| Reference Type | Journal (article/letter/editorial) |
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| Title | Post-cumulus disruption of the Lilloise Intrusion, East Greenland |
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| Journal | Geological Magazine |
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| Authors | Matthews, D. W. | Author |
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| Year | 1976 (May) | Volume | 113 |
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| Issue | 3 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800043272Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 251165 | Long-form Identifier | mindat:1:5:251165:2 |
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| GUID | 0 |
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| Full Reference | Matthews, D. W. (1976) Post-cumulus disruption of the Lilloise Intrusion, East Greenland. Geological Magazine, 113 (3) 287-296 doi:10.1017/s0016756800043272 |
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| Plain Text | Matthews, D. W. (1976) Post-cumulus disruption of the Lilloise Intrusion, East Greenland. Geological Magazine, 113 (3) 287-296 doi:10.1017/s0016756800043272 |
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| In | (1976, May) Geological Magazine Vol. 113 (3) Cambridge University Press (CUP) |
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| Abstract/Notes | SummaryField, petrographic and chemical evidence from the cumulates of western Lilloise suggest a substantially higher level of exposure in the cumulus pile than is seen on the E side, due to relative subsistence of the western half of the intrusion. It is suggested that the subsistence started while both cumulus pile and the surrounding basalts were still hot and not fully consolidated. When, later, reactivation occurred, the rocks were in a more cohesive state and ‘syenitic’ magma was available for intrusion as discrete sheets and veins. |
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