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	<title>Sellafield Member - Revision history</title>
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	<updated>2026-04-16T16:21:49Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<id>http://earthwise-staging.bgs.ac.uk/index.php?title=Sellafield_Member&amp;diff=52991&amp;oldid=prev</id>
		<title>Dbk: 1 revision imported</title>
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		<updated>2021-07-26T15:21:48Z</updated>

		<summary type="html">&lt;p&gt;1 revision imported&lt;/p&gt;
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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 16:21, 26 July 2021&lt;/td&gt;
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		<author><name>Dbk</name></author>
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	<entry>
		<id>http://earthwise-staging.bgs.ac.uk/index.php?title=Sellafield_Member&amp;diff=52990&amp;oldid=prev</id>
		<title>Geosource&gt;BobMcIntosh at 10:33, 27 June 2015</title>
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		<updated>2015-06-27T10:33:18Z</updated>

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&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;== Sellafield Member [http://www.bgs.ac.uk/lexicon/lexicon.cfm?pub=SELF (SELF)]==&lt;br /&gt;
&lt;br /&gt;
=== Previous nomenclature  ===&lt;br /&gt;
* Kirklinton Sandstone (Dixon et al., 1926)&lt;br /&gt;
* Ormskirk Sandstone Formation (Institute of Geological Sciences, 1977)&lt;br /&gt;
&lt;br /&gt;
=== Parent unit  ===&lt;br /&gt;
[[Helsby Sandstone Formation]]&lt;br /&gt;
&lt;br /&gt;
=== Derivation of name  ===&lt;br /&gt;
From the Sellafield area of Cumbria&lt;br /&gt;
&lt;br /&gt;
=== Type section  ===&lt;br /&gt;
NY 04506 00184: Sellafield Borehole 13B, Cumbria. BGS Registered No. NY00SW/42, 0 to 176.42 m.&lt;br /&gt;
&lt;br /&gt;
=== Reference sections  ===&lt;br /&gt;
* NY 0280 0310 to 0255 0274: River Calder, Cumbria (Barnes et al., 1994).&lt;br /&gt;
* NY 034 012: Seascale Scar, Cumbria (Gregory, 1915).&lt;br /&gt;
&lt;br /&gt;
=== Extant exposures/sections  ===&lt;br /&gt;
Very scarce exposures in the Sellafield–Seascale–Drigg area, west Cumbria.&lt;br /&gt;
&lt;br /&gt;
=== Lithology  ===&lt;br /&gt;
The dominant lithology is a red-brown, weathering to orange-brown, fine-grained, well-sorted sandstone with well-rounded grains of aeolian origin. It is commonly cross-bedded. This aeolian dune facies is interbedded with an interdune facies comprising well-cemented, fine-to medium-grained, poorly sorted sandstone with common wavy silty laminae. Small-scale convolutions, loading and dewatering structures are common.&lt;br /&gt;
&lt;br /&gt;
=== Lower boundary  ===&lt;br /&gt;
The lower boundary is taken at the sharp upward change from fine-to coarse-grained fluvial sandstone in the underlying part of the Helsby Sandstone Formation to medium-grained, aeolian sandstone. In borehole geophysical logs it is marked by an upward decrease in gamma-ray values and an upward decrease in sonic velocity. Both log signatures are more serrated than in the underlying part of the Helsby Sandstone Formation.&lt;br /&gt;
&lt;br /&gt;
=== Upper boundary  ===&lt;br /&gt;
The upper boundary is not seen but will be marked by the incoming of dominantly red-brown mudstones and siltstones of the [[Mercia Mudstone Group]].&lt;br /&gt;
&lt;br /&gt;
=== Thickness  ===&lt;br /&gt;
The thickest known sequence is 176.42 m, in the Sellafield 13B Borehole.&lt;br /&gt;
&lt;br /&gt;
=== Age  ===&lt;br /&gt;
Anisian (early Mid Triassic)&lt;br /&gt;
&lt;br /&gt;
=== Equivalent unit ===&lt;br /&gt;
Helsby Sandstone Formation (pars.)  &lt;br /&gt;
=== Geographical extent  ===&lt;br /&gt;
The member only crops out between Drigg and Sellafield on the Cumbrian coast.&lt;br /&gt;
=== Subdivisions  ===&lt;br /&gt;
None&lt;br /&gt;
&lt;br /&gt;
== References ==&lt;br /&gt;
&amp;lt;references/&amp;gt;&lt;br /&gt;
[[Category:Triassic lithostratigraphical nomenclature]]&lt;/div&gt;</summary>
		<author><name>Geosource&gt;BobMcIntosh</name></author>
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