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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.1967.036.277.10</article-id>
<title-group>
<article-title>X-ray Studies of Natural Fabrics. I. Growth-Fabrics in Hematite Kidney Ore and in Fibrous Calcite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Bradshaw</surname>
<given-names>R.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Phillips</surname>
<given-names>F. C.</given-names>
</name></contrib>
<aff>Department of Geology, University of Bristol</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1967</year>
</pub-date>
<volume>36</volume>
<issue>277</issue>
<fpage>70</fpage>
<lpage>77</lpage>
<history>
<date date-type="received">
<day>17</day>
<month>11</month>
<year>1966</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1967, The Mineralogical Society</copyright-statement>
<copyright-year>1967</copyright-year>
<abstract>
<title>Summary</title>
<p>Fibres of hematite in kidney ore are elongated at right angles to the <italic>c</italic>-axis. The fibre axis, which may be normal to a face of either of the hexagonal prisms &#x007B;<inline-formula><mml:math><mml:mrow><mml:mn>10</mml:mn><mml:mover><mml:mn>1</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>0</mml:mn></mml:mrow></mml:math></inline-formula>&#x007D; or &#x007B;<inline-formula><mml:math><mml:mrow><mml:mn>11</mml:mn><mml:mover><mml:mn>2</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>0</mml:mn></mml:mrow></mml:math></inline-formula>&#x007D;, may show an abrupt change of orientation along the length of a fibre. There is little preferred orientation around the length of the fibres.</p>
<p>It is confirmed that in some calcite satin spar the fibres are elongated parallel to an edge of the cleavage rhombohedron; in other fibrous growths the elongation is either parallel to or Perpendicular to <italic>c</italic>.</p></abstract>
</article-meta>
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