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Asbestos Fibers and Other Elongate Mineral Particles: State of the ...

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Table 2. Definitions <strong>of</strong> specific minerals (Continued)<br />

Glossary <strong>of</strong> Geology, 5th ed.<br />

[American Geological Institute 2005] Leake et al. [1997] NIOSH [1990a]<br />

Dictionary <strong>of</strong> Mining,<br />

<strong>Mineral</strong>, <strong>and</strong> Related Terms<br />

[U.S. Bureau <strong>of</strong> Mines 1996]<br />

[Note: Footnotes identify <strong>the</strong> Primary<br />

Source Citation for <strong>the</strong> definition]<br />

Term<br />

Fluoro-edenite A vitreous dark brown monoclinic<br />

mineral <strong>of</strong> <strong>the</strong> amphibole group: (Na,K)<br />

Ca2(Mg,Fe2+ ) 5(Si7Al)O22(F,OH). It<br />

represents edenite with F>OH.<br />

NIOSH CIB 62 • <strong>Asbestos</strong><br />

A monoclinic Mg-Fe-Mn-Li<br />

amphibole: Fe2+ 7Si8O22(OH) 2;<br />

may also contain magnesium<br />

but with Mg/(Mg+Fe2+ ) < 0.50<br />

(o<strong>the</strong>rwise it is cummingtonite).<br />

Grunerite A monoclinic mineral,<br />

(Fe,Mg) 7Si8O22(OH) 2;<br />

amphibole group; with Mg/<br />

(Mg+Fe2+ ) = 0-0.30; forms<br />

series with cummingtonite <strong>and</strong><br />

magnesiocummingtonite; fibrous<br />

or needlelike, commonly in<br />

radial aggregates; characteristic<br />

<strong>of</strong> iron formations in <strong>the</strong> Lake<br />

Superior <strong>and</strong> Labrador Trough<br />

regions. Also spelled gruenerite.<br />

A 1:1 aluminosilicate clay mineral<br />

Al •<br />

2Si2O5(OH) 4 X(H2O) similar to kaolinite<br />

but perhaps with some Al(IV) <strong>and</strong><br />

interlayer cations to compensate for <strong>the</strong><br />

Al(IV). Probably because <strong>of</strong> this it is able<br />

to incorporate water in <strong>the</strong> interlayer space<br />

[Bailey 1989]. The terms “halloysite (7Å)” <strong>and</strong><br />

halloysite (10Å)” were recommended for <strong>the</strong><br />

anhydrous <strong>and</strong> dihydrate forms, respectively<br />

[Brindley <strong>and</strong> Pegro 1976] 3 ; <strong>the</strong> term “endellite”<br />

should not be used [Bailey et al. 1980]. 4<br />

Halloysite 1. A monoclinic mineral,<br />

2[Al4Si4(OH) 8O10]; kaoliniteserpentine<br />

group; made up<br />

<strong>of</strong> slender tubes as shown<br />

by electron microscopy; a<br />

gangue mineral in veins.<br />

2. Used as a group name to include<br />

natural “halloysite minerals” with<br />

different levels <strong>of</strong> hydration, as<br />

well as those formed artificially.<br />

See footnotes at end <strong>of</strong> table. (Continued)<br />

149

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