Smith, W. W. (1959) Pseudomorphs after olivine in Markle basalt. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (247) 324-331 doi:10.1180/minmag.1959.032.247.05

Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Pseudomorphs after olivine in Markle basalt | ||
Journal | Mineralogical Magazine and Journal of the Mineralogical Society | ||
Authors | Smith, W. W. | Author | |
Year | 1959 (December) | Volume | 32 |
Issue | 247 | ||
Publisher | Mineralogical Society | ||
Download URL | https://rruff.info/doclib/MinMag/Volume_32/32-247-324.pdf+ | ||
DOI | doi:10.1180/minmag.1959.032.247.05 | ||
Generate Citation Formats | |||
Mindat Ref. ID | 5537 | Long-form Identifier | mindat:1:5:5537:0 |
GUID | 0 | ||
Full Reference | Smith, W. W. (1959) Pseudomorphs after olivine in Markle basalt. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (247) 324-331 doi:10.1180/minmag.1959.032.247.05 | ||
Plain Text | Smith, W. W. (1959) Pseudomorphs after olivine in Markle basalt. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (247) 324-331 doi:10.1180/minmag.1959.032.247.05 | ||
In | (1959) Mineralogical Magazine Vol. 32 (247) Mineralogical Society | ||
Abstract/Notes | SummaryPseudomorphs after olivine in Markle basalt from Holyrood Park, Edinburgh, consist of an intimate mixture of hematite and chlorite, along with a small percentage of quartz. A definite relationship exists between the orientations of the two main constituents and is dependent upon their structures. |
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