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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.1977.041.320.10</article-id>
<title-group>
<article-title>The Mayo Belwa Meteorite: A New Enstatite Achondrite Fall</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Graham</surname>
<given-names>A. L.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Easton</surname>
<given-names>A. J.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Hutchison</surname>
<given-names>R.</given-names>
</name></contrib>
<aff>Department of Mineralogy, British Museum (Natural History), London SW7 5BD</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1977</year>
</pub-date>
<volume>41</volume>
<issue>320</issue>
<fpage>487</fpage>
<lpage>492</lpage>
<history>
<date date-type="received">
<day>17</day>
<month>11</month>
<year>1976</year>
</date>
<date date-type="rev-recd">
<day>6</day>
<month>1</month>
<year>1977</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1977, The Mineralogical Society</copyright-statement>
<copyright-year>1977</copyright-year>
<abstract>
<title>Summary</title>
<p>Mayo Belwa, a highly shocked enstatite achondrite, fell during the evening of 3 August 1974 in the Adamawa District, NE. Nigeria (8&#x00B0; 58' N., 12&#x00B0; 05' E.). The stone weighed 4&#x00B7;85 kg and was deposited in the Geological Survey of Nigeria and loaned for study to the British Museum (Natural History). It is composed principally of enstatite (0&#x00B7;02 FeO%), with some olivine (Fo<sub>100</sub>), diopside, feldspar (An<sub>9</sub> Ab<sub>88</sub> Or<sub>3</sub>), and minor Fe-Ni metal and the sulphides oldhamite, daubr&#x00E9;elite, ferroan alabandine, and troilite. The kamacite contains between 0&#x00B7;15% and 1&#x00B7;2% Si and the troilite contains 1&#x00B7;1%. The meteorite possesses vuggy cavities, which contain fluor-amphibole needles projecting from their walls, suggesting the presence at some time of a volatile-rich phase. The titanium-rich troilite, the nearly ironfree enstatite and the Mg/Si ratio are typical of the E-achondrites.</p></abstract>
</article-meta>
</front>
</article>
