| Reference Type | Journal (article/letter/editorial) |
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| Title | Note on the Depth and Temperature of the Gault Sea as indicated by Foraminifera |
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| Journal | Geological Magazine |
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| Authors | Khan, M. H. | Author |
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| Year | 1950 (June) | Volume | 87 |
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| Issue | 3 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800076901 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 247935 | Long-form Identifier | mindat:1:5:247935:8 |
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| GUID | 0 |
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| Full Reference | Khan, M. H. (1950) Note on the Depth and Temperature of the Gault Sea as indicated by Foraminifera. Geological Magazine, 87 (3) 175-180 doi:10.1017/s0016756800076901 |
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| Plain Text | Khan, M. H. (1950) Note on the Depth and Temperature of the Gault Sea as indicated by Foraminifera. Geological Magazine, 87 (3) 175-180 doi:10.1017/s0016756800076901 |
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| In | (1950, June) Geological Magazine Vol. 87 (3) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractForaminiferal evidence in the past has been held to suggest that the Gault is a deep sea deposit—a view which conflicts with the belief held by many on geological and other palaeontological grounds that the Gault was laid down in fairly shallow water. This contradiction is due to a misinterpretation of the foraminiferal evidence which, in the opinion of the writer, favours a temperate, relatively shallow marine environment for the deposition of the Gault, at least in South-East of England. |
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These are possibly similar items as determined by title/reference text matching only.
