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    <loc>https://www.newmanenergyresearch.com/virf</loc>
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    <priority>0.75</priority>
    <lastmod>2020-11-22</lastmod>
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      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/591b9469ff7c50aaa2d951a8/1494979731441/</image:loc>
      <image:title>VIRF - In this North American example the VR analyst classified their measurements into perhydrous vitrinite, normal vitrinite, and inertinite based on a subjective assessment of morphology. Virf analysis reveals that the vitrinite of normal chemistry has been attributed to inertinite, resulting in a reflectance value that is more than 0.4% too low.</image:title>
    </image:image>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/58e6de6fbf629a14bc66b12d/1497402390679/</image:loc>
      <image:title>VIRF - In this image two coals have been mounted side by side and polished. The coal on the left has VR 1.8%, the coal on the right has VR 0.6%.</image:title>
      <image:caption>Incident light, Oil Immersion.</image:caption>
    </image:image>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/5fbae3d0caf0401020009cf7/1606083550343/map+test+2.jpg</image:loc>
      <image:title>VIRF</image:title>
    </image:image>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/58e6e9c1d2b85764df60092c/1491528142350/</image:loc>
      <image:title>VIRF</image:title>
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    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/5940a22503596ed295dc69a1/1497408052360/</image:loc>
      <image:title>VIRF</image:title>
    </image:image>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/58e6e9128419c2d7b981ec01/1496284980064/</image:loc>
      <image:title>VIRF - As an example, many analysts would identify this subject as vitrinite. However, the sample is a Cambrian oil shale that was deposited long before land plants began to evolve.</image:title>
      <image:caption>Incident light, Oil Immersion</image:caption>
    </image:image>
    <image:image>
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      <image:title>VIRF</image:title>
    </image:image>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/58e6eb60c534a5de6cf850cc/1498432412853/</image:loc>
      <image:title>VIRF - VIRF defines a complex maturity profile for the Clipper-1 well (Canterbury Basin, New Zealand). This is attributed to hydrothermal activity driven by igneous intrusion. VIRF suggests that the VR analysts who originally analysed samples from Clipper-1 selectively measured caved and perhydrous vitrinite. Indigenous vitrinite with normal chemisty was likely assigned to inertinite or reworked vitrinite.</image:title>
    </image:image>
    <image:image>
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      <image:title>VIRF</image:title>
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  <url>
    <loc>https://www.newmanenergyresearch.com/home</loc>
    <changefreq>daily</changefreq>
    <priority>1.0</priority>
    <lastmod>2020-04-16</lastmod>
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      <image:title>Petrographic analysis, research and consultation</image:title>
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    <image:image>
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      <image:title>Petrographic analysis, research and consultation</image:title>
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  <url>
    <loc>https://www.newmanenergyresearch.com/preparation</loc>
    <changefreq>daily</changefreq>
    <priority>0.75</priority>
    <lastmod>2017-06-14</lastmod>
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      <image:title>Sample Preparation</image:title>
      <image:caption>Acicular and plumose crystals of an opaque oxide mineral associated with devitrified vesicular igneous glass</image:caption>
    </image:image>
    <image:image>
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      <image:title>Sample Preparation</image:title>
      <image:caption>Graphite polished perpendicular to layering</image:caption>
    </image:image>
    <image:image>
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      <image:title>Sample Preparation</image:title>
      <image:caption>Thermally altered dispersed organic matter</image:caption>
    </image:image>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/58f6a58b46c3c424ad73305f/1532561863782/</image:loc>
      <image:title>Sample Preparation</image:title>
    </image:image>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/59029f7659cc6847c0e10a08/1532561863771/</image:loc>
      <image:title>Sample Preparation</image:title>
      <image:caption>Polished Salt crystals viewed with electron scanning microscope</image:caption>
    </image:image>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/58e593e03e00be09006bad69/1456938939229/header-woodhouse-JessieWebster_Treehouse_22.jpg</image:loc>
      <image:title>Sample Preparation</image:title>
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  </url>
  <url>
    <loc>https://www.newmanenergyresearch.com/consultation</loc>
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    <priority>0.75</priority>
    <lastmod>2017-04-06</lastmod>
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  <url>
    <loc>https://www.newmanenergyresearch.com/contact</loc>
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    <priority>0.75</priority>
    <lastmod>2017-04-21</lastmod>
  </url>
  <url>
    <loc>https://www.newmanenergyresearch.com/research</loc>
    <changefreq>daily</changefreq>
    <priority>0.75</priority>
    <lastmod>2017-06-26</lastmod>
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      <image:title>Petrographic evidence for hydrothermal and magmatic controls on petroleum systems</image:title>
    </image:image>
    <image:image>
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      <image:title>Petrographic evidence for hydrothermal and magmatic controls on petroleum systems</image:title>
    </image:image>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/5950848ae58c62475796a809/1498449071124/</image:loc>
      <image:title>Petrographic evidence for hydrothermal and magmatic controls on petroleum systems</image:title>
    </image:image>
    <image:image>
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      <image:title>Petrographic evidence for hydrothermal and magmatic controls on petroleum systems</image:title>
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    <image:image>
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      <image:title>Petrographic evidence for hydrothermal and magmatic controls on petroleum systems</image:title>
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  <url>
    <loc>https://www.newmanenergyresearch.com/sample-preparation</loc>
    <changefreq>daily</changefreq>
    <priority>0.75</priority>
    <lastmod>2021-02-22</lastmod>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/5b5909c78a922d06e012496d/1496284198471/Montage.jpg</image:loc>
      <image:title>Petrographic Analysis of Coals</image:title>
      <image:caption>Thermally altered dispersed organic matter</image:caption>
    </image:image>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/5b5909c78a922d06e012496b/1492561250234/Polished+mineral+oxides</image:loc>
      <image:title>Petrographic Analysis of Coals</image:title>
      <image:caption>Acicular and plumose crystals of an opaque oxide mineral associated with devitrified vesicular igneous glass</image:caption>
    </image:image>
    <image:image>
      <image:loc>https://static1.squarespace.com/static/58cb23f7f5e2316b91fd4183/t/5b5909c78a922d06e012496f/1492559256800/</image:loc>
      <image:title>Petrographic Analysis of Coals</image:title>
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    <image:image>
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      <image:title>Petrographic Analysis of Coals</image:title>
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