| Reference Type | Journal (article/letter/editorial) |
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| Title | New evidence that the high temperature hornblende-schists below the Shetland ophiolite include basic igneous rocks intruded during obduction of the ‘cold’ ophiolite |
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| Journal | Scottish Journal of Geology |
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| Authors | Flinn, Derek | Author |
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| Year | 1993 (November) | Volume | 29 |
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| Issue | 2 |
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| Publisher | Geological Society of London |
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| DOI | doi:10.1144/sjg29020159Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 18621 | Long-form Identifier | mindat:1:5:18621:6 |
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| GUID | 0 |
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| Full Reference | Flinn, Derek (1993) New evidence that the high temperature hornblende-schists below the Shetland ophiolite include basic igneous rocks intruded during obduction of the ‘cold’ ophiolite. Scottish Journal of Geology, 29 (2) 159-165 doi:10.1144/sjg29020159 |
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| Plain Text | Flinn, Derek (1993) New evidence that the high temperature hornblende-schists below the Shetland ophiolite include basic igneous rocks intruded during obduction of the ‘cold’ ophiolite. Scottish Journal of Geology, 29 (2) 159-165 doi:10.1144/sjg29020159 |
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| In | (1993, November) Scottish Journal of Geology Vol. 29 (2) Geological Society of London |
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These are possibly similar items as determined by title/reference text matching only.
