"Wetherill diagram" meaning in English

{
  "etymology_text": "Named after American physicist George Wetherill. From circa 1956.",
  "forms": [
    {
      "form": "Wetherill diagrams",
      "tags": [
        "plural"
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      "expansion": "Wetherill diagram (plural Wetherill diagrams)",
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  "lang": "English",
  "lang_code": "en",
  "pos": "noun",
  "senses": [
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          "kind": "other",
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          "langcode": "en",
          "name": "Geology",
          "orig": "en:Geology",
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            "Fundamental"
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          "source": "w"
        }
      ],
      "examples": [
        {
          "text": "The \"x\" and \"y\" axes of the Wetherill diagram are the quantities of the respective end (lead) isotopes of the actinium series and uranium series decay chains, each adjusted and expressed as a ratio to the amount remaining of the corresponding start (uranium) isotope.",
          "type": "example"
        },
        {
          "text": "In the Wetherill diagram, no isotope is found on both axes, allowing the two decay schemes to be evaluated independently.",
          "type": "example"
        },
        {
          "ref": "1983, Lazarus J. Salop, translated by V. P. Grudina, Geological Evolution of the Earth During the Precambrian, Springer, page 50:",
          "text": "However, these workers suggest that the age of the Amitsoq gneisses is closer to the true one when determined by the U-Th-Pb method on zircons, and the zircon isochron on the Wetherill diagram crosses the concordia in the point corresponding to 3600 m.y.",
          "type": "quote"
        },
        {
          "ref": "2014, K. Stephen Hughes et al., “2: Geology, Geochemistry and Geochronology of the western Piedmont of northern Virginia”, in Christopher M. Bailey, Lorrie V. Coiner, editors, Elevating Geoscience in the Southeastern United States, Geological Society of America, page 57:",
          "text": "The fifth analysis shows signs of Pb loss and plots below the concordia line on the Wetherill diagram.",
          "type": "quote"
        },
        {
          "text": "2020, Myint Myat Phyo, et al., U—Pb Dating of Zircon and Zirconolite Inclusions in Marble-Hosted Gem-Quality Ruby and Spinel from Mogok, Myanmar, Frederick Lin Sutherland, Khin Zaw (editors), Mineralogy and Geochemistry of Ruby, MDPI Books, page 115,\nFigure 4. Wetherill diagrams showing wide range of U-Pb age of (a) zircon inclusion in gem-quality ruby and spinel, (b) accessory zircon in Bawlongyi marble, (c) zirconolite inclusion in ruby from Mansin and (d) zirconolite intergrown with zircon in Bawlongyi marble."
        }
      ],
      "glosses": [
        "A type of concordia diagram, used in the context of uranium–lead dating, whose axes are the ratios ²⁰⁶Pb/²³⁸U and ²³⁷Pb/²³⁵Pb."
      ],
      "id": "en-Wetherill_diagram-en-noun-3cdtiLIr",
      "links": [
        [
          "geology",
          "geology"
        ],
        [
          "concordia diagram",
          "concordia diagram"
        ]
      ],
      "raw_glosses": [
        "(geology, geochronology) A type of concordia diagram, used in the context of uranium–lead dating, whose axes are the ratios ²⁰⁶Pb/²³⁸U and ²³⁷Pb/²³⁵Pb."
      ],
      "synonyms": [
        {
          "word": "Wetherill concordia diagram"
        }
      ],
      "topics": [
        "geography",
        "geology",
        "natural-sciences"
      ],
      "translations": [
        {
          "code": "fr",
          "lang": "French",
          "sense": "type of concordia diagram",
          "tags": [
            "masculine"
          ],
          "word": "diagramme de Wetherill"
        },
        {
          "code": "de",
          "lang": "German",
          "sense": "type of concordia diagram",
          "tags": [
            "neuter"
          ],
          "word": "Wetherill-Diagramm"
        }
      ],
      "wikipedia": [
        "George Wetherill"
      ]
    }
  ],
  "word": "Wetherill diagram"
}

{
  "etymology_text": "Named after American physicist George Wetherill. From circa 1956.",
  "forms": [
    {
      "form": "Wetherill diagrams",
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        "Terms with French translations",
        "Terms with German translations",
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      "examples": [
        {
          "text": "The \"x\" and \"y\" axes of the Wetherill diagram are the quantities of the respective end (lead) isotopes of the actinium series and uranium series decay chains, each adjusted and expressed as a ratio to the amount remaining of the corresponding start (uranium) isotope.",
          "type": "example"
        },
        {
          "text": "In the Wetherill diagram, no isotope is found on both axes, allowing the two decay schemes to be evaluated independently.",
          "type": "example"
        },
        {
          "ref": "1983, Lazarus J. Salop, translated by V. P. Grudina, Geological Evolution of the Earth During the Precambrian, Springer, page 50:",
          "text": "However, these workers suggest that the age of the Amitsoq gneisses is closer to the true one when determined by the U-Th-Pb method on zircons, and the zircon isochron on the Wetherill diagram crosses the concordia in the point corresponding to 3600 m.y.",
          "type": "quote"
        },
        {
          "ref": "2014, K. Stephen Hughes et al., “2: Geology, Geochemistry and Geochronology of the western Piedmont of northern Virginia”, in Christopher M. Bailey, Lorrie V. Coiner, editors, Elevating Geoscience in the Southeastern United States, Geological Society of America, page 57:",
          "text": "The fifth analysis shows signs of Pb loss and plots below the concordia line on the Wetherill diagram.",
          "type": "quote"
        },
        {
          "text": "2020, Myint Myat Phyo, et al., U—Pb Dating of Zircon and Zirconolite Inclusions in Marble-Hosted Gem-Quality Ruby and Spinel from Mogok, Myanmar, Frederick Lin Sutherland, Khin Zaw (editors), Mineralogy and Geochemistry of Ruby, MDPI Books, page 115,\nFigure 4. Wetherill diagrams showing wide range of U-Pb age of (a) zircon inclusion in gem-quality ruby and spinel, (b) accessory zircon in Bawlongyi marble, (c) zirconolite inclusion in ruby from Mansin and (d) zirconolite intergrown with zircon in Bawlongyi marble."
        }
      ],
      "glosses": [
        "A type of concordia diagram, used in the context of uranium–lead dating, whose axes are the ratios ²⁰⁶Pb/²³⁸U and ²³⁷Pb/²³⁵Pb."
      ],
      "links": [
        [
          "geology",
          "geology"
        ],
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          "concordia diagram",
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      ],
      "raw_glosses": [
        "(geology, geochronology) A type of concordia diagram, used in the context of uranium–lead dating, whose axes are the ratios ²⁰⁶Pb/²³⁸U and ²³⁷Pb/²³⁵Pb."
      ],
      "topics": [
        "geography",
        "geology",
        "natural-sciences"
      ],
      "wikipedia": [
        "George Wetherill"
      ]
    }
  ],
  "synonyms": [
    {
      "word": "Wetherill concordia diagram"
    }
  ],
  "translations": [
    {
      "code": "fr",
      "lang": "French",
      "sense": "type of concordia diagram",
      "tags": [
        "masculine"
      ],
      "word": "diagramme de Wetherill"
    },
    {
      "code": "de",
      "lang": "German",
      "sense": "type of concordia diagram",
      "tags": [
        "neuter"
      ],
      "word": "Wetherill-Diagramm"
    }
  ],
  "word": "Wetherill diagram"
}

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