| Reference Type | Journal (article/letter/editorial) |
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| Title | Zeolites of the elinoptilolite–heulandite type in sediments of south-east England |
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| Journal | Mineralogical Magazine |
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| Authors | Brown, G. | Author |
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| Catt, J. A. | Author |
| Weir, A. H. | Author |
| Year | 1969 (December) | Volume | 37 |
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| Issue | 288 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_37/37-288-480.pdf+ |
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| DOI | doi:10.1180/minmag.1969.037.288.08Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6321 | Long-form Identifier | mindat:1:5:6321:4 |
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| GUID | 0 |
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| Full Reference | Brown, G., Catt, J. A., Weir, A. H. (1969) Zeolites of the elinoptilolite–heulandite type in sediments of south-east England. Mineralogical Magazine, 37 (288) 480-488 doi:10.1180/minmag.1969.037.288.08 |
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| Plain Text | Brown, G., Catt, J. A., Weir, A. H. (1969) Zeolites of the elinoptilolite–heulandite type in sediments of south-east England. Mineralogical Magazine, 37 (288) 480-488 doi:10.1180/minmag.1969.037.288.08 |
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| In | (1969, December) Mineralogical Magazine Vol. 37 (288) Mineralogical Society |
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| Abstract/Notes | SummaryClinoptilolite-heulandite is reported from Jurassic, Cretaceous, and Palaeocene sediments in south-east England. It occurs mainly in 1–20 μm size fractions, and is associated with abundant montmorillonite and often also with glauconite and amorphous silica or low-temperature disordered cristobalite-tridymite. Its mode of occurrence and the associated minerals suggest an authigenic origin, but there is no evidence that the source material was volcanic. |
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