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Bradshaw, R., Phillips, F. C. (1967) X-ray studies of natural fabrics: I. Growth-fabrics in hematite kidney ore and in fibrous calcite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (277) 70-77 doi:10.1180/minmag.1967.036.277.10

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Reference TypeJournal (article/letter/editorial)
TitleX-ray studies of natural fabrics: I. Growth-fabrics in hematite kidney ore and in fibrous calcite
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsBradshaw, R.Author
Phillips, F. C.Author
Year1967 (March)Volume36
Issue277
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_36/36-277-70.pdf+
DOIdoi:10.1180/minmag.1967.036.277.10Search in ResearchGate
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Mindat Ref. ID6036Long-form Identifiermindat:1:5:6036:7
GUID0
Full ReferenceBradshaw, R., Phillips, F. C. (1967) X-ray studies of natural fabrics: I. Growth-fabrics in hematite kidney ore and in fibrous calcite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (277) 70-77 doi:10.1180/minmag.1967.036.277.10
Plain TextBradshaw, R., Phillips, F. C. (1967) X-ray studies of natural fabrics: I. Growth-fabrics in hematite kidney ore and in fibrous calcite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (277) 70-77 doi:10.1180/minmag.1967.036.277.10
In(1966) Mineralogical Magazine Vol. 36 (277) Mineralogical Society
Abstract/NotesSummaryFibres of hematite in kidney ore are elongated at right angles to the c-axis. The fibre axis, which may be normal to a face of either of the hexagonal prisms {101Μ„0} or {112Μ„0}, may show an abrupt change of orientation along the length of a fibre. There is little preferred orientation around the length of the fibres.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 c.


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