"intracrustal" meaning in English

{
  "etymology_templates": [
    {
      "args": {
        "1": "en",
        "2": "intra",
        "3": "crustal"
      },
      "expansion": "intra- + crustal",
      "name": "prefix"
    }
  ],
  "etymology_text": "From intra- + crustal.",
  "head_templates": [
    {
      "args": {
        "1": "-"
      },
      "expansion": "intracrustal (not comparable)",
      "name": "en-adj"
    }
  ],
  "lang": "English",
  "lang_code": "en",
  "pos": "adj",
  "senses": [
    {
      "categories": [
        {
          "kind": "other",
          "name": "English entries with incorrect language header",
          "parents": [
            "Entries with incorrect language header",
            "Entry maintenance"
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          "source": "w"
        },
        {
          "kind": "other",
          "name": "English terms prefixed with intra-",
          "parents": [],
          "source": "w"
        },
        {
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          "name": "Pages with 1 entry",
          "parents": [],
          "source": "w"
        },
        {
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          "source": "w"
        }
      ],
      "examples": [
        {
          "ref": "1998 November 6, J. C. Savage et al., “Detecting Strain in the Yucca Mountain Area, Nevada”, in Science, volume 282, number 5391, →DOI:",
          "text": "There are two main mechanisms that govern postseismic deformation: (i) viscoelastic relaxation in an intracrustal asthenospheric layer (4 ) and (ii) afterslip in a velocity-strengthening region above the coseismic rupture zone (5 ).",
          "type": "quote"
        }
      ],
      "glosses": [
        "inside or within crusts"
      ],
      "id": "en-intracrustal-en-adj-1ps4X0Bo",
      "links": [
        [
          "crust",
          "crust"
        ]
      ],
      "tags": [
        "not-comparable"
      ]
    }
  ],
  "word": "intracrustal"
}

{
  "etymology_templates": [
    {
      "args": {
        "1": "en",
        "2": "intra",
        "3": "crustal"
      },
      "expansion": "intra- + crustal",
      "name": "prefix"
    }
  ],
  "etymology_text": "From intra- + crustal.",
  "head_templates": [
    {
      "args": {
        "1": "-"
      },
      "expansion": "intracrustal (not comparable)",
      "name": "en-adj"
    }
  ],
  "lang": "English",
  "lang_code": "en",
  "pos": "adj",
  "senses": [
    {
      "categories": [
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        "English entries with incorrect language header",
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        "English terms prefixed with intra-",
        "English terms with quotations",
        "English uncomparable adjectives",
        "Pages with 1 entry",
        "Pages with entries"
      ],
      "examples": [
        {
          "ref": "1998 November 6, J. C. Savage et al., “Detecting Strain in the Yucca Mountain Area, Nevada”, in Science, volume 282, number 5391, →DOI:",
          "text": "There are two main mechanisms that govern postseismic deformation: (i) viscoelastic relaxation in an intracrustal asthenospheric layer (4 ) and (ii) afterslip in a velocity-strengthening region above the coseismic rupture zone (5 ).",
          "type": "quote"
        }
      ],
      "glosses": [
        "inside or within crusts"
      ],
      "links": [
        [
          "crust",
          "crust"
        ]
      ],
      "tags": [
        "not-comparable"
      ]
    }
  ],
  "word": "intracrustal"
}