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                <text>&lt;h2&gt;&lt;strong&gt;L351&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Limestone, mudstone, micrite, chalk&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Upper Cretaceous&lt;br /&gt;&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Melbourn, Cambridge&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Hand Specimen&lt;/h3&gt;
&lt;div class="element-text"&gt;This white rock is virtually pure carbonate. It fizzes with acid. It is fine-grained and poorly cemented, making it soft and low density. It is commonly known as ‘chalk’.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Thin-section&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Very uniform&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/184"&gt;cryptocrystalline&lt;/a&gt;&lt;span&gt; &lt;/span&gt;carbonate.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Rare larger calcite crystals &amp;lt;0.5mm.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock History&lt;/h3&gt;
&lt;div class="element-text"&gt;Very fine-grained, so deposited in a very low energy environment.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Such fine carbonate could have been produced in one of two ways:&lt;br /&gt;1. Tests of calcitic plankton.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;2. Very finely ground shell fragments. Currents alone could not grind the shells this finely. This would require bioerosion – e.g. fish ingesting organisms with carbonate shells, and grinding the carbonate to a fine powder.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Name&lt;/h3&gt;
&lt;div class="element-text"&gt;limestone&lt;br /&gt;mustone&lt;br /&gt;micrite&lt;br /&gt;chalk&lt;/div&gt;
&lt;/div&gt;</text>
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;L350&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Limestone, argillaceous&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Jurassic&lt;/p&gt;
&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Purbeck&lt;br /&gt;Near Salisbury&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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            <description>An account of the resource</description>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Hand Specimen&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Pale yellow-grey mudstone containing the fossil remains of a&lt;span&gt; &lt;/span&gt;&lt;span&gt;small arthropod with a segmented exoskeleton.&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;The rock is banded and shows some surface discolouration due to weathering.&lt;br /&gt;Rock fizzes with acid, so contains carbonate.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;This is a soft, though well consolidated limestone (the surface has been scratched).&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Thin-section&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Moving across the slide, perpendicular to the laminations, there are alternations (gradual transitions) between calcareous mudstone and&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/176"&gt;argillaceous&lt;/a&gt;&lt;span&gt; &lt;/span&gt;limestone. One band is rich in angular quartz grains (0.1 to 0.2 mm), and contains carbonate shell fragments.&lt;/p&gt;
&lt;p&gt;Calcite mudstone – fine-grained mosaic of calcite, small proportion of transparent brown impurity and a few small grains of quartz.&lt;/p&gt;
&lt;p&gt;Argillaceous limestone – even finer grained calcite mosaic, more abundant brown material (probably organic) than in the calcite mudstone.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock History&lt;/h3&gt;
&lt;div class="element-text"&gt;Low energy, aqueous environment.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced Notes&lt;/h3&gt;
&lt;div class="element-text"&gt;The fossil remains are those of Archaeoniscus, a small crustacean (which belongs to the arthropods), of supposed freshwater origin. With this extra knowledge it may be inferred that the rock was deposited in fresh water.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Name&lt;/h3&gt;
&lt;div class="element-text"&gt;argillaceous limestone&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>aqueous</name>
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;L341&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Mudstone, calcareous&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Lower Carboniferous&lt;/p&gt;
&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Millstone Grit Series&lt;br /&gt;Bowland, West Yorkshire&lt;/p&gt;
&lt;/div&gt;
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            <description>An account of the resource</description>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Hand Specimen&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Very dark grey to black mudstone.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Faint, fine-scale laminations visible on cut surface.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Not&lt;span&gt; &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/196"&gt;fissile&lt;/a&gt;&lt;span&gt; &lt;/span&gt;- does not readily split along bedding planes.&lt;br /&gt;Contains fossils and fossil imprints.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Some glinting flakes of mica.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;This rock fizzes gently with acid, indicating that it contains some carbonate.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Weathered to light brown-grey in places.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Thin-section&lt;/h3&gt;
&lt;div class="element-text"&gt;Laminations are very clear when the thin-section is held up to the light. They are mainly planar, but some wrap around lighter regions in the rock.&lt;br /&gt;&lt;br /&gt;Under the microscope, the rock is brown, with fine dark brown streaks, laminated.&lt;br /&gt;Mainly carbonate, some white mica, rare quartz.&lt;br /&gt;Bioclasts, mainly along bedding surfaces, probably gastropods and bivalves. Some of the shells have been dissolved. The spaces left have been filled by secondary calcite.&lt;br /&gt;Sparry carbonate cement.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock History&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Fine-grained, so formed in a very low energy environment.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Shells are too large to have been swept in by such low energy currents, so the shells are in life position.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;If the shells are indeed gastropods and bivalves the rock could be marine or non-marine. The presence of brachiopods&lt;span&gt; &lt;/span&gt;&lt;em&gt;would&lt;/em&gt;&lt;span&gt; &lt;/span&gt;indicate a marine environment.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Name&lt;/h3&gt;
&lt;div class="element-text"&gt;calcareous mudstone&lt;/div&gt;
&lt;/div&gt;</text>
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