"simatic" meaning in English

See simatic in All languages combined, or Wiktionary

Adjective

Etymology: From sima + -ic. Etymology templates: {{suf|en|sima|ic}} sima + -ic Head templates: {{en-adj|-}} simatic (not comparable)
  1. (petrology) Composed predominantly of silica-bearing, magnesia-bearing, and ferriferous minerals such as olivine, pyroxene, amphibole, and biotite. Tags: not-comparable Categories (topical): Petrology Synonyms: mafic, ferromagnesic, basic

Download JSON data for simatic meaning in English (2.4kB)

{
  "etymology_templates": [
    {
      "args": {
        "1": "en",
        "2": "sima",
        "3": "ic"
      },
      "expansion": "sima + -ic",
      "name": "suf"
    }
  ],
  "etymology_text": "From sima + -ic.",
  "head_templates": [
    {
      "args": {
        "1": "-"
      },
      "expansion": "simatic (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"
          ],
          "source": "w"
        },
        {
          "kind": "other",
          "name": "English terms suffixed with -ic",
          "parents": [],
          "source": "w"
        },
        {
          "kind": "topical",
          "langcode": "en",
          "name": "Petrology",
          "orig": "en:Petrology",
          "parents": [
            "Geology",
            "Earth sciences",
            "Sciences",
            "All topics",
            "Fundamental"
          ],
          "source": "w"
        }
      ],
      "examples": [
        {
          "text": "Coordinate term: sialic"
        },
        {
          "text": "Near-synonym: ensimatic"
        },
        {
          "ref": "1977, Robert F. Mueller & Surendra K. Saxena, Chemical Petrology: with applications to The Terrestrial Planets and Meteorites, Springer-Verlag, →DOI, page 110",
          "text": "In this process the sial is squeezed out laterally and forms the nuclei of continents, while the subsided region becomes an ocean basin. Thereafter the low-lying basins. which are comprised of solid basic or simatic material. continue to attract basic volcanism because the basic lavas are lighter than their solid counterparts. On the other hand. the high-standing sialic continents largely prevent the extrusion of basic lavas on their surfaces because they are less dense on the average than the basic magmas. By these mechanisms the continents and ocean basins are preserved and continue to grow.",
          "type": "quotation"
        }
      ],
      "glosses": [
        "Composed predominantly of silica-bearing, magnesia-bearing, and ferriferous minerals such as olivine, pyroxene, amphibole, and biotite."
      ],
      "id": "en-simatic-en-adj-hnlZ4Qph",
      "links": [
        [
          "petrology",
          "petrology"
        ],
        [
          "silica",
          "silica"
        ],
        [
          "magnesia",
          "magnesia"
        ],
        [
          "ferriferous",
          "ferriferous"
        ],
        [
          "minerals",
          "mineral"
        ],
        [
          "olivine",
          "olivine"
        ],
        [
          "pyroxene",
          "pyroxene"
        ],
        [
          "amphibole",
          "amphibole"
        ],
        [
          "biotite",
          "biotite"
        ]
      ],
      "raw_glosses": [
        "(petrology) Composed predominantly of silica-bearing, magnesia-bearing, and ferriferous minerals such as olivine, pyroxene, amphibole, and biotite."
      ],
      "synonyms": [
        {
          "word": "mafic"
        },
        {
          "word": "ferromagnesic"
        },
        {
          "word": "basic"
        }
      ],
      "tags": [
        "not-comparable"
      ],
      "topics": [
        "geography",
        "geology",
        "natural-sciences",
        "petrology"
      ]
    }
  ],
  "word": "simatic"
}
{
  "etymology_templates": [
    {
      "args": {
        "1": "en",
        "2": "sima",
        "3": "ic"
      },
      "expansion": "sima + -ic",
      "name": "suf"
    }
  ],
  "etymology_text": "From sima + -ic.",
  "head_templates": [
    {
      "args": {
        "1": "-"
      },
      "expansion": "simatic (not comparable)",
      "name": "en-adj"
    }
  ],
  "lang": "English",
  "lang_code": "en",
  "pos": "adj",
  "senses": [
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        "English entries with incorrect language header",
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        "English terms suffixed with -ic",
        "English terms with quotations",
        "English uncomparable adjectives",
        "en:Petrology"
      ],
      "examples": [
        {
          "text": "Coordinate term: sialic"
        },
        {
          "text": "Near-synonym: ensimatic"
        },
        {
          "ref": "1977, Robert F. Mueller & Surendra K. Saxena, Chemical Petrology: with applications to The Terrestrial Planets and Meteorites, Springer-Verlag, →DOI, page 110",
          "text": "In this process the sial is squeezed out laterally and forms the nuclei of continents, while the subsided region becomes an ocean basin. Thereafter the low-lying basins. which are comprised of solid basic or simatic material. continue to attract basic volcanism because the basic lavas are lighter than their solid counterparts. On the other hand. the high-standing sialic continents largely prevent the extrusion of basic lavas on their surfaces because they are less dense on the average than the basic magmas. By these mechanisms the continents and ocean basins are preserved and continue to grow.",
          "type": "quotation"
        }
      ],
      "glosses": [
        "Composed predominantly of silica-bearing, magnesia-bearing, and ferriferous minerals such as olivine, pyroxene, amphibole, and biotite."
      ],
      "links": [
        [
          "petrology",
          "petrology"
        ],
        [
          "silica",
          "silica"
        ],
        [
          "magnesia",
          "magnesia"
        ],
        [
          "ferriferous",
          "ferriferous"
        ],
        [
          "minerals",
          "mineral"
        ],
        [
          "olivine",
          "olivine"
        ],
        [
          "pyroxene",
          "pyroxene"
        ],
        [
          "amphibole",
          "amphibole"
        ],
        [
          "biotite",
          "biotite"
        ]
      ],
      "raw_glosses": [
        "(petrology) Composed predominantly of silica-bearing, magnesia-bearing, and ferriferous minerals such as olivine, pyroxene, amphibole, and biotite."
      ],
      "synonyms": [
        {
          "word": "mafic"
        },
        {
          "word": "ferromagnesic"
        },
        {
          "word": "basic"
        }
      ],
      "tags": [
        "not-comparable"
      ],
      "topics": [
        "geography",
        "geology",
        "natural-sciences",
        "petrology"
      ]
    }
  ],
  "word": "simatic"
}

This page is a part of the kaikki.org machine-readable English dictionary. This dictionary is based on structured data extracted on 2024-05-10 from the enwiktionary dump dated 2024-05-02 using wiktextract (a644e18 and edd475d). The data shown on this site has been post-processed and various details (e.g., extra categories) removed, some information disambiguated, and additional data merged from other sources. See the raw data download page for the unprocessed wiktextract data.

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