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	<title>Enterkin Mudstone Formation - Revision history</title>
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		<id>http://earthwise-staging.bgs.ac.uk/index.php?title=Enterkin_Mudstone_Formation&amp;diff=52744&amp;oldid=prev</id>
		<title>Geosource&gt;Volunteer 01 at 12:22, 7 July 2015</title>
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&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;==Enterkin Mudstone Formation [http://www.bgs.ac.uk/lexicon/lexicon.cfm?pub=ENT (ENT)], Carboniferous, Midland Valley of Scotland ==&lt;br /&gt;
Enterkin Mudstone Formation is part of the [[Clackmannan Group]]&lt;br /&gt;
=== Name ===&lt;br /&gt;
From Enterkin Burn, north of Carronbridge, Dumfries and Galloway. Defined as a formation by McMillan (2002&amp;lt;ref name=&amp;quot;Mcmillan02&amp;quot;&amp;gt;McMillan, A A.2002.Geology of the New Galloway and Thornhill district.&amp;#039;&amp;#039;Memoir of the British Geological Survey&amp;#039;&amp;#039;, Sheets 9E and 9W (Scotland).&amp;lt;/ref&amp;gt;; see also Simpson and Richey, 1936&amp;lt;ref name=&amp;quot;SandR36&amp;quot;&amp;gt;Simpson, J B, and Richey, J E.1936.The geology of the Sanquhar coalfield and adjacent basin of Thornhill.&amp;#039;&amp;#039;Memoir of the Geological Survey of Great Britain&amp;#039;&amp;#039;, Sheets part 9 and 15 (Scotland)&amp;lt;/ref&amp;gt;).&lt;br /&gt;
&lt;br /&gt;
=== Lithology ===&lt;br /&gt;
The formation consists dominantly of purple-grey mudstone and siltstone with interbedded sandstone.&lt;br /&gt;
&lt;br /&gt;
=== Genetic interpretation ===&lt;br /&gt;
This &amp;#039;&amp;#039;mixed shelf carbonate and deltaic (‘Yoredale’) facies &amp;#039;&amp;#039;unit formed in a marine–intertidal environment. The mudstones contain a marine fauna.&lt;br /&gt;
&lt;br /&gt;
=== Stratotype ===&lt;br /&gt;
The type section is in the Enterkin Burn (NS 8706 0526) where up to 15 m of interbedded red-brown and purple mudstone and siltstone, and purplish red sandstone and seatearth are exposed (McMillan, 2002&amp;lt;ref name=&amp;quot;Mcmillan02&amp;quot;&amp;gt;&amp;lt;/ref&amp;gt;; Simpson and Richey, 1936, table 3&amp;lt;ref name=&amp;quot;SandR36&amp;quot;&amp;gt;&amp;lt;/ref&amp;gt;).&lt;br /&gt;
&lt;br /&gt;
=== Lower and upper boundaries ===&lt;br /&gt;
The base of the formation is unconformable on the mainly sandstone-dominated turbidites of the Ordovician Glenlee Formation, Leadhills Supergroup.&lt;br /&gt;
&lt;br /&gt;
The top of the formation is conformable with the base of the Scottish Lower Coal Measures Formation (Figure 6, Column 6) comprising sandstones, siltstones and mudstones, with seatearths.&lt;br /&gt;
&lt;br /&gt;
=== Thickness ===&lt;br /&gt;
Up to 15 m of the formation are exposed at the type section in the Enterkin Burn (NS 8706 0526) (McMillan, 2002&amp;lt;ref name=&amp;quot;Mcmillan02&amp;quot;&amp;gt;&amp;lt;/ref&amp;gt;; Simpson and Richey, 1936, table 3&amp;lt;ref name=&amp;quot;SandR36&amp;quot;&amp;gt;&amp;lt;/ref&amp;gt;).&lt;br /&gt;
&lt;br /&gt;
=== Distribution and regional correlation ===&lt;br /&gt;
The formation is restricted to the Thornhill Basin. The mudstones contain a fauna, that suggests possible correlation with the Clackmannan Group (undivided) Visean strata of the Sanquhar Basin.&lt;br /&gt;
&lt;br /&gt;
=== Age and biostratigraphical characterisation ===&lt;br /&gt;
Visean to Namurian (Brigantian to early Pendleian). The mudstones contain a brachiopod, bivalve and nautiloid fauna, which may be of similar age to the fauna of the Closeburn Limestone Formation.&lt;br /&gt;
&lt;br /&gt;
== References ==&lt;br /&gt;
&amp;lt;references/&amp;gt;&lt;br /&gt;
[[Category:Carboniferous lithostratigraphical nomenclature]]&lt;/div&gt;</summary>
		<author><name>Geosource&gt;Volunteer 01</name></author>
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