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<front>
<journal-meta>
<journal-id journal-id-type="archive">gsminmag</journal-id>
<journal-title>Mineralogical Magazine</journal-title>
<abbrev-journal-title abbrev-type="full">Mineralogical Magazine</abbrev-journal-title>
<issn pub-type="ppub">0026-461X</issn>
<publisher>
<publisher-name>Mineralogical Society</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1180/minmag.1979.043.325.04</article-id>
<title-group>
<article-title>Georgeite, a New Amorphous Copper Carbonate from the Carr Boyd Mine, Western Australia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Bridge</surname>
<given-names>P. J.</given-names>
</name>
<aff>Government Chemical Laboratories, 30 Plain Street, Perth, Western Australia 6000</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Just</surname>
<given-names>J.</given-names>
</name>
<aff>Australian Selection (Pty.) Ltd., 50 St. George's Terrace, Perth, Western Australia 6000</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Hey</surname>
<given-names>M. H.</given-names>
</name>
<aff>Department of Geology and Mineralogy, Parks Road, Oxford</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1979</year>
</pub-date>
<volume>43</volume>
<issue>325</issue>
<fpage>97</fpage>
<lpage>98</lpage>
<history>
<date date-type="received">
<day>4</day>
<month>1</month>
<year>1978</year>
</date>
<date date-type="rev-recd">
<day>25</day>
<month>9</month>
<year>1978</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1979, The Mineralogical Society</copyright-statement>
<copyright-year>1979</copyright-year>
<abstract>
<title>Summary</title>
<p>Georgeite, an amorphous copper carbonatehydrate, has been found in the oxidation zone of the Carr Boyd nickel deposit, Western Australia. It forms thin coatings mostly associated with malachite and chalconatronite on partly weathered tremolite rock containing disseminated copper and iron sulphides.</p>
<p>Physical properties: Colour light blue, streak pale blue, lustre vitreous to earthy, fracture conchoidal, soft, sp. gr. 2.55; transparent to sub-opaque (aggregates), <italic>n</italic>(Na<sub>D</sub>) = 1.593, isotropic. Amorphous to X-rays and electron beam.</p>
<p>Chemical microanalysis gave (wt%) CuO 54.9, ZnO 0.4, Na<sub>2</sub>O 2.7, CO<sub>2</sub> 20.8, H<sub>2</sub>O 21.7, sum 100.5. After deduction of all Na<sub>2</sub>O and corresponding amounts of CuO, CO<sub>2</sub>, and H<sub>2</sub>O as chalconatronite (12.35 wt%) the atomic ratios correspond to an empirical formula (Cu<sub>5.0</sub>, Zn<sub>0.05</sub>)(CO<sub>3</sub>)<sub>3</sub>(OH)<sub>4.12</sub>.6.3H<sub>2</sub>O, the ideal formula being Cu<sub>5</sub>(CO<sub>3</sub>)<sub>3</sub>(OH)<sub>4</sub>.6H<sub>2</sub>O.</p></abstract>
</article-meta>
</front>
</article>
