28.04.2014 Views

guide to thin section microscopy - Mineralogical Society of America

guide to thin section microscopy - Mineralogical Society of America

guide to thin section microscopy - Mineralogical Society of America

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Guide <strong>to</strong> Thin Section Microscopy<br />

Extinction<br />

Sign <strong>of</strong> elongation l<br />

Crystals with columnar <strong>to</strong> acicular or platy <strong>to</strong> flaky habits show elongate <strong>section</strong>s if cut<br />

parallel <strong>to</strong> their long morphological axis or perpendicular <strong>to</strong> a dominantly developed basal<br />

plane. If such elongate <strong>section</strong>s are rotated in<strong>to</strong> a diagonal position (i.e., long axis l parallel <strong>to</strong><br />

NE-SW) they show under crossed polarizers and compensa<strong>to</strong>r-in (first-order red plate or λ/4<br />

plate) either addition (Γ Comp + Γ Min = Γ <strong>to</strong>tal ) or subtraction (Γ Comp - Γ Min = Γ <strong>to</strong>tal ), depending on<br />

their optic sign (Fig. 4-45).<br />

Addition is observed if the wave with the larger refractive index (n z ') vibrates parallel or at a<br />

small angle <strong>to</strong> the long dimension <strong>of</strong> the crystal <strong>section</strong>: l (+) = positive sign <strong>of</strong> elongation or<br />

"length-slow". Examples: acicular-columnar crystals– sillimanite, gedrite, anthophyllite; platy<br />

crystals– gehlenite, micas, antigorite, pennine.<br />

Subtraction is observed if the wave with the smaller refractive index (n x ') vibrates parallel or<br />

at a small angle <strong>to</strong> the long dimension <strong>of</strong> the crystal <strong>section</strong>: l (–) = negative sign <strong>of</strong><br />

elongation or "length-fast". Examples: acicular-columnar crystals– <strong>to</strong>urmaline, apatite; platy<br />

crystals– åkermanite, brucite, clinochlore.<br />

For optically uniaxial mineral species with acicular-columnar habit, the sign <strong>of</strong> elongation<br />

corresponds <strong>to</strong> the optic sign. For platy uniaxial minerals, the two signs are opposite.<br />

Elongate <strong>section</strong>s in which n y is parallel (or at a small angle) <strong>to</strong> the morphological long axis<br />

<strong>of</strong> the crystal or perpendicular <strong>to</strong> the planar dimension <strong>of</strong> platy crystals show a variable sign<br />

<strong>of</strong> elongation, l(+) or l(–), depending on the exact orientation <strong>of</strong> the crystal in <strong>thin</strong> <strong>section</strong>.<br />

Examples <strong>of</strong> such elongate crystals– wollas<strong>to</strong>nite, epidote.<br />

Raith, Raase & Reinhardt – February 2012<br />

Figure 4-45 A. Platy muscovite showing positive sign <strong>of</strong> elongation. In muscovite and firs<strong>to</strong>rder<br />

red plate, fast (n x ) and slow (n y ↔n z ) waves vibrate in identical orientation. Therefore,<br />

the retardation adds up and increased interference colours result (Γ res = Γ Red1 + Γ Ms = 1231 nm;<br />

second-order blue-green).<br />

109

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!