| Reference Type | Journal (article/letter/editorial) |
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| Title | Seismic reflection test on the granite of the Skye Tertiary igneous centre |
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| Journal | Geological Magazine |
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| Authors | Goulty, N. R. | Author |
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| Leggett, M. | Author |
| Douglas, T. | Author |
| Emeleus, C. H. | Author |
| Year | 1992 (September) | Volume | 129 |
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| Issue | 5 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800021804Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 255495 | Long-form Identifier | mindat:1:5:255495:6 |
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| GUID | 0 |
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| Full Reference | Goulty, N. R., Leggett, M., Douglas, T., Emeleus, C. H. (1992) Seismic reflection test on the granite of the Skye Tertiary igneous centre. Geological Magazine, 129 (5) 633-636 doi:10.1017/s0016756800021804 |
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| Plain Text | Goulty, N. R., Leggett, M., Douglas, T., Emeleus, C. H. (1992) Seismic reflection test on the granite of the Skye Tertiary igneous centre. Geological Magazine, 129 (5) 633-636 doi:10.1017/s0016756800021804 |
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| In | (1992, September) Geological Magazine Vol. 129 (5) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractWe have conducted a seismic reflection test over a short profile on the granite of the Skye Tertiary central intrusive complex. From previous gravity modelling work it had been inferred that the granite is approximately 1.5 km thick and overlies basic rocks. The seismic data indicate that the granite is at least 2 km thick at the test location. Reflection events of alternating polarity between depths of 2.1 and 2.4 km suggest that basic and acidic sheets are interlayered at the base of the granitic mass. |
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