Young, B., Dyer, A., Hubbard, N., Starkey, R. E. (1991) Apophyllite and other zeolite-type minerals from the Whin Sill of the northern Pennines. Mineralogical Magazine, 55 (379) 203-207 doi:10.1180/minmag.1991.055.379.08
Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Apophyllite and other zeolite-type minerals from the Whin Sill of the northern Pennines | ||
Journal | Mineralogical Magazine | ISSN | 0026-461X |
Authors | Young, B. | Author | |
Dyer, A. | Author | ||
Hubbard, N. | Author | ||
Starkey, R. E. | Author | ||
Year | 1991 (June) | Volume | 55 |
Page(s) | 203-207 | Issue | 379 |
Publisher | Mineralogical Society | ||
Download URL | https://rruff.info/doclib/MinMag/Volume_55/55-379-203.pdf+ | ||
DOI | doi:10.1180/minmag.1991.055.379.08Search in ResearchGate | ||
Classification | Not set | LoC | Not set |
Mindat Ref. ID | 1716 | Long-form Identifier | mindat:1:5:1716:3 |
GUID | a4dbe7d2-552c-4de1-8e81-2644e055b9ff | ||
Full Reference | Young, B., Dyer, A., Hubbard, N., Starkey, R. E. (1991) Apophyllite and other zeolite-type minerals from the Whin Sill of the northern Pennines. Mineralogical Magazine, 55 (379) 203-207 doi:10.1180/minmag.1991.055.379.08 | ||
Plain Text | Young, B., Dyer, A., Hubbard, N., Starkey, R. E. (1991) Apophyllite and other zeolite-type minerals from the Whin Sill of the northern Pennines. Mineralogical Magazine, 55 (379) 203-207 doi:10.1180/minmag.1991.055.379.08 | ||
In | (1991, June) Mineralogical Magazine Vol. 55 (379) Mineralogical Society | ||
Abstract/Notes | AbstractApophyllite, analcite, chabazite, prehnite and stilbite are described from pectolite-, chlorite-, calcite- and quartz-bearing veins and joint coatings in the late Carboniferous quartz dolerite of the Whin Sill of the northern Pennines. These veins represent the final hydrothermal stages in the sill's emplacement and are not related to the widespread lead-zinc-barium-fluorite mineralization of the northern Pennine orefield. Thermogravimetric studies of apophyllites from the two Whin Sill occurrences reveal that at one locality the mineral is fluorapophyllite, at the other hydroxyapophyllite. |
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