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单词 oligoclase
释义

Definition of oligoclase in English:

oligoclase

noun ˈɒlɪɡə(ʊ)kleɪzˈɑləɡoʊˌkleɪs
mass noun
  • A feldspar mineral common in siliceous igneous rocks, consisting of a sodium-rich plagioclase (with more calcium than albite).

    奥长石

    Example sentencesExamples
    • They recognized kyanite-staurolite assemblages in pelites to the north of the Annagh Gneiss Complex exposures, but only garnet and oligoclase to the south.
    • Here it was found sparsely as rounded grains associated with pargasite, diopside, oligoclase and lazurite.
    • Granite sample RHGI can be modelled by continuing this felsic scheme, for example with 22% fractionation of oligoclase, amphibole, biotite and the usual minor apatite and titanite.
    • They range from bytownite - labradorite in basalts and gabbros, andesine - oligoclase in diorites and andesites to albite in granites and rhyolites.
    • It is composed of quartz, oligoclase, and microcline, with minor garnet, biotite, muscovite and iron-oxides.
    • However, this assumption is inconsistent with the fairly simultaneous appearance of the second garnet generation and oligoclase.

Origin

Mid 19th century: from oligo- 'relatively little' + Greek klasis 'breaking' (because thought to have a less perfect cleavage than albite).

Definition of oligoclase in US English:

oligoclase

nounˈɑləɡoʊˌkleɪsˈäləɡōˌklās
  • A feldspar mineral common in siliceous igneous rocks, consisting of a sodium-rich plagioclase (with more calcium than albite).

    奥长石

    Example sentencesExamples
    • They range from bytownite - labradorite in basalts and gabbros, andesine - oligoclase in diorites and andesites to albite in granites and rhyolites.
    • They recognized kyanite-staurolite assemblages in pelites to the north of the Annagh Gneiss Complex exposures, but only garnet and oligoclase to the south.
    • Granite sample RHGI can be modelled by continuing this felsic scheme, for example with 22% fractionation of oligoclase, amphibole, biotite and the usual minor apatite and titanite.
    • Here it was found sparsely as rounded grains associated with pargasite, diopside, oligoclase and lazurite.
    • However, this assumption is inconsistent with the fairly simultaneous appearance of the second garnet generation and oligoclase.
    • It is composed of quartz, oligoclase, and microcline, with minor garnet, biotite, muscovite and iron-oxides.

Origin

Mid 19th century: from oligo- ‘relatively little’ + Greek klasis ‘breaking’ (because thought to have a less perfect cleavage than albite).

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更新时间:2025/1/31 5:50:45