"host-rock" meaning in All languages combined

{
  "forms": [
    {
      "form": "host-rocks",
      "tags": [
        "plural"
      ]
    }
  ],
  "head_templates": [
    {
      "args": {
        "1": "~"
      },
      "expansion": "host-rock (countable and uncountable, plural host-rocks)",
      "name": "en-noun"
    }
  ],
  "lang": "English",
  "lang_code": "en",
  "pos": "noun",
  "senses": [
    {
      "alt_of": [
        {
          "word": "host rock"
        }
      ],
      "categories": [
        {
          "kind": "other",
          "name": "English entries with incorrect language header",
          "parents": [
            "Entries with incorrect language header",
            "Entry maintenance"
          ],
          "source": "w"
        },
        {
          "kind": "other",
          "name": "Pages with 1 entry",
          "parents": [],
          "source": "w"
        },
        {
          "kind": "other",
          "name": "Pages with entries",
          "parents": [],
          "source": "w"
        }
      ],
      "examples": [
        {
          "ref": "1968, Transactions of the Geological Society of South Africa, page 148:",
          "text": "Their exact relationship to the host-rock is obscure but from their texture and observed metamorphic relationship they are thought to be intrusive dykes rather than intercalations of more basic lava.",
          "type": "quote"
        },
        {
          "ref": "2007, Olivier Lacombe, Jérôme Lavé, Francois M. Roure, Thrust Belts and Foreland Basins, page 99:",
          "text": "The column dif δ¹⁸O indicates the difference between de δ¹⁸O of the calcite cement in the veins and its adjacent host-rock.",
          "type": "quote"
        },
        {
          "ref": "2019, S. Ferrero, P. Lanari, P. Goncalves, Metamorphic Geology: Microscale to Mountain Belts, page 72:",
          "text": "We simplify the concept of thermodynamic equilibrium by assuming that 100% of the melt will be in thermodynamic equilibrium with a fixed weight fraction of the host-rock it travels through.",
          "type": "quote"
        }
      ],
      "glosses": [
        "Alternative form of host rock"
      ],
      "id": "en-host-rock-en-noun-gKusINcq",
      "links": [
        [
          "host rock",
          "host rock#English"
        ]
      ],
      "tags": [
        "alt-of",
        "alternative",
        "countable",
        "uncountable"
      ]
    }
  ],
  "word": "host-rock"
}

{
  "forms": [
    {
      "form": "host-rocks",
      "tags": [
        "plural"
      ]
    }
  ],
  "head_templates": [
    {
      "args": {
        "1": "~"
      },
      "expansion": "host-rock (countable and uncountable, plural host-rocks)",
      "name": "en-noun"
    }
  ],
  "lang": "English",
  "lang_code": "en",
  "pos": "noun",
  "senses": [
    {
      "alt_of": [
        {
          "word": "host rock"
        }
      ],
      "categories": [
        "English countable nouns",
        "English entries with incorrect language header",
        "English lemmas",
        "English multiword terms",
        "English nouns",
        "English terms with quotations",
        "English uncountable nouns",
        "Pages with 1 entry",
        "Pages with entries"
      ],
      "examples": [
        {
          "ref": "1968, Transactions of the Geological Society of South Africa, page 148:",
          "text": "Their exact relationship to the host-rock is obscure but from their texture and observed metamorphic relationship they are thought to be intrusive dykes rather than intercalations of more basic lava.",
          "type": "quote"
        },
        {
          "ref": "2007, Olivier Lacombe, Jérôme Lavé, Francois M. Roure, Thrust Belts and Foreland Basins, page 99:",
          "text": "The column dif δ¹⁸O indicates the difference between de δ¹⁸O of the calcite cement in the veins and its adjacent host-rock.",
          "type": "quote"
        },
        {
          "ref": "2019, S. Ferrero, P. Lanari, P. Goncalves, Metamorphic Geology: Microscale to Mountain Belts, page 72:",
          "text": "We simplify the concept of thermodynamic equilibrium by assuming that 100% of the melt will be in thermodynamic equilibrium with a fixed weight fraction of the host-rock it travels through.",
          "type": "quote"
        }
      ],
      "glosses": [
        "Alternative form of host rock"
      ],
      "links": [
        [
          "host rock",
          "host rock#English"
        ]
      ],
      "tags": [
        "alt-of",
        "alternative",
        "countable",
        "uncountable"
      ]
    }
  ],
  "word": "host-rock"
}