Reference Type | Journal (article/letter/editorial) |
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Title | The dolerite-chalk contact of Scawt Hill, Co. Antrim. The production of basic alkali-rocks by the assimilation of limestone by basaltic magma |
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Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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Authors | Tilley, C. E. | Author |
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Harwood, H. F. | Author |
Year | 1931 (March) | Volume | 22 |
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Page(s) | 439-468 | Issue | 132 |
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Publisher | Mineralogical Society |
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URL | |
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Download URL | https://rruff.info/doclib/MinMag/Volume_22/22-132-439.pdf+ |
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DOI | doi:10.1180/minmag.1931.022.132.02 |
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| Generate Citation Formats |
Classification | Not set | LoC | Not set |
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Mindat Ref. ID | 7110 | Long-form Identifier | mindat:1:5:7110:3 |
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GUID | 0 |
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Full Reference | Tilley, C. E., Harwood, H. F. (1931) The dolerite-chalk contact of Scawt Hill, Co. Antrim. The production of basic alkali-rocks by the assimilation of limestone by basaltic magma. Mineralogical Magazine and Journal of the Mineralogical Society, 22 (132). 439-468 doi:10.1180/minmag.1931.022.132.02 |
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Plain Text | Tilley, C. E., Harwood, H. F. (1931) The dolerite-chalk contact of Scawt Hill, Co. Antrim. The production of basic alkali-rocks by the assimilation of limestone by basaltic magma. Mineralogical Magazine and Journal of the Mineralogical Society, 22 (132). 439-468 doi:10.1180/minmag.1931.022.132.02 |
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In | (1929) Mineralogical Magazine Vol. 22 (132) Mineralogical Society |
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Abstract/Notes | In the following pages an account is given of the rock assemblages produced at the contact of a dolcrite intrusion with chalk. Owing to the intense localized assimilation of calcium carbonate by the dolerite magma, unusual rock types are produced. The products of the endogenous contact-zone are dealt with in detail. Those of the exogenous contact-zone have in part been described already, but some additional data are incorporated in this account. |
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