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	<title>Geology of the Aberfoyle district: Minor intrusions - Revision history</title>
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	<updated>2026-04-17T15:05:31Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<updated>2021-07-29T12:57:55Z</updated>

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				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 13:57, 29 July 2021&lt;/td&gt;
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		<title>Geosource&gt;Ajhil: Created page with &quot;{{AberfoyleSD}} Minor intrusions are common in the Aberfoyle district, particularly to the north of the Highland Boundary Fault. They comprise mafic to felsic dykes, sheets an...&quot;</title>
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		<updated>2016-08-04T13:04:54Z</updated>

		<summary type="html">&lt;p&gt;Created page with &amp;quot;{{AberfoyleSD}} Minor intrusions are common in the Aberfoyle district, particularly to the north of the Highland Boundary Fault. They comprise mafic to felsic dykes, sheets an...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;{{AberfoyleSD}}&lt;br /&gt;
Minor intrusions are common in the Aberfoyle district, particularly to the north of the Highland Boundary Fault. They comprise mafic to felsic dykes, sheets and sills, ranging in age from Neoproterozoic to Palaeogene. The oldest predate the Caledonian Orogeny and are deformed and metamorphosed, manifest now as amphibolites.&lt;br /&gt;
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== Geology of the Aberfoyle district - contents ==&lt;br /&gt;
{{Aberfoylepages}}&lt;br /&gt;
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[[category:Aberfoyle - the geology of the district| 18]]&lt;/div&gt;</summary>
		<author><name>Geosource&gt;Ajhil</name></author>
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