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	<title>File:YGS CHR 04 DINA FIG 08.jpg - Revision history</title>
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	<updated>2026-04-14T14:07:10Z</updated>
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		<title>Scotfot: Scotfot uploaded a new version of File:YGS CHR 04 DINA FIG 08.jpg</title>
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		<updated>2019-08-07T19:41:28Z</updated>

		<summary type="html">&lt;p&gt;Scotfot uploaded a new version of &lt;a href=&quot;/index.php/File:YGS_CHR_04_DINA_FIG_08.jpg&quot; title=&quot;File:YGS CHR 04 DINA FIG 08.jpg&quot;&gt;File:YGS CHR 04 DINA FIG 08.jpg&lt;/a&gt;&lt;/p&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 20:41, 7 August 2019&lt;/td&gt;
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		<id>http://earthwise-staging.bgs.ac.uk/index.php?title=File:YGS_CHR_04_DINA_FIG_08.jpg&amp;diff=41611&amp;oldid=prev</id>
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		<updated>2019-07-31T08:58:56Z</updated>

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|description={{en|1=Figure 8 The palaeogeography of the Lower Limestone Group, highlighting the occurrence of two types of channel sandbody, regular delta distributaries and larger palaeovalleys. The southern extent of the delta progradations is loosely constrained by well data. It seems that a distal deepwater basin was established by this time and that a distinct basin margin was present, across which sand may have been bypassed, particularly during low-stand episodes.&lt;br /&gt;
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|date=2019-07-30 14:15:50&lt;br /&gt;
|source=Yorkshire Geological Society&lt;br /&gt;
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