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catalogue of western australian meteorite collections

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Plate XXVI.<br />

(a), Photomicrograph <strong>of</strong> the MeIlenbye Meteorite--showing granular aggre.­<br />

gates <strong>of</strong> olivine and probably some pyroxene, apparently crushed fragments<br />

<strong>of</strong> chondrules or recrystaIlized chondrules. There is not very<br />

much glass evident and the <strong>meteorite</strong> appears to be brecciated and considerably<br />

recrystaIlized. The dark areas are nickel-iron and troilite and<br />

the white areas are cavities in this rather spongy <strong>meteorite</strong>. Magnification<br />

X25, PPL.<br />

(b) Photomicrograph <strong>of</strong> the W oolgorong Meteorite--showing large excentricfan<br />

type chondrule. The chondrule itself appears to be olivine. There<br />

is no glass present and the black material which shows in patches and<br />

veins is nickel-iron and troilite. White specks are oligocIase and this<br />

tends to fringe the chondrules. Magnification X63, PPL.<br />

(c) Photomicrograph <strong>of</strong> the Rawlinna Meteorite-showing a large olivine<br />

chondrule (a rather sparse occurrence in this <strong>meteorite</strong>) set in a granular<br />

base <strong>of</strong> olivine and subordinate orthopyroxene (both grey) nickel-iron<br />

and sulphide (both black). This <strong>meteorite</strong> appears to be slightly recrystallized<br />

and contains much more nickel-iron than is present in the<br />

*olivine-hypersthene-chondrites. Magnification X25, PPL.<br />

128

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