ◽  
H. Yoneyama ◽  
H. Fujita

Recently, a new sort of nano-composites has been prepared by incorporating such fine particles as metal oxide microcrystallites and organic polymers into the interlayer space of montmorillonite. Owing to their extremely large specific surface area, the nano-composites are finding wide application[1∼3]. However, the topographic features of the microstructures have not been elucidated as yet In the present work, the microstructures of iron oxide-pillared montmorillonite have been investigated by high-resolution transmission electron microscopy.Iron oxide-pillared montmorillonite was prepared through the procedure essentially the same as that reported by Yamanaka et al. Firstly, 0.125 M aqueous solution of trinuclear acetato-hydroxo iron(III) nitrate, [Fe3(OCOCH3)7 OH.2H2O]NO3, was prepared and then the solution was mixed with an aqueous suspension of 1 wt% clay by continuously stirring at 308 K. The final volume ratio of the latter aqueous solution to the former was 0.4. The clay used was sodium montmorillonite (Kunimine Industrial Co.), having a cation exchange capacity of 100 mequiv/100g. The montmorillonite in the mixed suspension was then centrifuged, followed by washing with deionized water. The washed samples were spread on glass plates, air dried, and then annealed at 673 K for 72 ks in air. The resultant film products were approximately 20 μm in thickness and brown in color.


2018 ◽  
Vol 6 (10) ◽  
Author(s):  
Hosam Zaghloul ◽  
Doaa A. Shahin ◽  
Ibrahim El- Dosoky ◽  
Mahmoud E. El-awady ◽  
Fardous F. El-Senduny ◽  
...  

Antisense oligonucleotides (ASO) represent an attractive trend as specific targeting molecules but sustain poor cellular uptake meanwhile superparamagnetic iron oxide nanoparticles (SPIONs) offer stability of ASO and improved cellular uptake. In the present work we aimed to functionalize SPIONs with ASO targeting the mRNA of Cyclin B1 which represents a potential cancer target and to explore its anticancer activity. For that purpose, four different SPIONs-ASO conjugates, S-M (1–4), were designated depending on the sequence of ASO and constructed by crosslinking carboxylated SPIONs to amino labeled ASO. The impact of S-M (1–4) on the level of Cyclin B1, cell cycle, ROS and viability of the cells were assessed by flowcytometry. The results showed that S-M3 and S-M4 reduced the level of Cyclin B1 by 35 and 36%, respectively. As a consequence to downregulation of Cyclin B1, MCF7 cells were shown to be arrested at G2/M phase (60.7%). S-M (1–4) led to the induction of ROS formation in comparison to the untreated control cells. Furthermore, S-M (1–4) resulted in an increase in dead cells compared to the untreated cells and SPIONs-treated cells. In conclusion, targeting Cyclin B1 with ASO-coated SPIONs may represent a specific biocompatible anticancer strategy.


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