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Walters, S. G., Ineson, P. R. (1983) Clay minerals in the basalts of the South Pennines. Mineralogical Magazine, 47 (342) 21-26 doi:10.1180/minmag.1983.047.342.03

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Reference TypeJournal (article/letter/editorial)
TitleClay minerals in the basalts of the South Pennines
JournalMineralogical MagazineISSN0026-461X
AuthorsWalters, S. G.Author
Ineson, P. R.Author
Year1983 (March)Volume47
Page(s)21-26Issue342
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_47/47-342-21.pdf+
DOIdoi:10.1180/minmag.1983.047.342.03Search in ResearchGate
Mindat Ref. ID3465Long-form Identifiermindat:1:5:3465:8
GUIDd67c97cf-8726-425a-986f-b6514eb85629
Full ReferenceWalters, S. G., Ineson, P. R. (1983) Clay minerals in the basalts of the South Pennines. Mineralogical Magazine, 47 (342) 21-26 doi:10.1180/minmag.1983.047.342.03
Plain TextWalters, S. G., Ineson, P. R. (1983) Clay minerals in the basalts of the South Pennines. Mineralogical Magazine, 47 (342) 21-26 doi:10.1180/minmag.1983.047.342.03
In(1983, March) Mineralogical Magazine Vol. 47 (342) Mineralogical Society
Abstract/NotesAbstractX-ray diffraction, electron microprobe and STEM EDAX analyses of basalts from the South Pennines (Derbyshire) indicate that Fe-rich smectites are the dominant alteration products, occurring either as pseudomorphs or infilling veins and vesicles. Previously chlorite has been identified as the common alteration product but its occurrence is very infrequent.


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