Olivine-bearing and other basic hornfelses around the insch igneous mass, Aberdeenshire
By: Sadashivaiah, M.S
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Material type: 
ArticleDescription: 121-130p ; Illustration.Subject(s): Olivine bearing - Aberdeenshire - Scotland | Hornfelses - Insch igneous mass - Aberdeenshire - Scotland | Petrogenesis - Scotland | Methamorphic rock - Grampian region - Scotland
In:
Geological magazine : Vol. 87 Iss. 1-6 Year. 1950Summary: Abstract
Basic hornfelses occurring at the contact of slates and olivinenorite are ascribed to influx of Ca, Mg, Fe, Ti, Mn, and P from the gabbro magma into the sedimentary rocks. This kind of basic front, unlike those postulated for acid bodies, has a basic back.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode |
|---|---|---|---|---|---|---|
Article
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Library and Information Centre Periodical Section | Bound Journal Collection | Not for loan | 002560_20 | ||
Serials/Scientific Journal
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Library and Information Centre Periodical Section | Bound Journal Collection | 550 GEO (Browse shelf) | Available | 002560 |
Abstract
Basic hornfelses occurring at the contact of slates and olivinenorite are ascribed to influx of Ca, Mg, Fe, Ti, Mn, and P from the gabbro magma into the sedimentary rocks. This kind of basic front, unlike those postulated for acid bodies, has a basic back.
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