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Sure, back then mindful-vaping spas and perma-brunch V.R. cafés were ubiquitous, but at least you didn't stagger along outside those places of business, brittle-boned and lethargic from a lack of vitamins and minerals, while the moneyed scenesters inside licked huge chunks of calcium-rich, life-giving mineral blocks.
Illite and mixture of illite and montmorillonite with strong attached conductance are the major clay minerals, while the content of kaolinite with weak attached conductance is low.
The mercury in YZ coal is mainly distributed in clay minerals while the pyrite dispersed in fine size in vitrinite is syngenetic originated.
Aluminium (Al) and magnesium (Mg) were also detected all across the door frame, most likely originating from matrix minerals, while the presence of strontium (Sr) relates to the presence of calcium carbonate.
The Selebi-Phikwe ore body consists of four co-occurring sulphide minerals pentlandite, chalcopyrite, pyrite and pyrrhotite along with other minerals, while the major gangues are amphibolites, quartz, mica and feldspar, forming typically about 68%% (Table 1).
When compared with the parent material (the Cg horizon), the Bt1 and Bt2 horizons are enriched in clay minerals while the Ap, AEg, and E horizons are depleted in clays.
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As, Hg, Mo, Ge, Ga, Ta, Ti, W, Mn are mainly concentrated in the minerals while Be, Th, P, Sc, Sr, Y, Yb, B, V are mainly found in the organic matter according to the correlation analyses of the trace elements and between the trace elements and the maceral groups.
Also Ca particles are mainly due to building activity; these hypothesis are reinforced by HCA results which show a strong correlation between Si-Al then associated to K, in urban and rural sites (Si, Al and K are characteristic of the local terrigenous minerals), while in the yard site two linked sub-groups of correlated parameter are evident (Si-O and K-Al).
Calcium in conjunction with dissolved inorganic carbon formed compact and localized aragonite minerals, while in the absence of calcium chukanovite dominated, which covered and passivated the reactive surface to a higher extent.
Gene expression of bone morphogenic protein-2 and osteopontin was elevated on mineral-containing regions as compared to regions without mineral, while the expression of alkaline phosphatase mRNA revealed the opposite trend.
We showed that the symmetric mode often happens at large aspect ratio and large volume fraction of mineral, while the anti-symmetric happens at small aspect ratio and small volume fraction.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com