| Reference Type | Journal (article/letter/editorial) |
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| Title | Petrology of a Wealden Sandstone at Clock House, Capel, Surrey |
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| Journal | Geological Magazine |
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| Authors | Allen, P. | Author |
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| Year | 1948 (August) | Volume | 85 |
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| Issue | 4 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800073155 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 247744 | Long-form Identifier | mindat:1:5:247744:6 |
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| GUID | 0 |
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| Full Reference | Allen, P. (1948) Petrology of a Wealden Sandstone at Clock House, Capel, Surrey. Geological Magazine, 85 (4) 235-241 doi:10.1017/s0016756800073155 |
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| Plain Text | Allen, P. (1948) Petrology of a Wealden Sandstone at Clock House, Capel, Surrey. Geological Magazine, 85 (4) 235-241 doi:10.1017/s0016756800073155 |
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| In | (1948, August) Geological Magazine Vol. 85 (4) Cambridge University Press (CUP) |
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| Abstract/Notes | The topmost band of sandstone in the Weald Clay at Capel (6) is now exposed for 100 yards, and varies in thickness from 8 inches at the southern end of the face to 1 foot at the northern end. The stone is glauconitic and highly micaceous, and carries so much fresh biotite on certain bedding-planes that they are heavily darkened. Flakes of biotite and muscovite commonly reach 2 mm. in diameter, and occasionally 3 mm. No petrological facies like it is known in the older Hastings Beds outcropping to the south and south-east. The petrography of the sandstone therefore merits description, and some discussion of the problems which it raises. |
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