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The internal tectonic fabric of minor intrusions and their potential as regional palaeostress indicators

By: Borradaile, Graham J.
Material type: ArticleArticleDescription: 665-671pp ; Illustration.Subject(s): Tectonic fabric | Caledcnides | Inner hebrides | Plutonic rock | Structural geology | Tectonic - United Kingdom In: Geological magazine : Vol. 123 Iss. 1-6 Year. 1986Summary: A suite of late-tectonic minor intrusive rocks in the Inner Hebrides of Scotland show a well developed internal tectonic fabric. This fabric has a similar orientation in adjacent intrusions and it is usually not seen in the wall rock. It is suggested that the intrusions' tectonic fabric records the effects of palaeostress over the cooling period of the intrusions and thus provides palaeostress trajectories over a geologically short period of time over the area occupied by the swarm of intrusions.
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Article Article Library and Information Centre
Periodical Section
Bound Journal Collection Not for loan 002533_141
Serials/Scientific Journal Serials/Scientific Journal Library and Information Centre
Periodical Section
Bound Journal Collection 550 GEO (Browse shelf) Available 002533

A suite of late-tectonic minor intrusive rocks in the Inner Hebrides of Scotland show a well developed internal tectonic fabric. This fabric has a similar orientation in adjacent intrusions and it is usually not seen in the wall rock. It is suggested that the intrusions' tectonic fabric records the effects of palaeostress over the cooling period of the intrusions and thus provides palaeostress trajectories over a geologically short period of time over the area occupied by the swarm of intrusions.

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